With annotations by: AccessIPCC - Version 1.02 - 2010 Dec 14 - Contains annotated versions of all 44 Chapters of Working Groups 1, 2 & 3
With the exception of Chapter and Section headings, all coloured text has been inserted by AccessIPCC. The non-coloured text is the IPCC original.
A number of emails from the Climate Research Unit (CRU) of the University of East Anglia were published on the Internet in November 2009. This has provided a window into the world of climate science.
We have identified a number of key individuals involved in the emails whom we have designated as Persons of Concern [PoC]; a Journal in which a PoC has published has been designated as a Journal of Concern [JoC].
This is not to suggest that we believe such papers are necessarily flawed, but rather that, as Joseph Alcamo noted at Bali in October 2009, "as policymakers and the public begin to grasp the multi-billion dollar price tag for mitigating and adapting to climate change, we should expect a sharper questioning of the science behind climate policy".
References occur in a list at the end of each chapter. Citations are within the normal text of sections and paragraphs.
Person of Concern Key individual involved in CRU emails as defined in this spreadsheet.
|References, Citations, IPCC Roles||2||2|
Journal of Concern A Journal which has published articles by one or more PoCs (Person of Concern)
Model or Simulation Reference appears to be a model or simulation, not observation or experiment
Non Peer Reviewed Reference has no Journal or no Volume or no Pages or it has Editors.
Self Reference Concern Author of a chapter containing references to own work.
|References, Citations, IPCC Roles||37||66|
Paper authored or co-authored by person who is also in list of Authors of another chapter.
Paper dated 2007, when IPCC policy stated cutoff was December 2005
The short inline citation matched with more than one reference; however, AccessIPCC will link to the first reference found.
The short inline citation was not matched with any reference. Believed to be caused by typing errors.
The reference was probably peer reviewed.
|Chapter 10: Asia||-||-||-||-|
|10.1 Summary of knowledge assessed in the Third Assessment Report||-||-||-||-|
|10.1.1 Climate change impacts in Asia||-||1||-||-|
|10.1.2 Vulnerabilities and adaptive strategies||-||-||-||-|
|10.2 Current sensitivity and vulnerability||-||-||-||-|
|10.2.1 Asia: regional characteristics||-||7||-||-|
|10.2.2 Observed climate trends, variability and extreme events||1||2||-||-|
|10.2.3 Observed changes in extreme climatic events||3||34||-||-|
|10.2.4 Impacts of observed changes in climate trends, variability and extreme events||-||-||-||-|
|10.2.4.1 Agriculture and food production||4||4||1||-|
|10.2.4.2 Hydrology and water resources||14||15||-||-|
|10.2.4.3 Oceans and coastal zones||5||12||-||-|
|10.2.4.4 Natural ecosystems||4||16||-||-|
|10.2.4.6 Human health||-||1||-||-|
|10.3 Assumptions about future trends||-||-||-||-|
|10.4 Key future impacts and vulnerabilities||-||-||-||-|
|10.4.1 Agriculture and food security||-||-||-||-|
|10.4.1.2 Farming system and cropping areas||2||6||-||-|
|10.4.1.3 Livestock, fishery, aquaculture||-||10||-||-|
|10.4.1.4 Future food supply and demand||1||9||-||-|
|10.4.1.5 Pests and diseases||-||3||-||-|
|10.4.2 Hydrology and water resources||-||-||-||-|
|10.4.2.1 Water availability and demand||2||6||-||1|
|10.4.2.2 Water quality||1||6||-||-|
|10.4.2.3 Implications of droughts and floods||2||4||-||-|
|10.4.3 Coastal and low lying areas||-||-||-||-|
|10.4.3.1 Coastal erosion and inundation of coastal lowland||6||18||-||1|
|10.4.3.2 Deltas, estuaries, wetland and other coastal ecosystems||5||16||-||-|
|10.4.4 Natural ecosystems and biodiversity||-||-||-||-|
|10.4.4.1 Structure, production and function of forests||3||10||-||-|
|10.4.4.2 Grasslands, rangelands and endangered species||2||2||1||-|
|10.4.6 Human dimensions||-||1||-||-|
|10.4.6.1 Population growth||1||3||-||-|
|10.4.6.2 Development activities||-||-||-||-|
|10.4.6.3 Climate extremes and migration||-||4||-||1|
|10.4.6.4 Urban development, infrastructure linkages, industry and energy||1||7||-||-|
|10.4.6.5 Financial aspects||1||7||-||-|
|10.4.6.6 Vulnerability of the poor||-||-||-||-|
|10.5 Adaptation: sector-specific practices, options and constraints||-||-||-||-|
|10.5.1 Agriculture and food security||8||6||-||-|
|10.5.2 Hydrology and water resources||1||6||-||-|
|10.5.3 Coastal and low lying areas||4||5||-||-|
|10.5.4 Natural ecosystems and biodiversity||-||1||-||-|
|10.5.5 Human health||2||2||-||-|
|10.5.6 Human dimensions||4||5||-||-|
|10.5.7 Key constraints and measures to strengthen adaptation||1||6||-||-|
|10.6 Case studies||-||-||-||-|
|10.6.1 Megadeltas in Asia||6||26||-||-|
|10.6.2 The Himalayan glaciers||-||3||-||-|
|10.7 Implications for sustainable development||-||-||-||-|
|10.7.1 Poverty and illiteracy||1||3||-||-|
|10.7.2 Economic growth and equitable development||2||-||-||-|
|10.7.3 Compliance with and governance of||-||1||-||-|
|10.7.4 Conservation of natural resources||1||-||-||-|
|10.8 Key uncertainties, research gaps and priorities||-||-||-||-|
|10.8.2 Confidence levels and unknowns||-||3||-||-|
|10.8.3 Research gaps and priorities||-||2||-||-|
|Number of citations of various credibilities||108||357||2||5|
|Percentages of citations of various credibilities||22.9%||75.6%||0.4%||1.1%|
Rex Victor Cruz (Philippines), Hideo Harasawa (Japan) [SRC:5], Murari Lal (India) [SRC:9], Shaohong Wu (China) [SRC:1],
|SRC >= 5||2|
|Potentially Biased Authors||3|
Yurij Anokhin (Russia) [SRC:4], Batima Punsalmaa (Mongolia), Yasushi Honda (Japan) [SRC:3], Mostafa Jafari (Iran), Congxian Li (China) [SRC:4], Nguyen Huu Ninh (Vietnam),
|Potentially Biased Authors||3|
Shiv D. Atri (India), Joseph Canadell (Australia), Seita Emori (Japan) [SRC:4], Daidu Fan (China) [SRC:3], Hui Ju (China) [SRC:1], Shuangcheng Li (China) [SRC:1], Tushar K. Moulik (India), Faizal Parish (Malaysia), Yoshiki Saito (Japan) [SRC:4], Ashok K. Sharma (India) [SRC:1], Kiyoshi Takahashi (Japan) [SRC:2], Tran Viet Lien (Vietnam), Qiaomin Zhang (China) [SRC:2],
|Potentially Biased Authors||8|
Daniel Murdiyarso (Indonesia) [SRC:4], Shuzo Nishioka (Japan) [SRC:2],
|Potentially Biased Authors||2|
Cruz, R.V., H. Harasawa, M. Lal, S. Wu, Y. Anokhin, B. Punsalmaa, Y. Honda, M. Jafari, C. Li and N. Huu Ninh, 2007: Asia. Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, M.L. Parry, O.F. Canziani, J.P. Palutikof, P.J. van der Linden and C.E. Hanson, Eds., Cambridge University Press, Cambridge, UK, 469-506.
New evidences show that climate change has affected many sectors in Asia (medium confidence).
The crop yield in many countries of Asia has declined, partly due to rising temperatures and extreme weather events. The retreat of glaciers and permafrost in Asia in recent years is unprecedented as a consequence of warming. The frequency of occurrence of climate-induced diseases and heat stress in Central, East, South and South-East Asia has increased with rising temperatures and rainfall variability. Observed changes in terrestrial and marine ecosystems have become more pronounced (medium confidence). [ 10.2.3 , 10.2.4 ]
Future climate change is likely to affect agriculture, risk of hunger and water resource scarcity with enhanced climate variability and more rapid melting of glaciers (medium confidence).
About 2.5 to 10% decrease in crop yield is projected for parts of Asia in 2020 s and 5 to 30% decrease in 2050 s compared with 1990 levels without CO2 effects (medium confidence) [ 10.4.1.1 ]. Freshwater availability in Central, South, East and South-East Asia, particularly in large river basins such as Changjiang, is likely to decrease due to climate change, along with population growth and rising standard of living that could adversely affect more than a billion people in Asia by the 2050 s (high confidence) [ 10.4.2 ]. It is estimated that under the full range of Special Report on Emission Scenarios (SRES) scenarios, 120 million to 1.2 billion will experience increased water stress by the 2020 s, and by the 2050 s the number will range from 185 to 981 million people (high confidence) [ 10.4.2.3 ]. Accelerated glacier melt is likely to cause increase in the number and severity of glacial melt-related floods, slope destabilisation and a decrease in river flows as glaciers recede (medium confidence) [ 10.2.4.2 , 10.4.2.1 ]. An additional 49 million, 132 million and 266 million people of Asia, projected under A2 scenario without carbon fertilisation, could be at risk of hunger by 2020, 2050 and 2080, respectively (medium confidence) [ 10.4.1.4 ].
Marine and coastal ecosystems in Asia are likely to be affected by sea-level rise and temperature increases (high confidence).
Projected sea-level rise is very likely to result in significant losses of coastal ecosystems and a million or so people along the coasts of South and South-East Asia will likely be at risk from flooding (high confidence) [ 10.4.3.1 ]. Sea-water intrusion due to sea-level rise and declining river runoff is likely to increase the habitat of brackish water fisheries but coastal inundation is likely to seriously affect the aquaculture industry and infrastructure particularly in heavily-populated megadeltas (high confidence) [ 10.4.1.3 , 10.4.3.2 ]. Stability of wetlands, mangroves and coral reefs around Asia is likely to be increasingly threatened (high confidence) [ 10.4.3.2 , 10.6.1 ]. Recent risk analysis of coral reef suggests that between 24% and 30% of the reefs in Asia are likely to be lost during the next 10 years and 30 years, respectively (medium confidence) [ 10.4.3.2 ].
Climate change is likely to affect forest expansion and migration, and exacerbate threats to biodiversity resulting from land use/cover change and population pressure in most of Asia (medium confidence).
Increased risk of extinction for many flora and fauna species in Asia is likely as a result of the synergistic effects of climate change and habitat fragmentation (medium confidence) [ 10.4.4.1 ]. In North Asia, forest growth and northward shift in the extent of boreal forest is likely (medium confidence) [ 10.4.4 ]. The frequency and extent of forest fires in North Asia is likely to increase in the future due to climate change that could likely limit forest expansion (medium confidence) [ 10.4.4 ].
Future climate change is likely to continue to adversely affect human health in Asia (high confidence).
Increases in endemic morbidity and mortality due to diarrhoeal disease primarily associated with climate change are expected in South and South-East Asia (high confidence). Increases in coastal water temperature would exacerbate the abundance and/or toxicity of cholera in south Asia (high confidence). Natural habitats of vector-borne and water-borne diseases in north Asia are likely to expand in the future (medium confidence). [10.4.5]
Multiple stresses in Asia will be compounded further due to climate change (high confidence).
It is likely that climate change will impinge on sustainable development of most developing countries of Asia as it compounds the pressures on natural resources and the environment associated with rapid urbanisation, industrialisation and economic development. Mainstreaming sustainable development policies and the inclusion of climate-proofing concepts in national development initiatives are likely to reduce pressure on natural resources and improve management of environmental risks (high confidence) [ 10.7 ].
Climate change and variability.
Extreme weather events in Asia were reported to provide evidence of increases in the intensity or frequency on regional scales throughout the 20th century. The Third Assessment Report (TAR) predicted that the area-averaged annual mean warming would be about 3°C in the decade of the 2050 s and about 5°C in the decade of the 2080 s over the land regions of Asia as a result of future increases in atmospheric concentration of greenhouse gases ( Lal et al., 2001a [NPR, SRC] ). The rise in surface air temperature was projected to be most pronounced over boreal Asia in all seasons.
Climate change impacts.
An enhanced hydrological cycle and an increase in area-averaged annual mean rainfall over Asia were projected. The increase in annual and winter mean precipitation would be highest in boreal Asia; as a consequence, the annual runoff of major Siberian Rivers would increase significantly. A decline in summer precipitation was likely over the central parts of arid and semi-arid Asia leading to expansion of deserts and periodic severe water stress conditions. Increased rainfall intensity, particularly during the summer monsoon, could increase flood-prone areas in temperate and tropical Asia.
Vulnerable sectors. Water and agriculture sectors are likely to be most sensitive to climate change-induced impacts in Asia. Agricultural productivity in Asia is likely to suffer severe losses because of high temperature, severe drought, flood conditions, and soil degradation. Forest ecosystems in boreal Asia would suffer from floods and increased volume of runoff associated with melting of permafrost regions. The processes of permafrost degradation resulting from global warming strengthen the vulnerability of all relevant climate-dependent sectors affecting the economy in high-latitude Asia.
Vulnerable regions. Countries in temperate and tropical Asia are likely to have increased exposure to extreme events, including forest die back and increased fire risk, typhoons and tropical storms, floods and landslides, and severe vector-borne diseases. The stresses of climate change are likely to disrupt the ecology of mountain and highland systems in Asia. Glacial melt is also expected to increase under changed climate conditions. Sea-level rise would cause large-scale inundation along the vast Asian coastline and recession of flat sandy beaches. The ecological stability of mangroves and coral reefs around Asia would be put at risk.
Adaptation strategies. Increases in income levels, education and technical skills, and improvements in public food distribution, disaster preparedness and management, and health care systems through sustainable and equitable development could substantially enhance social capital and reduce the vulnerability of developing countries of Asia to climate change. Development and implementation of incremental adaptation strategies and policies to exploit ‘no regret’ measures and ‘win-win’ options were to be preferred over other options. Adaptations to deal with sea-level rise, potentially more intense cyclones, and threats to ecosystems and biodiversity were recommended as high priority actions in temperate and tropical Asian countries. It was suggested that the design of an appropriate adaptation programme in any Asian country must be based on comparison of damages avoided with costs of adaptation.
Advances since the TAR. Aside from new knowledge on the current trends in climate variability and change – including the extreme weather events – more information is now available that confirms most of the key findings on impacts, vulnerabilities and adaptations for Asia. This chapter assesses the state of knowledge on impacts, vulnerabilities and adaptations for various regions in Asia.
Asia is the most populous continent ( Figure 10.1 ). Its total population in 2002 was reported to be about 3,902 million, of which almost 61% is rural and 38.5% lives within 100 km of the coast ( Table 10.1 ). The coastline of Asia is 283,188 km long ( Duedall and Maul, 2005 [NPR] ). In this report, Asia is divided into seven sub-regions, namely North Asia, Central Asia, West Asia, Tibetan Plateau, East Asia, South Asia and South-East Asia (for further details on boundaries of these sub-regions see Table 10.5 ).
North Asia, located in the Boreal climatic zone, is the coldest region of the northern hemisphere in winter ( ACIA, 2005 [NPR] ). One of the world’s largest and oldest lakes, Baikal, located in this region contains as much as 23,000 km3 of freshwater and holds nearly 20% of the world surface freshwater resources ( Izrael and Anokhin, 2000 [SRC] ). Central and West Asia include several countries of predominantly arid and semi-arid region. Tibetan Plateau can be divided into the eastern part (forest region), the northern part (open grassland), and the southern and central part (agricultural region). East Asia stretches in the east-west direction to about 5,000 km and in the north-south to about 3,000 km including part of China, Japan and Korea. South Asia is physiographically diverse and ecologically rich in natural and crop-related biodiversity. The region has five of the 20 megacities of the world ( UN-HABITAT, 2004 [NPR] ). South-East Asia is characterised by tropical rainforest, monsoon climates with high and constant rainfall, heavily-leached soils, and diverse ethnic groups. Table 10.1 lists the key socio-economic and natural resource features of the countries of Asia ( WRI, 2003 [NPR] ; FAO, 2004a [NPR] , b, c; World Bank, 2005 [NPR] ).
|Country||Total population (1,000 inhab) 2004||2004 GDP per capita (constant US$2000)||Land area* (1,000ha) 2002||Arable land and perm-anent crops (1,000 ha) 2002||Arable land (1,000 ha) 2002||Total forest area, 2005 (1,000ha)||Percent of forest cover (FAO, 2005)||Natural RWR**, 2002 (per capita m3)||Water res-ources: total renewable per capita (actual) (m3/inhab/yr) 1998 to 2002||Average production of cereals, 2005 (1,000t)||Annual fish and fishery products (kg/ capita) (2002)|
|Iran, Islamic Rep||69788||1885||163620||17088||15020||11075||6.8||1900||2020||21510||5|
|Papua New Guinea||5836||604||45286||870||220||7162||24||x||143394||11||x|
|Russia - E. of Urals||142397||2286||1638098||125300||123465||808790||47.9||31354||31283||76420||19|
|Syrian Arab Rep||18223||1115||18378||5421||4593||461||2.5||1541||1511||5620||3|
Past and present climate trends and variability in Asia are generally characterised by increasing surface air temperature which is more pronounced during winter than in summer. Increasing trends have been observed across the seven sub-regions of Asia. The observed increases in some parts of Asia during recent decades ranged between less than 1°C to 3°C per century. Increases in surface temperature are most pronounced in North Asia ( (Savelieva et al., 2000; ) Izrael et al., 2002a [NPR] ; Climate Change in Russia, 2003; Gruza and Rankova, 2004 [NPR] ).
Interseasonal, interannual and spatial variability in rainfall trend has been observed during the past few decades all across Asia. Decreasing trends in annual mean rainfall are observed in Russia, North-East and North China, coastal belts and arid plains of Pakistan, parts of North-East India, Indonesia, Philippines and some areas in Japan. Annual mean rainfall exhibits increasing trends in Western China, Changjiang Valley and the South-Eastern coast of China, Arabian Peninsula, Bangladesh and along the western coasts of the Philippines. Table 10.2 lists more details on observed characteristics in surface air temperature and rainfall in Asian sub-regions.
|Region||Country||Change in temperature||Change in precipitation||References|
|North Asia||Russia||2 to 3°C rise in past 90 years, more pronounced in spring and winter||Highly variable, decrease during 1951 to 1995, increase in last decade||Savelieva et al., 2000; Peterson et al., 2002; Gruza and Rankova, 2004|
|Mongolia||1.8°C rise in last 60 years, most pronounced in winter||7.5% decrease in summer and 9% increase in winter||Batima et al., 2005a; Natsagdorj et al., 2005|
|Central Asia||Regional mean||1 to 2°C rise in temperature per century||No clear trend during 1900 to 1996.||Peterson et al., 2002|
|North-West China||0.7°C increase in mean annual temperature from 1961 to 2000||Between 22% and 33% increase in rainfall||Shi et al., 2002|
|Tibetan Plateau||Regional mean||0.16 and 0.32°C per decade increase in annual and winter temperatures, respectively||Generally increasing in north-east region||Liu et al., 1998; Yao et al., 2000; Liu and Chen, 2001; Cai et al., 2003; Du and Ma, 2004; Zhao et al., 2004|
|West Asia (Middle East)||Iran||During 1951 to 2003 several stations in different climatological zones of Iran reported significant decrease in frost days due to rise in surface temperature||Some stations show a decreasing trend in precipitation (Anzali, Tabriz, Zahedan) while others (Mashad, Shiraz) have reported increasing trends||IRIMO, 2006a, b; Rahimzadeh, 2006|
|East Asia||China||Warming during last 50 years, more pronounced in winter than summer, rate of increase more pronounced in minimum than in maximum temperature||Annual rain declined in past decade in North-East and North China, increase in Western China, Changjiang River and along south-east coast||Zhai et al., 1999; Hu et al., 2003; Zhai and Pan, 2003|
|Japan||About 1.0°C rise in 20th century, 2 to 3°C rise in large cities||No significant trend in the 20th century although fluctuations increased||Ichikawa, 2004; Japan Meteorological Agency, 2005|
|Korea||0.23°C rise in annual mean temperature per decade, increase in diurnal range||More frequent heavy rain in recent years||Jung et al., 2002; Ho et al., 2003|
|South Asia||India||0.68°C increase per century, increasing trends in annual mean temperature, warming more pronounced during post monsoon and winter||Increase in extreme rains in north-west during summer monsoon in recent decades, lower number of rainy days along east coast||Kripalani et al., 1996; Lal et al., 1996; Lal et al., 2001b; Singh and Sontakke, 2002; Lal, 2003|
|Nepal||0.09°C per year in Himalayas and 0.04°C in Terai region, more in winter||No distinct long-term trends in precipitation records for 1948 to 1994||Shrestha et al., 2000; Bhadra, 2002; Shrestha, 2004|
|Pakistan||0.6 to 1.0°C rise in mean temperature in coastal areas since early 1900s||10 to 15% decrease in coastal belt and hyper arid plains, increase in summer and winter precipitation over the last 40 years in northern Pakistan||Farooq and Khan, 2004|
|Bangladesh||An increasing trend of about 1°C in May and 0.5°C in November during the 14 year period from 1985 to 1998||Decadal rain anomalies above long term averages since 1960s||Mirza and Dixit, 1997; Khan et al., 2000; Mirza, 2002|
|Sri Lanka||0.016°C increase per year between 1961 to 90 over entire country, 2°C increase per year in central highlands||Increase trend in February and decrease trend in June||Chandrapala and Fernando, 1995; Chandrapala, 1996|
|S-E Asia||General||0.1 to 0.3°C increase per decade reported between 1951 to 2000||Decreasing trend between 1961 and 1998. Number of rainy days have declined throughout S-E Asia||Manton et al., 2001|
|Indonesia||Homogeneous temperature data were not available||Decline in rainfall in southern and increase in northern region||Manton et al., 2001; Boer and Faqih, 2004|
|Philippines||Increase in mean annual, maximum and minimum temperatures by 0.14°C between 1971 to 2000||Increase in annual mean rainfall since 1980s and in number of rainy days since 1990s, increase in inter-annual variability of onset of rainfall||PAGASA, 2001; Cruz et al., 2006|
New evidences on recent trends, particularly on the increasing tendency in the intensity and frequency of extreme weather events in Asia over the last century and into the 21st century, are briefly discussed below and summarised in Table 10.3 . In South-East Asia, extreme weather events associated with El-Niño were reported to be more frequent and intense in the past 20 years ( Trenberth and Hoar, 1997 [PoC, JoC] ; Aldhous, 2004 [JoC] ).
|Russia||Heatwaves broke past 22-year record in May 2005||Shein, 2006|
|Mongolia||Heatwave duration has increased by 8 to 18 days in last 40 years; coldwave duration has shortened by 13.3 days||Batima et al., 2005a|
|China||Increase in frequency of short duration heatwaves in recent decade, increasing warmer days and nights in recent decades||Zhai et al., 1999; Zhai and Pan, 2003|
|Japan||Increasing incidences of daily maximum temperature >35°C, decrease in extremely low temperature||Kawahara and Yamazaki, 1999; Japan Meteorological Agency, 2005|
|Korea||Increasing frequency of extreme maximum temperatures with higher values in 1980s and 1990s; decrease in frequency of record low temperatures during 1958 to 2001||Ryoo et al., 2004|
|India||Frequency of hot days and multiple-day heatwave has increased in past century; increase in deaths due to heat stress in recent years||De and Mukhopadhyay, 1998; Lal, 2003|
|South-East Asia||Increase in hot days and warm nights and decrease in cold days and nights between 1961 and 1998||Manton et al., 2001; Cruz et al., 2006; Tran et al., 2005|
|Intense Rains and Floods|
|Russia||Increase in heavy rains in western Russia and decrease in Siberia; increase in number of days with more than 10 mm rain; 50 to 70% increase in surface runoff in Siberia||Gruza et al., 1999; Izrael and Anokhin, 2001; Ruosteenoja et al., 2003; Gruza and Rankova, 2004|
|China||Increasing frequency of extreme rains in western and southern parts including Changjiang river, and decrease in northern regions; more floods in Changjiang river in past decade; more frequent floods in North-East China since 1990s; more intense summer rains in East China; severe flood in 1999; seven-fold increase in frequency of floods since 1950s||Zhai et al., 1999; Ding and Pan, 2002; Zhai and Pan, 2003; Zhai, 2004|
|Japan||Increasing frequency of extreme rains in past 100 years attributed to frontal systems and typhoons; serious flood in 2004 due to heavy rains brought by 10 typhoons; increase in maximum rainfall during 1961 to 2000 based on records from 120 stations||Kawahara and Yamazaki, 1999; Isobe, 2002; Kajiwara et al., 2003; Kanai et al., 2004|
|South Asia||Serious and recurrent floods in Bangladesh, Nepal and north-east states of India during 2002, 2003 and 2004; a record 944 mm of rainfall in Mumbai, India on 26 to 27 July 2005 led to loss of over 1,000 lives with loss of more than US$250 million; floods in Surat, Barmer and in Srinagar during summer monsoon season of 2006; 17 May 2003 floods in southern province of Sri Lanka were triggered by 730 mm rain||India Meteorological Department, 2002 to 2006; Dartmouth Flood Observatory, 2003.|
|South-East Asia||Increased occurrence of extreme rains causing flash floods in Vietnam; landslides and floods in 1990 and 2004 in the Philippines, and floods in Cambodia in 2000||FAO/WFP, 2000; Environment News Service, 2002; FAO, 2004a; Cruz et al., 2006; Tran et al., 2005|
|Russia||Decreasing rain and increasing temperature by over 1°C have caused droughts; 27 major droughts in 20th century have been reported||Golubev and Dronin, 2003; Izrael and Sirotenko, 2003|
|Mongolia||Increase in frequency and intensity of droughts in recent years; droughts in 1999 to 2002 affected 70% of grassland and killed 12 million livestock||Batima, 2003; Natsagdorj et al., 2005|
|China||Increase in area affected by drought has exceeded 6.7 Mha since 2000 in Beijing, Hebei Province, Shanxi Province, Inner Mongolia and North China; increase in dust storm affected area||Chen et al., 2001; Yoshino, 2000, 2002; Zhou, 2003|
|South Asia||50% of droughts associated with El Niño; consecutive droughts in 1999 and 2000 in Pakistan and N-W India led to sharp decline in watertables; consecutive droughts between 2000 and 2002 caused crop failures, mass starvation and affected ~11 million people in Orissa; droughts in N-E India during summer monsoon of 2006||Webster et al., 1998; Lal, 2003; India Meteorological Department, 2006|
|South-East Asia||Droughts normally associated with ENSO years in Myanmar, Laos, Philippines, Indonesia and Vietnam; droughts in 1997 to 98 caused massive crop failures and water shortages and forest fires in various parts of Philippines, Laos and Indonesia||Duong, 2000; Kelly and Adger, 2000; Glantz, 2001; PAGASA, 2001|
|Philippines||On an average, 20 cyclones cross the Philippines Area of Responsibility with about 8 to 9 landfall each year; with an increase of 4.2 in the frequency of cyclones entering PAR during the period 1990 to 2003||PAGASA, 2001|
|China||Number and intensity of strong cyclones increased since 1950s; 21 extreme storm surges in 1950 to 2004 of which 14 occurred during 1986 to 2004||Fan and Li, 2005|
|South Asia||Frequency of monsoon depressions and cyclones formation in Bay of Bengal and Arabian Sea on the decline since 1970 but intensity is increasing causing severe floods in terms of damages to life and property||Lal, 2001, 2003|
|Japan||Number of tropical storms has two peaks, one in mid 1960s and another in early 1990s, average after 1990 and often lower than historical average||Japan Meteorological Agency, 2005|
Significantly longer heatwave duration has been observed in many countries of Asia, as indicated by pronounced warming trends and several cases of severe heatwaves ( (De and Mukhopadhyay, 1998; ) Kawahara and Yamazaki, 1999 [NPR] ; Zhai et al., 1999 [JoC, SRC] ; Lal, 2003 [SRC] ; Zhai and Pan, 2003 [JoC] ; Ryoo et al., 2004 [JoC] ; Batima et al., 2005a [ARC] ; Cruz et al., 2006 [NPR, ARC] ; Tran et al., 2005 [NPR] ).
Generally, the frequency of occurrence of more intense rainfall events in many parts of Asia has increased, causing severe floods, landslides, and debris and mud flows, while the number of rainy days and total annual amount of precipitation has decreased ( Zhai et al., 1999 [JoC, SRC] ;( Khan et al., 2000; ) Shrestha et al., 2000 [JoC] ; Izrael and Anokhin, 2001 [NPR, SRC] ; Mirza, 2002 [JoC] ; Kajiwara et al., 2003 [NPR, ARC] ; Lal, 2003 [SRC] ; Min et al., 2003 [JoC] ; Ruosteenoja et al., 2003 [NPR, MoS, ARC] ; Zhai and Pan, 2003 [JoC] ; Gruza and Rankova, 2004 [NPR] ;( Zhai, 2004 ) ). However, there are reports that the frequency of extreme rainfall in some countries has exhibited a decreasing tendency ( Manton et al., 2001 [JoC, ARC] ; Kanai et al., 2004 [ARC] ).
Increasing frequency and intensity of droughts in many parts of Asia are attributed largely to a rise in temperature, particularly during the summer and normally drier months, and during ENSO events ( Webster et al., 1998 [JoC, MoS] ; Duong, 2000 [NPR] ; PAGASA, 2001 [NPR] ; Lal, 2002 [NPR, SRC] , 2003; Batima, 2003 [NPR, ARC] ; Gruza and Rankova, 2004 [NPR] ; Natsagdorj et al., 2005 [NPR, MoS, ARC] ).
Recent studies indicate that the frequency and intensity of tropical cyclones originating in the Pacific have increased over the last few decades ( Fan and Li, 2005 [SRC] ). In contrast, cyclones originating from the Bay of Bengal and Arabian Sea have been noted to decrease since 1970 but the intensity has increased ( Lal, 2001 [SRC] ). In both cases, the damage caused by intense cyclones has risen significantly in the affected countries, particularly India, China, Philippines, Japan, Vietnam and Cambodia, Iran and Tibetan Plateau ( PAGASA, 2001 [NPR] ; ABI, 2005 [NPR] ; GCOS, 2005a [NPR] , b).
Production of rice, maize and wheat in the past few decades has declined in many parts of Asia due to increasing water stress arising partly from increasing temperature, increasing frequency of El Niño and reduction in the number of rainy days ( (Wijeratne, 1996; ) Aggarwal et al., 2000 [ARC] ;( Jin et al., 2001; ) Fischer et al., 2002 [NPR] ;( Tao et al., 2003a; ) ( Tao et al., 2004 ) ). In a study at the International Rice Research Institute, the yield of rice was observed to decrease by 10% for every 1°C increase in growing-season minimum temperature ( Peng et al., 2004 [JoC] ). A decline in potentially good agricultural land in East Asia and substantial increases in suitable areas and production potentials in currently cultivated land in Central Asia have also been reported ( Fischer et al., 2002 [NPR] ). Climate change could make it more difficult than it is already to step up the agricultural production to meet the growing demands in Russia (Izrael and Sirotenko, 2003 [NotFound] ) and other developing countries in Asia.
Rapid thawing of permafrost ( Table 10.4 ) and decrease in depths of frozen soils (4 to 5 m in Tibet according to ( Wang et al., 2004b ) ) due largely to rising temperature has threatened many cities and human settlements, has caused more frequent landslides and degeneration of some forest ecosystems, and has resulted in increased lake-water levels in the permafrost region of Asia ( (Osterkamp et al., 2000; ) ( Guo et al., 2001; ) Izrael and Anokhin, 2001 [NPR, SRC] ; Jorgenson et al., 2001 [JoC] ; Izrael et al., 2002b [SRC] ; Fedorov and Konstantinov, 2003 [NPR] ; Gavriliev and Efremov, 2003 [NPR] ;( Melnikov and Revson, 2003; ) Nelson, 2003 [JoC, ARC] ; ACIA, 2005 [NPR] ).
|Country||Region||Permafrost temperature change/trends||References|
|Russia||East Siberia (1.6 to 3.2 m), 1960 to 1992||+0.03°C/year||Romanovsky et al., 2001|
|West Siberia (10 m), 1960 to 2005||+0.6°C/year||Izrael et al., 2006|
|China||Qinghai-Tibet Plateau (1975 to 1989)||+0.2 to +0.3°C||Cheng and Wu, 2007|
|Kazakhstan||Northern Tian Shan (1973 to 2003)||+0.2° to +0.6°C||Marchenko, 2002|
|Mongolia||Khentei and Khangai Mountains, Lake Hovsgol (1973 to 2003)||+0.3° to +0.6°C||Sharkhuu, 2003|
In drier parts of Asia, melting glaciers account for over 10% of freshwater supplies ( (Meshcherskaya and Blazhevich, 1990; ) Fitzharris, 1996 [NPR, ARC] ; Meier, 1998 [NPR] ). Glaciers in Asia are melting faster in recent years than before, as reported in Central Asia, Western Mongolia and North-West China, particularly the Zerafshan glacier, the Abramov glacier and the glaciers on the Tibetan Plateau (see Section 10.6.2 ( (Pu et al., 2004 ) ). As a result of rapid melting of glaciers, glacial runoff and frequency of glacial lake outbursts causing mudflows and avalanches have increased ( Bhadra, 2002 [NPR] ; WWF, 2005 [NPR] ). A recent study in northern Pakistan, however, suggests that glaciers in the Indus Valley region may be expanding, due to increases in winter precipitation over western Himalayas during the past 40 years ( (Archer and Fowler, 2004 ) ).
In parts of China, the rise in temperature and decreases in precipitation ( (Ma and Fu, 2003; ) ( Wang and Zhai, 2003 ) ), along with increasing water use have caused water shortages that led to drying up of lakes and rivers ( ( Liu et al., 2006; ) ( Wang and Jin, 2006 ) ). In India, Pakistan, Nepal and Bangladesh, water shortages have been attributed to rapid urbanisation and industrialisation, population growth and inefficient water use, which are aggravated by changing climate and its adverse impacts on demand, supply and water quality. In arid Central and West Asia, changes in climate and its variability continue to challenge the ability of countries in the arid and semi-arid region to meet the growing demands for water ( (Abu-Taleb, 2000; ) UNEP, 2002 [NPR] ;( Bou-Zeid and El-Fadel, 2002; ) Ragab and Prudhomme, 2002 [ARC] ). Decreasing precipitation and increasing temperature commonly associated with ENSO have been reported to increase water shortage, particularly in parts of Asia where water resources are already under stress from growing water demands and inefficiencies in water use ( Manton et al., 2001 [JoC, ARC] ).
Global warming and sea-level rise in the coastal zone of Boreal Asia have influenced sea-ice formation and decay, thermo-abrasion process, permafrost and the time of river freeze-up and break-up in recent decades ( ACIA, 2005 [NPR] ; Leont’yev, 2004 [MoS] ). The coastlines in monsoon Asia are cyclone-prone with ~42% of the world’s total tropical cyclones occurring in this region ( (Ali, 1999 ) ). The combined extreme climatic and non climatic events caused coastal flooding, resulting in substantial economic losses and fatalities ( Yang, 2000 [MoS] ; Li et al., 2004a [SRC] ). Wetlands in the major river deltas have been significantly altered in recent years due to large scale sedimentation, land-use conversion, logging and human settlement ( Lu, 2003 [NPR] ). Coastal erosion in Asia has led to loss of lands at rates dependent on varying regional tectonic activities, sediment supply and sea-level rise ( (Sin, 2000 ) ). Salt water from the Bay of Bengal is reported to have penetrated 100 km or more inland along tributary channels during the dry season ( (Allison et al., 2003 ) ). Severe droughts and unregulated groundwater withdrawal have also resulted in sea-water intrusion in the coastal plains of China ( (Ding et al., 2004 ) ).
Over 34% of the vast and diverse coral reefs of Asia that are of immense ecological and economic importance to this region ( Spalding et al., 2001 [NPR] ; Burke et al., 2002 [NPR] ; Zafar, 2005 [NPR] ) particularly in South, South-East and East Asia are reported to have been lost in 1998, largely due to coral bleaching induced by the 1997 /98 El Niño event Wilkinson,/98 El Niño event Wilkinson,( Arceo et al., 2001; ) Wilkinson, 2002 [NPR] ; Ministry of the Environment and Japanese Coral Reef Society, Ministry of the Environment and Japanese Coral Reef Society, Yamano and Tamura, 2004 [MoS] ). The destructive effects of climate change compound the human-induced damages on the corals in this region. A substantial portion of the vast mangroves in South and South-East Asian regions has also been reportedly lost during the last 50 years of the 20th century, largely attributed to human activities ( Zafar, 2005 [NPR] ). Evidence of the impacts of climate-related factors on mangroves remain limited to the severe destruction of mangroves due to reduction of freshwater flows and salt-water intrusion in the Indus delta and Bangladesh ( IUCN, 2003a [NPR] ).
Increasing intensity and spread of forest fires in Asia were observed in the past 20 years, largely attributed to the rise in temperature and decline in precipitation in combination with increasing intensity of land uses ( Page et al., 2002 [JoC] ; de Grandi et al., 2003 [NPR] ;( Goldammer et al., 2003; ) FFARF, 2004 [NPR] ; Isaev et al., 2004 [NPR] ; Murdiyarso et al., 2004 [SRC] ; Shoigu, 2004 [NPR] ; Vorobyov, 2004 [NPR] ; Achard et al., 2005 [NPR] ; Murdiyarso and Adiningsih, 2006 [SRC] ). During the last decade, 12,000 to 38,000 wild fires annually hit the boreal forests in North Asia affecting some 0.3 to 3 million hectares ( Dumnov et al., 2005 [NPR] ;( Malevski-Malevich et al., 2005; ) FNCRF, 2006 [NPR] ). Recent studies have also shown a dramatic increase of fires in Siberian peatlands (of which 20 million ha were burnt in 2003 ) linked to increased human activities combined with changing climate conditions, particularly the increase in temperature. Fires in peatlands of Indonesia during the 1997 to 98 El Niño dry season affected over 2 million ha and emitted an estimated 0.81 to 2.57 PgC to the atmosphere ( Page et al., 2002 [JoC] ). In the past 10 years about 3 million ha of peatland in South-East Asia have been burnt, releasing between 3 to 5 PgC, and drainage of peat has affected an additional 6 million ha and released a further 1 to 2 PgC. As a consequence of a 17% decline in spring precipitation and a rise in surface temperature by 1.5°C during the last 60 years, the frequency and aerial extent of the forest and steppe fires in Mongolia have significantly increased over a period of 50 years ( Erdnethuya, 2003 [NPR] ). The 1997 /98 ENSO event in Indonesia triggered forest and brush fires in 9.7 million hectares, with serious domestic and trans-boundary pollution consequences. Thousands of hectares of second growth and logged-over forests were also burned in the Philippines during the 1997 /98 ENSO events ( Glantz, 2001 [NPR] ; PAGASA, 2001 [NPR] ).
With the gradual reduction in rainfall during the growing season for grass, aridity in Central and West Asia has increased in recent years, reducing growth of grasslands and increasing bareness of the ground surface ( (Bou-Zeid and El-Fadel, 2002 ) ). Increasing bareness has led to increased reflection of solar radiation, such that more soil moisture is evaporated and the ground has become increasingly drier in a feedback process, thus adding to the acceleration of grassland degradation ( Zhang et al., 2003 [JoC, MoS] ).
Wetlands in Asia are being increasingly threatened by warmer climate in recent decades. The precipitation decline and droughts in most delta regions of Pakistan, Bangladesh, India and China have resulted in the drying up of wetlands and severe degradation of ecosystems. The recurrent droughts from 1999 to 2001, as well as the building of an upriver reservoir and improper use of groundwater, have led to drying up of the Momoge Wetland located in the Songnen Plain ( (Pan et al., 2003 ) ).
Biodiversity in Asia is being lost as a result of development activities and land degradation (especially overgrazing and deforestation), pollution, over-fishing, hunting, infrastructure development, species invasion, land-use change, climate change and the overuse of freshwater ( UNEP, 2002 [NPR] ; Gopal, 2003 [NPR, MoS, ARC] ). Though evidence of climate-related biodiversity loss in Asia remains limited, a large number of plant and animal species are reported to be moving to higher latitudes and altitudes as a consequence of observed climate change in many parts of Asia in recent years ( (Yoshio and Ishii, 2001; ) IUCN, 2003a [NPR] ). Changes in the flowering date of Japanese Cherry, a decrease in alpine flora in Hokkaido and other high mountains and the expansion of the distribution of southern broad-leaved evergreen trees have also been reported ( (Oda and Ishii, 2001; ) Ichikawa, 2004 [NPR] ;( Kudo et al., 2004; ) Wada et al., 2004 [NPR] ).
In South Asia, endemic morbidity and mortality due to diarrhoeal disease is linked to poverty and hygiene behaviour compounded by the effect of high temperatures on bacterial proliferation ( Checkley et al., 2000 [ARC] ). Diarrhoeal diseases and outbreaks of other infectious diseases (e.g., cholera, hepatitis, malaria, dengue fever) have been reported to be influenced by climate-related factors such as severe floods, ENSO-related droughts, sea-surface temperatures and rainfall in association with non-climatic factors such as poverty, lack of access to safe drinking water and poor sewerage system ( (Durkin et al., 1993; ) Akhtar and McMichael, 1996 [ARC] ;( Bouma and van der Kaay, 1996; ) Colwell, 1996 [JoC] ;( Bangs and Subianto, 1999; ) Lobitz et al., 2000 [JoC] ; Pascual et al., 2000 [JoC, ARC] ;( Bouma and Pascual, 2001; ) Glantz, 2001 [NPR] ;( Pascual et al., 2002; ) Rodo et al., 2002 [JoC, ARC] ).
A large number of deaths due to heatwaves – mainly among the poor, elderly and labourers such as rural daily wage earners, agricultural workers and rickshaw pullers – have been reported in the Indian state of Andhra Pradesh, Orissa and elsewhere during the past five years ( Lal, 2002 [NPR, SRC] ). Serious health risks associated with extreme summer temperatures and heatwaves have also been reported in Siberian cities (Zolotov and Caliberny, 2004 ).
Table 10.5 provides a snapshot of the projections on likely increase in area-averaged seasonal surface air temperature and percent change in area-averaged seasonal precipitation (with respect to the baseline period 1961 to 1990 ) for the seven sub-regions of Asia. The temperature projections for the 21st century, based on Fourth Assessment Report (AR4) Atmosphere-Ocean General Circulation Models (AOGCMs), and discussed in detail in Working Group I Chapter 11 , suggest a significant acceleration of warming over that observed in the 20th century ( Ruosteenoja et al., 2003 [NPR, MoS, ARC] ; Christensen et al., 2007 [NPR, ARC, 2007] ). Warming is least rapid, similar to the global mean warming, in South-East Asia, stronger over South Asia and East Asia and greatest in the continental interior of Asia (Central, West and North Asia). In general, projected warming over all sub-regions of Asia is higher during northern hemispheric winter than during summer for all time periods. The most pronounced warming is projected at high latitudes in North Asia. Recent modelling experiments suggest that the warming would be significant in Himalayan Highlands including the Tibetan Plateau and arid regions of Asia ( (Gao et al., 2003 ) ).
|Sub- regions||Season||2010 to 2039||2040 to 2069||2070 to 2099|
|Temperature °C||Precipitation %||Temperature °C||Precipitation %||Temperature °C||Precipitation %|
The consensus of AR4 models, as discussed in Chapter 2 and in Christensen et al. 2007 [NPR, ARC, 2007] ) and confirmed in several studies using regional models ( Lal, 2003 [SRC] ; Rupa Kumar et al., 2003 [NPR] ; Kwon et al., 2004 [NPR] ;( Boo et al., 2004; ) Japan Meteorological Agency, 2005; Kurihara et al., 2005 [MoS] ), indicates an increase in annual precipitation in most of Asia during this century; the relative increase being largest and most consistent between models in North and East Asia. The sub-continental mean winter precipitation will very likely increase in northern Asia and the Tibetan Plateau and likely increase in West, Central, South-East and East Asia. Summer precipitation will likely increase in North, South, South-East and East Asia but decrease in West and Central Asia. The projected decrease in mean precipitation in Central Asia will be accompanied by an increase in the frequency of very dry spring, summer and autumn seasons. In South Asia, most of the AR4 models project a decrease of precipitation in December, January and February (DJF) and support earlier findings reported in Lal et al. 2001b [MoS, SRC] ).
An increase in occurrence of extreme weather events including heatwave and intense precipitation events is also projected in South Asia, East Asia, and South-East Asia ( Emori et al., 2000 [NPR, SRC] ; Kato et al., 2000 [MoS] ; Sato, 2000 [MoS] ; Lal, 2003 [SRC] ; Rupa Kumar et al., 2003 [NPR] ; Hasumi and Emori, 2004 [NPR, MoS, SRC] ; Ichikawa, 2004 [NPR] ; May, 2004b; ( Walsh, 2004; ) Japan Meteorological Agency, 2005; Kurihara et al., 2005 [MoS] ) along with an increase in the interannual variability of daily precipitation in the Asian summer monsoon ( Lal et al., 2000 [MoS, SRC] ; May, 2004a; Giorgi and Bi, 2005 [JoC, MoS] ). Results of regional climate model experiments for East Asia ( Sato, 2000 [MoS] ; Emori et al., 2000 [NPR, SRC] ; Kato et al., 2000 [MoS] ; Ichikawa, 2004 [NPR] ; Japan Meteorological Agency, 2005; Kurihara et al., 2005 [MoS] ) indicate that heatwave conditions over Japan are likely to be enhanced in the future ( Figure 10.2 ). Extreme daily precipitation, including that associated with typhoon, would be further enhanced over Japan due to the increase in atmospheric moisture availability ( Hasumi and Emori, 2004 [NPR, MoS, SRC] ). The increases in annual temperature and precipitation over Japan are also projected regionally using regional climate model ( Figure 10.3 ; Japan Meteorological Agency, 2005; Kurihara et al., 2005 [MoS] ).
An increase of 10 to 20% in tropical cyclone intensities for a rise in sea-surface temperature of 2 to 4°C relative to the current threshold temperature is likewise projected in East Asia, South-East Asia and South Asia ( Knutson and Tuleya, 2004 [JoC, MoS] ). Amplification in storm-surge heights could result from the occurrence of stronger winds, with increase in sea-surface temperatures and low pressures associated with tropical storms resulting in an enhanced risk of coastal disasters along the coastal regions of East, South and South-East Asian countries. The impacts of an increase in cyclone intensities in any location will be determined by any shift in the cyclone tracks ( Kelly and Adger, 2000 [JoC] ).
In coastal areas of Asia, the current rate of sea-level rise is reported to be between 1 to 3 mm/yr which is marginally greater than the global average ( Dyurgerov and Meier, 2000 [JoC, ARC] ; Nerem and Mitchum, 2001 [NPR] ; Antonov et al., 2002 [JoC] ; Arendt et al., 2002 [JoC] ; Rignot et al., 2003 [JoC, ARC] ; Woodworth et al., 2004 [NPR, ARC] ). A rate of sea-level rise of 3.1 mm/yr has been reported over the past decade compared to 1.7 to 2.4 mm/yr over the 20th century as a whole ( Arendt et al., 2002 [JoC] ; Rignot et al., 2003 [JoC, ARC] ), which suggests that the rate of sea-level rise has accelerated relative to the long-term average.
In the SRES framework narrative storylines were developed which provide broadly qualitative and quantitative descriptions of regional changes on socio-economic development (e.g., population, economic activity), energy services and resource availability (e.g., energy intensities, energy demand, structure of energy use), land use and land cover, greenhouse gases (GHG) and sulphur emissions, and atmospheric composition (Naki?enovi? and Swart, 2000 [Ambiguous] ). In Asia, GHG emissions were quantified reflecting socio-economic development such as energy use, land-use changes, industrial production processes, and so on. The population growth projections for Asia range between 1.54 billion people in 2050 and 4.5 billion people in 2100 (Naki?enovi? and Swart, 2000 [Ambiguous] ). The economic growth is estimated to range between 4.2-fold and 3.6-fold of the current gross domestic product (GDP), respectively.
Key future climate change impacts and vulnerabilities for Asia are summarised in Figure 10.4 . A detailed discussion of these impacts and vulnerabilities are presented in the sections below.
Results of recent studies suggest that substantial decreases in cereal production potential in Asia could be likely by the end of this century as a consequence of climate change. However, regional differences in the response of wheat, maize and rice yields to projected climate change could likely be significant ( Parry et al., 1999 [JoC, ARC] ; Rosenzweig et al., 2001 [ARC] ). Results of crop yield projection using HadCM2 indicate that crop yields could likely increase up to 20% in East and South-East Asia while it could decrease up to 30% in Central and South Asia even if the direct positive physiological effects of CO2 are taken into account. As a consequence of the combined influence of fertilisation effect and the accompanying thermal stress and water scarcity (in some regions) under the projected climate change scenarios, rice production in Asia could decline by 3.8% by the end of the 21st century ( Murdiyarso, 2000 [SRC] ). In Bangladesh, production of rice and wheat might drop by 8% and 32%, respectively, by the year 2050 ( (Faisal and Parveen, 2004 ) ). For the warming projections under A1FI emission scenarios (see Table 10.5 ), decreases in crop yields by 2.5 to 10% in 2020 s and 5 to 30% in 2050 s have been projected in parts of Asia ( Parry et al., 2004 [NPR, JoC, ARC] ). Doubled CO2 climates could decrease rice yields, even in irrigated lowlands, in many prefectures in central and southern Japan by 0 to 40% ( Nakagawa et al., 2003 [NPR] ) through the occurrence of heat-induced floret sterility ( (Matsui and Omasa, 2002 ) ). The projected warming accompanied by a 30% increase in tropospheric ozone and 20% decline in humidity is expected to decrease the grain and fodder productions by 26% and 9%, respectively, in North Asia Izrael,). The projected warming accompanied by a 30% increase in tropospheric ozone and 20% decline in humidity is expected to decrease the grain and fodder productions by 26% and 9%, respectively, in North Asia Izrael,).
Crop simulation modelling studies based on future climate change scenarios indicate that substantial loses are likely in rain-fed wheat in South and South-East Asia ( Fischer et al., 2002 [NPR] ). For example, a 0.5°C rise in winter temperature would reduce wheat yield by 0.45 tonnes per hectare in India ( Lal et al., 1998 [MoS, SRC] ; Kalra et al., 2003 [NPR, SRC] ). More recent studies suggest a 2 to 5% decrease in yield potential of wheat and maize for a temperature rise of 0.5 to 1.5°C in India ( Aggarwal, 2003 [ARC] ). Studies also suggest that a 2°C increase in mean air temperature could decrease rain-fed rice yield by 5 to 12% in China ( Lin et al., 2004 [NPR, MoS, SRC] ). In South Asia, the drop in yields of non-irrigated wheat and rice will be significant for a temperature increase of beyond 2.5°C incurring a loss in farm-level net revenue of between 9% and 25% ( Lal, 2007 [NPR, SRC, 2007] ). The net cereal production in South Asian countries is projected to decline at least between 4 to 10% by the end of this century under the most conservative climate change scenario ( Lal, 2007 [NPR, SRC, 2007] ). The changes in cereal crop production potential indicate an increasing stress on resources induced by climate change in many developing countries of Asia.
Climate change can affect not only crop production per unit area but also the area of production. Most of the arable land that is suitable for cultivation in Asia is already in use ( IPCC, 2001 [NPR] ). A northward shift of agricultural zones is likely, such that the dry steppe zone in eastern part of Mongolia would push the forest-steppe to the north resulting in shrinking of the high mountainous and forest-steppe zones and expansion of the steppe and desert steppe ( Tserendash et al., 2005 [NPR, ARC] ). Studies suggest that by the middle of this century in northern China, tri-planting boundary will likely shift by 500 km from Changjiang valley to Huanghe basin, and double planting regions will move towards the existing single planting areas, while single planting areas will shrink by 23% ( (Wang, 2002 ) ). Suitable land and production potentials for cereals could marginally increase in the Russian Federation and in East Asia ( Fischer et al., 2002 [NPR] ).
More than 28 Mha in South and East Asia require a substantial increase in irrigation for sustained productivity ( FAO, 2003 [NPR] ). Agricultural irrigation demand in arid and semi-arid regions of Asia is estimated to increase by at least 10% for an increase in temperature of 1°C ( Fischer et al., 2002 [NPR] ;( Liu, 2002 ) ). The rain-fed crops in the plains of North and North-East China could face water-related challenges in coming decades, due to increases in water demands and soil-moisture deficit associated with projected decline in precipitation ( Tao et al., 2003b [MoS] ).
As land for agriculture becomes limited, the need for more food in South Asia could likely be met by increasing yields per unit of land, water, energy and time, such as through precision farming. Enhanced variability in hydrological characteristics will likely continue to affect grain supplies and food security in many nations of Asia. Intensification of agriculture will be the most likely means to meet the food requirements of Asia, which is likely to be invariably affected by projected climate change.
Consumption of animal products such as meat and poultry has increased steadily in comparison to milk and milk products-linked protein diets in the past few decades ( FAO, 2003 [NPR] ). However, in most regions of Asia (India, China, and Mongolia) pasture availability limits the expansion of livestock numbers. Cool temperate grassland is projected to shift northward with climate change and the net primary productivity will decline ( Sukumar et al., 2003 [NPR, ARC] ; Christensen et al., 2004 [JoC] ; Tserendash et al., 2005 [NPR, ARC] ). The limited herbaceous production, heat stress from higher temperature, and limited water intake due to a decrease in rainfall could cause reduced milk yields in animals and an increased incidence of some diseases.
The Asia-Pacific region is the world’s largest producer of fish, from both aquaculture and capture fishery sectors. Recent studies suggest a reduction of primary production in the tropical oceans because of changes in oceanic circulation in a warmer atmosphere. The tuna catch of East Asia and South-East Asia is nearly one-fourth of the world’s total. A modelling study showed significant large-scale changes of skipjack tuna habitat in the equatorial Pacific under projected warming scenario ( Loukos et al., 2003 [MoS] ). Marine fishery in China is facing threats from over fishing, pollution, red tide, and other climatic and environmental pressures. The migration route and migration pattern and, hence, regional catch of principal marine fishery species, such as ribbon fish, small and large yellow croakers, could be greatly affected by global climate change ( Su and Tang, 2002 [NPR] ; Zhang and Guo, 2004 [SRC] ). Increased frequency of El Niño events could likely lead to measurable declines in fish larvae abundance in coastal waters of South and South-East Asia. These phenomena are expected to contribute to a general decline in fishery production in the coastal waters of East, South and South-East Asia. Arctic marine fishery would also be greatly influenced by climate change. Moderate warming is likely to improve the conditions for some economically gainful fisheries, such as cod and herring. Higher temperatures and reduced ice cover could increase productivity of fish-prey and provide more extensive habitats. In contrast, the northern shrimp will likely decrease with rise in sea-surface temperatures ( ACIA, 2005 [NPR] ).
The impact of climate change on Asian fishery depends on the complicated food chains in the surrounding oceans, which are likely to be disturbed by the climate change. Fisheries at higher elevations are likely to be adversely affected by lower availability of oxygen, due to a rise in surface air temperatures. In the plains, the timing and amount of precipitation could also affect the migration of fish species from the river to the floodplains for spawning, dispersal and growth ( FAO, 2003 [NPR] ). Future changes in ocean currents, sea level, sea-water temperature, salinity, wind speed and direction, strength of upwelling, the mixing layer thickness and predator response to climate change have the potential to substantially alter fish breeding habitats and food supply for fish and ultimately the abundance of fish populations in Asian waters ( IPCC, 2001 [NPR] ).
Half the world’s population is located in Asia. There are serious concerns about the prevalence of malnutrition among poorer and marginal groups, particularly rural children, and about the large number of people below the poverty line in many countries. Large uncertainties in our understanding as to how the regional climate change will impact the food supply and demand in Asia continue to prevail in spite of recent scientific advances. Because of increasing interdependency of global food system, the impact of climate change on future food supply and demand in Asia as a whole as well as in countries located in the region depends on what happens in other countries. For example, India’s surplus grain in past few years has been used to provide food aid to drought-affected Cambodia ( Fischer et al., 2002 [NPR] ). However, increasing urbanisation and population in Asia will likely result in increased food demand and reduced supply due to limited availability of cropland area and yield declines projected in most cases ( Murdiyarso, 2000 [SRC] ;( Wang, 2002; ) Lin et al., 2004 [NPR, MoS, SRC] ).
Food supply or ability to purchase food directly depends on income and price of the products. The global cereal prices have been projected to increase more than three-fold by the 2080 s as a consequence of decline in net productivity due to projected climate change ( Parry et al., 2004 [NPR, JoC, ARC] ). Localised increases in food prices could be frequently observed. Subsistence producers growing crops, such as sorghum, millet, etc., could be at the greatest risk, both from a potential drop in productivity as well as from the danger of losing crop genetic diversity that has been preserved over generations. The risk of hunger, thus, is likely to remain very high in several developing countries with an additional 49 million, 132 million and 266 million people of Asia projected under A2 scenario without carbon fertilisation that could be at risk of hunger by 2020, 2050 and 2080, respectively ( Parry et al., 2004 [NPR, JoC, ARC] ). In terms of percent increase in risk hunger, it is projected under A2 scenario without CO2 fertilisation that an increase of 7 to 14% by 2020 s, 14 to 40% by 2050 s and 14 to 137% by 2080 s are likely ( Parry et al., 2004 [NPR, JoC, ARC] ).
Some recent studies ( PAGASA, 2001 [NPR] ; Sukumar et al., 2003 [NPR, ARC] ; Batima et al., 2005b [NPR, ARC] ) confirm TAR findings that grasslands, livestock and water resources in marginal areas of Central Asia and South-East Asia are likely to be vulnerable to climate change. Food insecurity and loss of livelihood are likely to be further exacerbated by the loss of cultivated land and nursery areas for fisheries by inundation and coastal erosion in low-lying areas of the tropical Asia. Management options, such as better stock management and more integrated agro-ecosystems could likely improve land conditions and reduce pressures arising from climate change.
Some studies ( Rosenzweig et al., 2001 [ARC] ; FAO, 2004c [NPR] ) agree that higher temperatures and longer growing seasons could result in increased pest populations in temperate regions of Asia. CO2 enrichment and changes in temperature may also affect ecology, the evolution of weed species over time and the competitiveness of C3 v. C4 weed species ( Ziska, 2003 [MoS] ). Warmer winter temperatures would reduce winter kill, favouring the increase of insect populations. Overall temperature increases may influence crop pathogen interactions by speeding up pathogen growth rates which increases reproductive generations per crop cycle, by decreasing pathogen mortality due to warmer winter temperatures, and by making the crop more vulnerable.
Climate change, as well as changing pest and disease patterns, will likely affect how food production systems perform in the future. This will have a direct influence on food security and poverty levels, particularly in countries with a high dependency on agriculture. In many cases, the impact will likely be felt directly by the rural poor, as they are often closely linked to direct food systems outcomes for their survival and are less able to substitute losses through food purchases. The urban poor are also likely to be affected negatively by an increase in food prices that may result from declining food production.
The impacts of climate change on water resources in Asia will be positive in some areas and negative in others. Changes in seasonality and amount of water flows from river systems are likely to occur due to climate change. In some parts of Russia, climate change could significantly alter the variability of river runoff such that extremely low runoff events may occur much more frequently in the crop growing regions of the south west ( Peterson et al., 2002 [PoC, JoC, ARC] ). Changes in runoff of river basins could have a significant effect on the power output of hydropower generating countries like Tajikistan, which is the third-highest producer in the world (World Bank, 2002 [NPR] ). Likewise, surface water availability from major rivers like the Euphrates and Tigris may also be affected by alteration of riverflows. In Lebanon the annual net usable water resources will likely decrease by 15% in response to a general circulation model (GCM) estimated average rise in temperature of 1.2°C under doubled CO2 climate, while the flows in rivers are likely to increase in winter and decrease in spring ( (Bou-Zeid and El-Fadel, 2002 ) ) which could negatively affect existing uses of river waters. In North China, irrigation from surface and groundwater sources will meet only 70% of the water requirement for agricultural production, due to the effects of climate change and increasing demand ( Liu et al., 2001 [Ambiguous] ; Qin, 2002 [NPR, MoS] ). The maximum monthly flow of the Mekong is estimated to increase by 35 to 41% in the basin and by 16 to 19% in the delta, with lower value estimated for years 2010 to 38 and higher value for years 2070 to 99, compared with 1961 to 90 levels. In contrast, the minimum monthly flows are estimated to decline by 17 to 24% in the basin and 26 to 29% in the delta (see Chapter 5 , Box 5.3 Hoanh et al., 2004 [NPR] ) suggesting that there could be increased flooding risks during wet season and an increased possibility of water shortage in dry season. Flooding could increase the habitat of brackish water fisheries but could also seriously affect the aquaculture industry and infrastructure, particularly in heavily-populated megadeltas. Decrease in dry season flows may reduce recruitment of some species.
In parts of Central Asia, regional increases in temperature will lead to an increased probability of events such as mudflows and avalanches that could adversely affect human settlements ( (Iafiazova, 1997 ) ). Climate change-related melting of glaciers could seriously affect half a billion people in the Himalaya-Hindu-Kush region and a quarter of a billion people in China who depend on glacial melt for their water supplies ( Stern, 2007 [NPR, 2007] ). As glaciers melt, river runoff will initially increase in winter or spring but eventually will decrease as a result of loss of ice resources. Consequences for downstream agriculture, which relies on this water for irrigation, will be likely unfavourable in most countries of South Asia. The thawing volume and speed of snow cover in spring is projected to accelerate in North-West China and Western Mongolia and the thawing time could advance, which will increase some water sources and may lead to floods in spring, but significant shortages in wintertime water availability for livestock are projected by the end of this century ( Batima et al., 2004 [NPR, ARC] , 2005b ).
Over-exploitation of groundwater in many countries of Asia has resulted in a drop in its level, leading to ingress of sea water in coastal areas making the sub-surface water saline. India, China and Bangladesh are especially susceptible to increasing salinity of their groundwater as well as surface water resources, especially along the coast, due to increases in sea level as a direct impact of global warming ( (Han et al., 1999 ) ). Rising sea level by 0.4 to 1.0 m can induce salt-water intrusion 1 to 3 km further inland in the Zhujiang estuary ( Huang and Xie, 2000 [NPR] ). Increasing frequency and intensity of droughts in the catchment area will lead to more serious and frequent salt-water intrusion in the estuary ( Xu, 2003 [NPR] ; Thanh et al., 2004 [SRC] ; Huang et al., 2005 [NPR, SRC] ) and thus deteriorate surface and groundwater quality.
Expansion of areas under severe water stress will be one of the most pressing environmental problems in South and South-East Asia in the foreseeable future as the number of people living under severe water stress is likely to increase substantially in absolute terms. It is estimated that under the full range of SRES scenarios, 120 million to 1.2 billion, and 185 to 981 million people will experience increased water stress by the 2020 s, and the 2050 s, respectively ( Arnell, 2004 [JoC, ARC] ). The decline in annual flow of the Red River by 13 to 19% and that of Mekong River by 16 to 24% by the end of 21st century will contribute in increasing water stress ( ADB, 1994 [NPR] ).
Global warming would cause an abrupt rise of water quantity as a result of snow or glacier melting that, in turn, would lead to floods. The floods quite often are caused by rise of river water level due to blockage of channels by drifting ice, as happened in Central Siberia, Lensk, or enormous precipitation from destructive shower cyclones, as it was in the North Asia Pacific coast, Vladivostok ( Izrael et al., 2002a [NPR] ). A projected increase in surface air temperature in North-West China will result in a 27% decline in glacier area (equivalent to the ice volume of 16,184 km3), a 10 to 15% decline in frozen soil area, an increase in flood and debris flow, and more severe water shortages ( Qin, 2002 [NPR, MoS] ). The duration of seasonal snow cover in alpine areas, namely the Tibetan Plateau, Xinjiang and Inner Mongolia of China, will shorten and snow cover will thaw out in advance of the spring season, leading to a decline in volume and resulting in severe spring droughts. Between 20 to 40% reduction of runoff per capita in Ningxia, Xinjiang and Qinghai Province is likely by the end of 21st century ( Tao et al., 2005 [JoC] ). However, the pressure due to increasing population and socio-economic development on water resources is likely to grow. ( Higashi et al. 2006 ) ) project that future flood risk in Tokyo, Japan between 2050 to 2300 under SRES A1B is likely to be 1.1 to 1.2 times higher than the present condition.
The gross per capita water availability in India will decline from about 1,820 m3/yr in 2001 to as low as about 1,140 m3/yr in 2050 ( (Gupta and Deshpande, 2004 ) ). India will reach a state of water stress before 2025 when the availability falls below 1000 m3 per capita ( CWC, 2001 [NPR] ). The projected decrease in the winter precipitation over the Indian subcontinent would reduce the total seasonal precipitation during December, January and February implying lesser storage and greater water stress during the lean monsoon period. Intense rain occurring over fewer days, which implies increased frequency of floods during the monsoon, will also result in loss of the rainwater as direct runoff, resulting in reduced groundwater recharging potential.
Average global sea-level rise over the second half of the 20th century was 1.8 ± 0.3 mm/yr, and sea-level rise of the order of 2 to 3 mm/yr is considered likely during the early 21st century as a consequence of global warming ( Woodroffe et al., 2006 [NPR, SRC] ). However, the sea-level rise in Asia is geographically variable and an additional half a metre of sea-level rise is projected for the Arctic during this century ( ACIA, 2005 [NPR] ). The rising rates of sea level vary considerably from 1.5 to 4.4 mm/yr along the East Asia coast, due to regional variation in land surface movement ( Mimura and Yokoki, 2004 [NPR, ARC] ). The projected rise of mean high-water level could be greater than that of mean sea level ( (Chen, 1991; ) ( Zhang and Du, 2000 ) ). The projected relative sea-level rise (RSLR), including that due to thermal expansion, tectonic movement, ground subsidence and the trend of rising river water level, is 40 to 60 cm, 50 to 70 cm and 70 to 90 cm in the Zhujiang, Changjiang and Huanghe Deltas, respectively by the year 2050 ( Li et al., 2004a [SRC] , b). ( Choi et al. 2002 ) ) has reported that the regional sea-level rise over the north-western Pacific Ocean would be much more significant compared with the global average mainly due to exceptionally large warming near the entrance of the Kuroshio extension. The slope of the land and land surface movement would also affect the relative sea-level rise in the Asian Arctic ( ACIA, 2005 [NPR] ).
In Asia, erosion is the main process that will occur to land as sea level continues to rise. As a consequence, coast-protection structures built by humans will usually be destroyed by the sea while the shoreline retreats. In some coastal areas of Asia, a 30 cm rise in sea level can result in 45 m of landward erosion. Climate change and sea-level rise will tend to worsen the currently eroding coasts ( Huang and Xie, 2000 [NPR] ). In Boreal Asia, coastal erosion will be enhanced as rising sea level and declining sea ice allow higher wave and storm surge to hit the shore ( ACIA, 2005 [NPR] ). The coastal recession can add up to 500 to 600 m in 100 years, with a rate of between 4 to 6 m/yr. The coastal recession by thermal abrasion is expected to accelerate by 1.4 to 1.5 times in the second half of the 21st century as compared to the current rate ( Leont’yev, 2004 [MoS] ). In monsoonal Asia, decreasing sediment flux is generally a main cause of coastal erosion. Available evidence suggests a tendency of river sediment to further decline that will tend to worsen coastal erosion in Asia ( Liu et al., 2001 [Ambiguous] ).
Projected sea-level rise could flood the residence of millions of people living in the low lying areas of South, South-East and East Asia such as in Vietnam, Bangladesh, India and China ( Wassmann et al., 2004 [JoC] ; Stern, 2007 [NPR, 2007] ). Even under the most conservative scenario, sea level will be about 40 cm higher than today by the end of 21st century and this is projected to increase the annual number of people flooded in coastal populations from 13 million to 94 million. Almost 60% of this increase will occur in South Asia (along coasts from Pakistan, through India, Sri Lanka and Bangladesh to Burma), while about 20% will occur in South-East Asia, specifically from Thailand to Vietnam including Indonesia and the Philippines ( Wassmann et al., 2004 [JoC] ). The potential impacts of one metre sea-level rise include inundation of 5,763 km2 and 2,339 km2 in India and in some big cities of Japan, respectively ( TERI, 1996 [NPR] ; Mimura and Yokoki, 2004 [NPR, ARC] ). For one metre sea-level rise with high tide and storm surge, the maximum inundation area is estimated to be 2,643 km2 or about 1.2% of total area of the Korean Peninsula ( Matsen and Jakobsen, 2004 [MoS] ). In China, a 30 cm sea-level rise would inundate 81,348 km2 of coastal lowland ( (Du and Zhang, 2000 ) ).
The coastal lowlands below the elevation of 1,000-year storm surge are widely distributed in Bangladesh, China, Japan, Vietnam and Thailand, where millions of people live ( Nicholls, 2004 [JoC, ARC] ). In Japan, an area of 861 km2 of coastal lowland is located below high water level mainly in large cities like Tokyo, Osaka and Nagoya. A one metre rise in sea level could put up to 4.1 million people at risk ( Mimura and Yokoki, 2004 [NPR, ARC] ). Using a coarse digital terrain model and global population distribution data, it is estimated that more than 1 million people will be directly affected by sea-level rise in 2050 in each of the Ganges-Brahmaputra-Meghna delta in Bangladesh, the Mekong delta in Vietnam and the Nile delta in Egypt (see Chapter 6 , Box 6.3 ( Ericson et al., 2005 ) ). Damages in flooded areas are largely dependent on the coastal protection level. It can be much less in highly protected coasts like in Japan but can be very high such as in coastal areas of South Asia where the protection level is low. A 30 cm rise in sea level will increase coastal flooding areas by five or six times in both the ‘with’ and ‘without protection’ scenarios in the Changjiang and Zhujiang deltas. Similarly, the flooding areas in the Huanghe delta for a 100 cm rise in sea level are almost the same under the ‘without protection’ and ‘existing protection’ scenarios. These two cases indicate that the current protection level is insufficient to protect the coasts from high sea-level rise ( (Du and Zhang, 2000; ) Li et al., 2004a [SRC] ). Further climate warming may lead to an increase in tropical cyclone destructive potential, and with an increasing coastal population substantial increase in hurricane-related losses in the 21st century is likely ( Emanuel, 2005 [JoC] ).
In summary, all coastal areas in Asia are facing an increasing range of stresses and shocks, the scale of which now poses a threat to the resilience of both human and environmental coastal systems, and are likely to be exacerbated by climate change. The projected future sea-level rise could inundate low lying areas, drown coastal marshes and wetlands, erode beaches, exacerbate flooding and increase the salinity of rivers, bays and aquifers. With higher sea level, coastal regions would also be subject to increased wind and flood damage due to storm surges associated with more intense tropical storms. In addition, warming would also have far reaching implications for marine ecosystems in Asia.
Future evolution of the major deltas in monsoonal Asia depends on changes in ocean processes and river sediment flux. Coastal erosion of the major deltas will be caused by sea-level rise, intensifying extreme events (e.g., storm surge) due to climate change and excessive pumping of groundwater for irrigation and reservoir construction upstream. In the Tibetan Plateau and adjoining region, sediment starvation is generally the main cause of shrinking of deltas. Annual mean sediment discharge in the Huanghe delta during the 1990 s was only 34% of that observed during the 1950 s and 1970 s. The Changjiang sediment discharge will also be reduced by 50% on average after construction of the Three-Gorges Dam ( Li et al., 2004b [SRC] ). Saltwater intrusion in estuaries due to decreasing river runoff can be pushed 10 to 20 km further inland by the rising sea level ( Shen et al., 2003 [NPR] ; Yin et al., 2003 [NPR] ; Thanh et al., 2004 [SRC] ).
Many megacities in Asia are located on deltas formed during sea-level change in the Holocene period ( (Hara et al., 2005 ) ). These Asian megacities with large populations and intensified socio-economic activities are subject to threats of climate change, sea-level rise and extreme climate event. For a 1 m rise in sea level, half a million square hectares of Red River delta and from 15,000 to 20,000 km2 of Mekong River delta is projected to be flooded. In addition, 2,500 km2 of mangrove will be completely lost, while approximately 1,000 km2 of cultivated farm land and sea product culturing area will become salt marshes ( Tran et al., 2005 [NPR] ).
Rise in water temperatures and eutrophication in the Zhujiang and Changjiang estuaries have led to the formation of the bottom oxygen-deficient horizon and an increase in the frequency and intensity of red tides ( Hu et al., 2001 [NPR] ). Projected increases in the frequency and intensity of extreme weather events will exert adverse impacts on aquatic ecosystems, and existing habitats will be redistributed, affecting estuarine flora distribution ( (Short and Neckles, 1999; ) ( Simas et al., 2001; ) Lu, 2003 [NPR] ;( Paerl et al., 2003 ) ).
Recent risk analysis of coral reefs suggests that between 24% and 30% of the reefs in Asia are projected to be lost during the next 2 to 10 years and 10 to 30 years, respectively (14% and 18% for global), unless the stresses are removed and relatively large areas are protected ( Table 10.6 ). In other words, the loss of reefs in Asia may be as high as 88% (59% for global) in the next 30 years under IS92a emission scenario ( IPCC, 1992 [NPR] ; Sheppard, 2003 [JoC, MoS] ; Wilkinson, 2004 [NPR, ARC] ). If conservation measures receive increasing attention, large areas of the reefs could recover from the direct and indirect damage within the next 10 years. However, if abnormally high sea-surface temperatures (SST) continue to cause major bleaching events (see Chapter 6 , Section 6.2.5 , Box 6.1 ), and reduce the capacity of reefs to calcify due to CO2 increase, most human efforts will be futile ( Kleypas et al., 1999 [JoC] ; Wilkinson, 2002 [NPR] ).
|Region||Coral reef area (km2)||Destroyed reefs (%)||Reefs recovered||Reefs at critical||Reefs at threatened||Reefs at low or no|
|since 1998 (%)||stage (%)||stage (%)||threat level (%)|
|E & N Asia||5,400||14||3||23||12||51|
A new study suggests that coral reefs, which have been severely affected by abnormally high SST in recent years, contain some coral species and their reef-associated micro-algal symbionts that show far greater tolerance to higher SST than others. Bleaching thresholds may be more realistically visualised as a broad spectrum of responses, rather than a single bleaching threshold for all coral species ( Hughes et al., 2003 [JoC, ARC] ; Baker et al., 2004 [JoC] ). This corals’ adaptive response to climate change may protect devastated reefs from extinction or significantly prolong the extinction of surviving corals beyond previous assumption.
Net growth rates of coral reef, which can reach up to 8 to 10 mm/year, may exceed the projected rates of future sea-level rise in the South China Sea, so that coral reefs could not be at risk due merely to sea-level rise. Water depth increased by sea-level rise would lead to storminess and destruction of coral reefs ( Knowlton, 2001 [JoC, MoS] ;( Wang, 2005 ) ).
Up to 50% of the Asia’s total biodiversity is at risk due to climate change. Boreal forests in North Asia would move further north. A projected large increase in taiga is likely to displace tundra, while the northward movement of the tundra will in turn decrease polar deserts (see Chapter 15 , Section 15.2.2 , Figure 15.3 Callaghan et al., 2005 [NPR, ARC] ; Juday et al., 2005 [NPR] ). Large populations of many other species could also be extirpated as a result of the synergistic effects of climate change and habitat fragmentation ( Ishigami et al., 2003 [MoS] , 2005 ). Projections under doubled-CO2 climate using two GCMs show that 105 to 1,522 plant species and 5 to 77 vertebrates in China and 133 to 2,835 plants and 10 to 213 vertebrates in Indo-Burma could become extinct ( Malcolm et al., 2006 [ARC] ).
As a consequence of climate change, no significant change in spatial patterns of productivity of the forest ecosystems in North-East China is projected ( Liu et al., 1998 [MoS] ). The areal coverage of broad-leaved Korean pine forests is projected to decrease by 20 to 35% with a significant northward shift ( (Wu, 2003 ) ). About 90% of the suitable habitat for a dominant forest species, beech tree (Fagus crenata), in Japan could disappear by the end of this century ( Matsui et al., 2004a [MoS] , b). The impact of elevated atmospheric CO2 on plant biomass production is influenced by the availability of soil nitrogen and deposition of atmospheric nitrogen ( Oren et al., 2001 [JoC] ; Hajima et al., 2005 [MoS] ;( Kitao et al., 2005; ) Reich et al., 2006 [JoC] ). The overall impact of climate change on the forest ecosystems of Pakistan could be negative ( (Siddiqui et al., 1999 ) ).
The observations in the past 20 years show that the increasing intensity and spread of forest fires in North and South-East Asia were largely related to rises in temperature and declines in precipitation in combination with increasing intensity of land uses (see Section 10.2.4.4 ). Whether this trend will persist in the future or not is difficult to ascertain in view of the limited literature on how the frequency and severity of forest and brush fires will likely respond to expected increase in temperature and precipitation in North and South-East Asia (see Section 10.3.1 ). The uncertainty lies on whether the expected increase in temperature would be enough to trigger more frequent and severe fires despite the projected increase in precipitation. One study on the impacts of climate change on fires show that for an average temperature increase of 1°C, the duration of wild fire season in North Asia could increase by 30% ( Vorobyov, 2004 [NPR] ), which could have varying adverse and beneficial impacts on biodiversity, forest structure and composition, outbreaks of pest and diseases, wildlife habitat quality and other key forest ecosystem functions.
The natural grassland coverage and the grass yield in Asia, in general, are projected to decline with a rise in temperature and higher evaporation ( Lu and Lu, 2003 [ARC] ). Large decreases in the natural capital of grasslands and savannas are likely in South Asia as a consequence of climate change. A rise in surface air temperature and decline in precipitation is estimated to reduce pasture productivity in the Mongolian steppe by about 10 to 30%, except in high mountains and in Gobi where a marginal decrease in pasture productivity is projected by the end of this century ( Tserendash et al., 2005 [NPR, ARC] ). Traditional land-use systems should provide conditions that would promote greater rangeland resilience and provide a better management strategy to cope with climate change in the region to offset the potential decrease of carbon storage and grassland productivity in the Mongolian Steppe under various climate scenarios (Ojima et al., 1998 [NotFound] ).
The location and areas of natural vegetation zone on the Tibetan Plateau will substantially change under the projected climate scenarios. The areas of temperate grassland and cold-temperate coniferous forest could expand, while temperate desert and ice-edge desert may shrink. The vertical distribution of vegetation zone could move to higher altitude. Climate change may result in a shift of the boundary of the farming-pastoral transition region to the south in North-East China, which can increase the grassland areas and provide favourable conditions for livestock production. However, as the transition area of farming-pastoral region is also the area of potential desertification, if protection measures are not taken in the new transition area, desertification may occur ( (Li and Zhou, 2001; ) ( Qiu et al., 2001 ) ). More frequent and prolonged droughts as a consequence of climate change and other anthropogenic factors together will result in the increasing trends of desertification in Asia.
The permafrost thawing will continue over vast territories of North Asia under the projected climate change scenarios ( Izrael et al., 2002b [SRC] ). The transient climate model simulations ( Pavlov and Ananjeva-Malkova, 2005 [NPR] ; FNCRF, 2006 [NPR] ) show that the perennially frozen rocks and soils (eastern part of the permafrost terrain) and soils (western part of the terrain) may be completely degraded within the present southern regions of North Asia (see Figure 10.5 ). In northern regions, mean annual temperature of frozen soil and rocks and the depth of seasonal thawing will increase in 2020 by as much as 4°C for the depth of 0.8 m and by at most 2.2°C for the depth of 1.6 m ( FNCRF, 2006 [NPR] ; Izrael et al., 2006 [NPR] ). The change in the rock and soil temperatures will result in a change in the strength characteristics, bearing capacity, and compressibility of the frozen rocks and soils, thaw settlement strains, frozen ground exploitability in the course of excavation and mining, generation of thermokarst, thermal erosion and some other geocryological processes (Climate Change, 2004 ).
Permafrost degradation will lead to significant ground surface subsidence and pounding ( (Osterkamp et al., 2000; ) Jorgenson et al., 2001 [JoC] ). Permafrost thawing on well-drained portions of slopes and highlands in Russia and Mongolia will improve the drainage conditions and lead to a decrease in the groundwater content ( Hinzman et al., 2003 [NPR] ; Batima et al., 2005b [NPR, ARC] ). On the Tibetan Plateau, in general, the permafrost zone is expected to decrease in size, move upward and face degradation by the end of this century ( Wu et al., 2001 [MoS, ARC] ). For a rise in surface temperature of 3°C and no change in precipitation, most Tibetan Plateau glaciers shorter than 4 km in length are projected to disappear and the glacier areas in the Changjiang Rivers will likely decrease by more than 60% ( Shen et al., 2002 [MoS, ARC] ).
10.4.5 Human health
Climate change poses substantial risks to human health in Asia. Global burden (mortality and morbidity) of climate-change attributable diarrhoea and malnutrition are already the largest in South-East Asian countries including Bangladesh, Bhutan, India, Maldives, Myanmar and Nepal in 2000, and the relative risks for these conditions for 2030 is expected to be also the largest ( McMichael et al., 2004 [NPR, ARC] ), although in some areas, such as southern states in India, there will be a reduction in the transmission season by 2080 ( Mitra et al., 2004 [NPR] ). An empirical model projected that the population at risk of dengue fever (the estimated risk of dengue transmission is greater than 50%) will be larger in India and China ( Hales et al., 2002 [MoS, ARC] ). Also in India and China, the excess mortality due to heat stress is projected to be very high ( Takahashi et al., 2007 [MoS, SRC, 2007] ), although this projection did not take into account possible adaptation and population change. There is already evidence of widespread damage to human health by urban air quality and enhanced climate variability in Asia. Throughout newly industrialised areas in Asia, such as Chongqing, China, and Jakarta, Indonesia, air quality has deteriorated significantly and will likely contribute to widespread heat stress and smog induced cardiovascular and respiratory illnesses in the region ( Patz et al., 2000 [ARC] ). Also, the number of patients of Japanese cedar pollen disease is likely to increase when the summer temperature rises ( Takahashi and Kawashima, 1999 [MoS] ;( Teranishi et al., 2000 ) ).
The negative influence of temperature anomalies on public health has been established in Russia ( Izmerov et al., 2004 [NPR, ARC] ) and in the semi-arid city, Beirut ( (El-Zein et al., 2004 ) ). Exposure to higher temperatures appears to be a significant risk factor for cerebral infarction and cerebral ischemia during the summer months ( Honda et al., 1995 [SRC] ). Natural habitats of vector-borne diseases are reported to be expanding ( Izmerov et al., 2004 [NPR, ARC] ). Prevalence of malaria and tick-borne encephalitis has also increased over time in Russia ( Yasukevich and Semenov, 2004 [NPR, ARC] ). The distribution of vector-borne infectious diseases such as malaria is influenced by the spread of vectors and the climate dependence of the infectious pathogens. There are reports on the possible effects of pesticide resistance of a certain type of mosquito on the transition of malaria type ( (Singh et al., 2004 ) ). The insect-borne infectious diseases strongly modulated by future climate change include malaria, schistosomiasis, dengue fever and other viral diseases ( (Kovats et al., 2003 ) ). Oncomelania is strongly influenced by climate and the infection rate of schistosomiasis is the highest in the temperature range of 24°C to 27°C. Temperature can directly influence the breeding of malaria protozoa and suitable climate conditions can intensify the invasiveness of mosquito ( (Tong and Ying, 2000 ) ). A warmer and more humid climate would be favourable for propagation and invasiveness of infectious insect vector. Serious problems are connected with the impact of air pollution due to Siberian forest fires on human health ( Rachmanin et al., 2004 [NPR] ).
Warmer sea-surface temperatures along coastlines of South and South-East Asia would support higher phytoplankton blooms. These phytoplankton blooms are excellent habitats for survival and spread of infectious bacterial diseases such as cholera ( (Pascual et al., 2002 ) ). Water-borne diseases including cholera and the suite of diarrhoeal diseases caused by organisms such as Giardia, Salmonella and Cryptosporidium could also become common with the contamination of drinking water. Precipitation increase and frequent floods, and sea-level rise in the future will degrade the surface water quality owing to more pollution and, hence, lead to more water-borne infectious diseases such as dermatosis, cardiovascular disease and gastrointestinal disease. For preventive actions, assessment of climate change impacts on nutritional situation, drinking water supply, water salinity and ecosystem damage will be necessary. The risk factor of climate-related diseases will depend on improved environmental sanitation, the hygienic practice and medical treatment facilities.
Study of social vulnerability provides a complementary approach to the study of climate impacts based on model projections and biophysical simulations. Adger et al. 2001 [NPR] ) illustrate the approach through theoretical discussion and case studies based in Vietnam. The following sections detail specific examples of the human dimension of general relevance within Asia.
As of mid- 2000, over 3.6 billion people, roughly three-fifths of the total population of the globe, resided in Asia. Seven of the world’s 10 most populous countries - China, India, Indonesia, Russia, Pakistan, Bangladesh and Japan - are located within Asia ( ADB, 2002 [NPR] ). The majority of the region’s population growth is forecast to come from South Asia, which expects to add 570 million people in India, 200 million in Pakistan and 130 million in Bangladesh over the next 50 years ( UN-DESA-PD, 2002 [NPR] ). Population growth, particularly in countries with already high population densities, is inextricably associated with the increasing pressure on the natural resources and the environment as the demands for goods and services expand. Some of the key impacts of increasing population include those linked with the intensification of use of natural forests including mangroves, agriculture, industrialisation and urbanisation. In Asia, the pressure on land in the 21st century will increase, due to the increasing food grain demand for the growing population, the booming economic development, as well as climate change. This will be exacerbated by the increasing scarcity of arable lands as a result of using vast agricultural lands to support industrialisation and urbanisation in pursuit of economic development ( (Zeqiang et al., 2001 ) ).
In the developing regions, the remaining natural flood plains are disappearing at an accelerating rate, primarily as a result of changes in land use and hydrological cycle, particularly changes in streamflows due to climatic and human-related factors. The future increase of human population will lead to further degradation of riparian areas, intensification of the land and water use, increase in the discharge of pollutants, and further proliferation of species invasions. The most threatened flood plains will be those in South and South-East Asia.
In some parts of South-East Asia, population growth, particularly in the uplands, continues to exert pressure on the remaining forests in the region. Encroachment into forest zones for cultivation, grazing, fuel wood and other purposes has been a major cause of changes in natural forests. In the Philippines, forest degradation has been attributed partly to upland farming ( Pulhin et al., 2006 [NPR, ARC] ).
Development, to a large extent, is responsible for much of the greenhouse gases emitted into the atmosphere that drives climate change. On the other hand, development greatly contributes in reducing vulnerability to climate change and in enhancing the adaptive capacity of vulnerable sectors.
Demands for biological resources caused by population and increased consumption have grown with increasing economy and fast development all over Asia in recent years. Rates of both total forest loss and forest degradation are higher in Asia than anywhere else in the world. The conversion of forested area to agriculture in Asia during the past two decades occurred at a rate of 30,900 km2/yr. In many developing countries of Asia, small scale fuel wood collection and industrial logging for exports of timber and conversion of forests into estate crop plantation (i.e., oil palm) and mining are also responsible for deforestation. It is likely that climate change would aggravate the adverse impacts of forest cover loss.
In Asia, migration accounts for 64% of urban growth ( Pelling, 2003 [NPR] ). Total population, international migration and refugees in Asia and the Pacific region are currently estimated to be 3,307 million, 23 million, and 4.8 million, respectively ( UN-HABITAT, 2004 [NPR] ). Future climate change is expected to have considerable impacts on natural resource systems, and it is well-established that changes in the natural environment can affect human sustenance and livelihoods. This, in turn, can lead to instability and conflict, often followed by displacement of people and changes in occupancy and migration patterns ( Barnett, 2003 [JoC] ).
Climate-related disruptions of human populations and consequent migrations can be expected over the coming decades. Such climate-induced movements can have effects in source areas, along migration routes and in the receiving areas, often well beyond national borders. Periods when precipitation shortfalls coincide with adverse economic conditions for farmers (such as low crop prices) would be those most likely to lead to sudden spikes in rural-to-urban migration levels in China and India. Climatic changes in Pakistan and Bangladesh would likely exacerbate present environmental conditions that give rise to land degradation, shortfalls in food production, rural poverty and urban unrest. Circular migration patterns, such as those punctuated by shocks of migrants following extreme weather events, could be expected. Such changes would likely affect not only internal migration patterns, but also migration movements to other western countries.
Food can be produced on currently cultivated land if sustainable management and adequate inputs are applied. Attaining this situation would also require substantial improvements of socio-economic conditions of farmers in most Asian countries to enable access to inputs and technology. Land degradation, if continued unchecked, may further exacerbate land scarcities in some countries of Asia. Concerns for the environment as well as socio-economic considerations may infringe upon the current agricultural resource base and prevent land and water resources from being developed for agriculture ( Tao et al., 2003b [MoS] ). The production losses due to climate change may drastically increase the number of undernourished in several developing countries in Asia, severely hindering progress against poverty and food insecurity ( Wang et al., 2006 [Ambiguous] ).
The compounding influence of future rises in temperature due to global warming, along with increases in temperature due to local urban heat-island effects, makes cities more vulnerable to higher temperatures than would be expected due to global warming alone ( Kalnay and Cai, 2003 [JoC] ; Patz et al., 2005 [JoC, ARC] ). Existing stresses in urban areas include crime, traffic congestion, compromised air and water quality, and disruptions due to development and deterioration of infrastructure. Climate change is likely to amplify some of these stresses ( Honda et al., 2003 [SRC] ), although much of the interactions are not yet well understood. For example, it has been suggested that climate change will exacerbate the existing heat-island phenomenon in cities of Japan by absorbing increased solar radiation ( (Shimoda, 2003 ) ). This will lead to further increases in temperatures in urban areas with negative implications for energy and water consumption, human health and discomfort, and local ecosystems. Vulnerabilities of urban communities in megacities of Asia to long-term impacts of projected climate change need to be assessed in terms of energy, communication, transportation, water run-off and water quality, as well as the interrelatedness of these systems, and implications for public health ( McMichael et al., 2003 [NPR, ARC] ).
Nature-based tourism is one of the booming industries in Asia, especially ski resorts, beach resorts and ecotourist destinations which are likely vulnerable to climate change; yet only a few assessment studies are on hand for this review. Fukushima et al. 2002 [SRC] ) reported a drop of more than 30% in skiers in almost all ski areas in Japan except in the northern region (Hokkaido) and high altitude regions (centre of the Main Island) in the event of a 3°C increase in air temperature. If the mean June to August temperature rises by 1°C in Japan, consumption of summer products such as air-conditioners, beer, soft drinks, clothing and electricity are projected to increase about 5% ( Harasawa and Nishioka, 2003 [NPR, SRC] ). Table 10.7 lists a summary of projected impacts of global warming on industries and energy sectors identified in Japan.
Limited studies on the impacts of climate change on the energy sector in Asia suggest that this sector will be affected by climate change. In particular, South Asia is expected to account for one-fifth of the world’s total energy consumption by the end of 21st century ( Parikh and Bhattacharya, 2004 [NPR] ). An increase in the energy consumption of industry, residential and transport sectors could be significant as population, urbanisation and industrialisation rise. It is likely that climate change will influence the pattern of change in energy consumption that could have significant effects on CO2 emission in this region.
|Changes in climate parameters||Impacts|
|1°C temperature increase in June to August||About 5% increase of consumption of summer products|
|Extension of high temperature period||Increase of consumption of air-conditioners, beer, soft drinks, ice creams|
|Increase in thunder storms||Damage to information devices and facilities|
|1°C temperature increase in summer||Increase in electricity demand by about 5 million kW Increase in electricity demand in factories to enhance production|
|Increase in annual average temperature||Increase of household electricity consumption in southern Japan Decrease in total energy consumption for cooling, warming in northern Japan|
|Change in amount and pattern of rainfall||Hydroelectric power generation, management and implementation of dams, cooling water management|
|1°C increase in cooling water temperature||0.2 to 0.4% reduction of generation of electricity in thermal power plants, 1 to 2% reduction in nuclear power plant|
The cost of damages from floods, typhoons and other climate-related hazards will likely increase in the future. According to the European insurer Munich Re, the annual cost of climate change-related claims could reach US$300 billion annually by 2050 . The Association of British Insurers examined the financial implications of climate change through its effects on extreme storms (hurricanes, typhoons and windstorms) using an insurance catastrophe model ( ABI, 2005 [NPR] ). Annual insured losses from hurricanes in United States, typhoons in Japan and windstorms in Europe are projected to increase by two-thirds to US$27 billion by the 2080 s. The projected increase in insured losses due to the most extreme storms (with current return periods of 100 to 250 years) by the 2080 s would be more than twice the reported losses of the 2004 typhoon season, the costliest in terms of damage during the past 100 years. The cost of direct damage in Asia caused by tropical cyclones has increased more than five times in the 1980 s as compared with those in the 1970 s and about 35 times more in the early 1990 s than in 1970 s ( (Yoshino, 1996 ) ). Flood-related damages also increased by about three times and eight times respectively in the 1990 s, relative to those in the 1980 s and 1970 s. These trends are likely to persist in the future.
Social vulnerability is the exposure of groups of people or individuals to stress as a result of the impacts of environmental change including climate change ( Adger, 2000 [ARC] ). Social vulnerability emphasises the inequitable distribution of damages and risks amongst groups of people ( Wu et al., 2002 [SRC] ) and is a result of social processes and structures that constrain access to the resources that enable people to cope with impacts ( Blaikie et al., 1994 [NPR] ). The poor, particularly in urban and urbanising cities of Asia, are highly vulnerable to climate change because of their limited access to profitable livelihood opportunities and limited access to areas that are fit for safe and healthy habitation. Consequently, the poor sector will likely be exposed to more risks from floods and other climate-related hazards in areas they are forced to stay in ( Adger, 2003 [ARC] ). This also includes the rural poor who live in the lower Mekong countries and are dependent on fisheries as their major livelihood, along with those living in coastal areas who are likely to suffer heavy losses without appropriate protection (see Table 10.10 MRC, 2003 [NPR] ). Protection from the social forces that create inequitable exposure to risk will be as important if not more important than structural protection from natural hazards in reducing the vulnerability of the poor ( Hewitt, 1997 [NPR] ).
Many studies ( Parry, 2002 [JoC, ARC] ;( Ge et al., 2002; ) ( Droogers, 2004; ) Lin et al., 2004 [NPR, MoS, SRC] ;( Vlek et al., 2004; ) ( Wang et al., 2004a; ) Zalikhanov, 2004 [NPR] ; Lal, 2007 [NPR, SRC, 2007] ; Batima et al., 2005c [NPR] ) on the impacts of climate change on agriculture and possible adaptation options have been published since the TAR. More common adaptation measures that have been identified in the above-mentioned studies are summarised in Table 10.8 . Generally, these measures are intended to increase adaptive capacity by modifying farming practices, improving crops and livestock through breeding and investing in new technologies and infrastructure. Specific examples include adaptation of grassland management to the actual environmental conditions as well as the practice of reasonable rotational grazing to ensure the sustainability of grassland resources ( (Li et al., 2002; ) ( Wang et al., 2004a; ) Batima et al., 2005c [NPR] ), improvement of irrigation systems and breeding of new rice varieties to minimise the risk of serious productivity losses caused by climate change ( (Ge et al., 2002 ) ), and information, education and communication programmes to enhance the level of awareness and understanding of the vulnerable groups.
|1°C temperature increase in June to August||Choice of crop and cultivar:
|Development of agricultural bio-technologies||
|Improvement of agricultural infrastructure||
Changes in management philosophy could also enhance adaptive capacity. This is illustrated by integrating fisheries and aquaculture management into coastal zone management to increase the coping ability of small communities in East Asia, South Asia and South-East Asia to sea-level rise ( (Troadec, 2000 ) ).
The ability of local populations to adapt their production systems to cope with climate change will vary across Asia and will be largely influenced by the way government institutions and policies mediate the supply of, and access to, food and related resources. The adaptive capacity of poor subsistence farming/herding communities is commonly low in many developing countries of Asia. One of the important and effective measures to enhance their adaptive capacity is through education and the provision of easy access to climate change-related information.
In some parts of Asia, conversion of cropland to forest (grassland), restoration and re-establishment of vegetation, improvement of the tree and herb varieties, and selection and cultivation of new drought-resistant varieties are effective measures to prevent water scarcity due to climate change. Water saving schemes for irrigation should be enforced to avert water scarcity in regions already under water stress ( (Wang, 2003 ) ). In North Asia, recycling and reuse of municipal wastewater ( Frolov et al., 2004 [NPR] ), increasing efficiency of water used for irrigation and other purposes ( Alcamo et al., 2004 [NPR, ARC] ), reduction of hydropower production ( Kirpichnikov et al., 2004 [NPR] ) and improved use of rivers for navigation ( Golitsyn and Yu, 2002 [NPR] ) will likely help avert water scarcity.
There are many adaptation measures that could be applied in various parts of Asia to minimise the impacts of climate change on water resources and use: several of which address the existing inefficiency in the use of water. Modernisation of existing irrigation schemes and demand management aimed at optimising physical and economic efficiency in the use of water resources and recycled water in water stressed countries of Asia could be useful in many agricultural areas in Asia, particularly in arid and semi-arid countries. Public investment policies which are aimed at improving access to available water resources, integrated water management, respect for the environment and promotion of better practices for wise use of water in agriculture, including recycled waste water could potentially enhance adaptive capacity. As an adaptation measure, apart from meeting non-potable water demands, recycled water can be used for recharging groundwater aquifers and augmenting surface water reservoirs. Recycled water can also be used to create or enhance wetlands and riparian habitats. While water recycling is a sustainable approach towards adaptation to climate change and can be cost-effective in the long term, the treatment of wastewater for reuse, such as that being practiced now in Singapore, and the installation of distribution systems, can be initially expensive compared to such water supply alternatives as imported water or groundwater, but are potentially important adaptive options in many countries of Asia. Reduction of water wastage and leakages, which in some cities like Damascus can be substantial, could be practiced to cushion the decrease in water supply due to decline in precipitation and increase in temperature. The use of market-oriented approaches to reduce wasteful water uses could also be effective in reducing effects of climate change on water resources ( Ragab and Prudhomme, 2002 [ARC] ). In rivers like the Mekong where wet season riverflows are estimated to increase and the dry season flows projected to decrease, planned water management interventions could marginally decrease wet season flows and substantially increase dry season flows (World Bank, 2004 [NPR, MoS] ).
The response to sea-level rise could mean protection, accommodation and retreat. As substantial socio-economic activities and populations are currently highly concentrated in the coastal zones in Asia, protection should remain a key focus area in Asia. Coastal protection constructions in Asia for 5-year to 1,000-year storm-surge elevations need to be considered. Most megacities of Asia located in coastal zones need to ensure that future constructions are done at elevated levels ( Nicholls, 2004 [JoC, ARC] ; Nishioka and Harasawa, 1998 [NPR, SRC] ;( Du and Zhang, 2000 ) ). The dike heightening and strengthening has been identified as one of the adaptation measures for coastal protection ( (Du and Zhang, 2000; ) Huang and Xie, 2000 [NPR] ; Li et al., 2004a [SRC] , b).
Integrated Coastal Zone Management (ICZM) provides an effective coastal protection strategy to maximise the benefits provided by the coastal zone and to minimise the conflicts and harmful effects of activities on social, cultural and environmental resources to promote sustainable management of coastal zones (World Bank, 2002 [NPR] ). The ICZM concept is being embraced as a central organising concept in the management of fisheries, coral reefs, pollution, megacities and individual coastal systems in China, India, Indonesia, Japan, Korea, the Philippines, Sri Lanka, Vietnam and Kuwait. It has been successfully applied for prevention and control of marine pollution in Batangas Bay of the Philippines and Xiamen of China over the past few years ( (Chua, 1999; ) ( Xue et al., 2004 ) ). The ICZM concept and principle could potentially promote sustainable coastal area protection and management in other countries of Asia.
The probability of significant adverse impacts of climate change on Asian forests is high in the next few decades ( Isaev et al., 2004 [NPR] ). Improved technologies for tree plantation development and reforestation could likely enhance adaptation especially in vulnerable areas such as the Siberian forests. Likewise improvement of protection from fires, insects and diseases could reduce vulnerability of most forests in Asia to climate change and variability.
Comprehensive intersectoral programs that combine measures to control deforestation and forest degradation with measures to increase agricultural productivity and sustainability will likely contribute more to reducing vulnerability of forests to climate change, land use change and other stress factors than independent sectoral initiatives. Other likely effective adaptation measures to reduce the impacts of climate change on forest ecosystems in Asia include extending rotation cycles, reducing damage to remaining trees, reducing logging waste, implementing soil conservation practices, and using wood in a more carbon-efficient way such that a large fraction of their carbon is conserved.
Assessment of the impact of climate change is the first step for exploring adaptation strategy. The disease monitoring system is essential as the basic data source. Specifically, the monitoring of diseases along with related ecological factors is required because the relation between weather factors and vector-borne diseases are complicated and delicate ( (Kovats et al., 2003 ) ). Also, disease monitoring is necessary in assessing the effectiveness and efficiency of the adaptation measures ( Wilkinson et al., 2003 [NPR] ). For effective adaptation measures, the potential impacts of climate variability and change on human health need to be identified, along with barriers to successful adaptation and the means of overcoming such barriers.
The heat watch and warning system in the USA was evaluated to be effective ( Ebi et al., 2004 [JoC, ARC] ). Also, a similar system was operated in Shanghai, China ( (Tan et al., 2004 ) ). Implementation of this type of heat watch and warning system and other similar monitoring systems in other parts of Asia will likely be helpful in reducing the impacts of climate change on human health.
Rapid population growth, urbanisation and weak land-use planning and enforcement are some of the reasons why poor people move to fragile and high-risk areas which are more exposed to natural hazards. Moreover, the rapid growth of industries in urban areas has induced rural-urban migration. Rural development together with networking and advocacy, and building alliances among communities is a prerequisite for reducing the migration of people to cities and coastal areas in most developing countries of Asia ( Kelly and Adger, 2000 [JoC] ). Raising awareness about the dangers of natural disasters, including those due to climate extremes, is also crucial among the governments and people so that mitigation and preparedness measures could be strengthened. Social capital has been paid attention to build adaptive capacity ( (Allen, 2006 ) ). For example, a community-based disaster management programme was introduced to reduce vulnerability and to strengthen people’s capacity to cope with hazards by the Asian Disaster Preparedness Centre, Bangkok ( Pelling, 2003 [NPR] ).
Tourism is one of the most important industries in Asia, which is the third centre of tourism activities following Europe and North America. Sea-level rise, warming sea temperatures and extreme weather events are likely to have impacts on the regions’ islands and coasts which attract considerable number of visitors from countries such as Japan and Taiwan (World Tourism Organization, 2003; Hamilton et al., 2005 [JoC, MoS, ARC] ). Relevant adaptation measures in this case include designing and building appropriate infrastructures to protect tourists, installation and maintenance of weather prediction and hazard warning systems, especially during rainy and tropical storm seasons. Conservation of mangroves is considered as effective natural protection against storm surges, coastal erosion and strong wave actions ( (Mazda et al., 1997, ) 2006; ( Vermaat and Thampanya, 2006 ) ). To minimise the anticipated impact of global warming on the ski industry, development of new leisure industries more resistant to or suited to a warmer atmosphere, thus avoiding excessive reliance on the ski industry, e.g., grass-skiing, hiking, residential lodging and eco-tourism, could be helpful in compensating for the income reduction due to snow deterioration ( Fukushima et al., 2002 [SRC] ).
To minimise the risks of heat stress that are most pronounced in large cities due to the urban heat-island effect in summer ( Kalnay and Cai, 2003 [JoC] ) urban planning should consider: reducing the heat island in summer, the heat load on buildings, cooling load and high night-time temperature, and taking climate change into account in planning new buildings and setting up new regulations on buildings and urban development. Planting trees, building houses with arcades and provision for sufficient ventilation could help in reducing heat load ( (Shimoda, 2003 ) ). The use of reflective surfaces, control of solar radiation by vegetation and blinds, earth tubes, the formation of air paths for natural ventilation, and rooftop planting could reduce the cooling load.
Effective adaptation and adaptive capacity in Asia, particularly in developing countries, will continue to be limited by several ecological, social and economic, technical and political constraints including spatial and temporal uncertainties associated with forecasts of regional climate, low level of awareness among decision makers of the local and regional impacts of El Niño, limited national capacities in climate monitoring and forecasting, and lack of co-ordination in the formulation of responses ( Glantz, 2001 [NPR] ).
Radical climate change may cause alterations of the physical environment in an area that may limit adaptation possibilities ( Nicholls and Tol, 2006 [JoC, ARC] ). For example, migration is the only option in response to sea-level rise that inundates islands and coastal settlements (see Chapter 17 , Section 188.8.131.52 ). Likewise, impacts of climate change may occur beyond certain thresholds in the ability of some ecosystems to adapt without dramatic changes in their functions and resilience. The inherent sensitivity of some ecosystems, habitats and even species with extremely narrow ranges of biogeographic adaptability will also limit the options and effectiveness of adaptation.
Poverty is identified as the largest barrier to developing the capacity to cope and adapt ( Adger et al., 2001 [NPR] ). The poor usually have a very low adaptive capacity due to their limited access to information, technology and other capital assets which make them highly vulnerable to climate change. Poverty also constrains the adaptation in other sectors. Poverty, along with infrastructural limitations and other socioeconomic factors, will continue to limit the efforts to conserve biodiversity in South-East Asia ( (Sodhi et al., 2004 ) ). Adaptive capacity in countries where there is a high incidence of poverty will likely remain limited.
Insufficient information and knowledge on the impacts of climate change and responses of natural systems to climate change will likely continue to hinder effective adaptation particularly in Asia. The limited studies on the interconnections between adaptation and mitigation options, costs and benefits of adaptation, and trade-offs between various courses of actions will also likely limit adaptation in Asia. The deficiency in available information and knowledge will continue to make it difficult to enhance public perception of the risks and dangers associated with climate change. In addition, the absence of information on adaptation costs and benefits makes it difficult to undertake the best adaptation option. This limiting factor will be most constraining in developing countries where systems for monitoring and research on climate and responses of natural and human systems to climate are usually lacking. More relevant information such as on the crop yield benefits linked to changes in planting dates for various regions, as reported by Tan and Shibasaki 2003 [MoS] ), and on the optimal levels and cost of coastal protection investment in Vietnam, Cambodia and other countries, as reported by Nicholls and Tol 2006 [JoC, ARC] ), will be needed.
Based on the discussion in Chapter 17 , Section 184.108.40.206 , it is very likely that in countries of Asia facing serious domestic conflicts, pervasive poverty, hunger, epidemics, terrorism and other pressing and urgent concerns, attention may be drawn away from the dangers of climate change and the need to implement adaptation. The slow change in political and institutional landscape in response to climate change could also be a major limitation to future adaptation. The existing legal and institutional framework in most Asian countries remains inadequate to facilitate implementation of comprehensive and integrated response to climate change in synergy with the pursuit of sectoral development goals.
To address the constraints discussed above and strengthen adaptation in Asia, some of the measures suggested by Stern 2007 [NPR, 2007] ) could be useful. These include improving access to high-quality information about the impacts of climate change; adaptation and vulnerability assessment by setting in place early warning systems and information distribution systems to enhance disaster preparedness; reducing the vulnerability of livelihoods and infrastructure to climate change; promoting good governance including responsible policy and decision making; empowering communities and other local stakeholders so that they participate actively in vulnerability assessment and implementation of adaptation; and mainstreaming climate change into development planning at all scales, levels and sectors.
There are 11 megadeltas with an area greater than 10,000 km2 ( Table 10.10 ) in the coastal zone of Asia that are continuously being formed by rivers originating from the Tibetan Plateau ( (Milliman and Meade, 1983; ) Penland and Kulp, 2005 [NPR] ) These megadeltas are vital to Asia because these are home to millions of people, especially the seven megacities that are located in these deltas ( Nicholls, 1995 [ARC] ; Woodroffe et al., 2006 [NPR, SRC] ). The megadeltas, particularly the Zhujiang delta, Changjiang delta and Huanghe delta, are also economically important, accounting for a substantial proportion of China’s total GDP ( Niou, 2002 [NPR] ; She, 2004 [NPR, MoS] ). Ecologically, the Asian megadeltas are critical diverse ecosystems of unique assemblages of plants and animals located in different climatic regions ( IUCN, 2003b [NPR] ; ACIA, 2005 [NPR] ; Macintosh, 2005 [NPR] ; Sanlaville and Prieur, 2005 ). However, the megadeltas of Asia are vulnerable to climate change and sea-level rise that could increase the frequency and level of inundation of megadeltas due to storm surges and floods from river drainage ( Nicholls, 2004 [JoC, ARC] ; Woodroffe et al., 2006 [NPR, SRC] ) putting communities, biodiversity and infrastructure at risk of being damaged. This impact could be more pronounced in megacities located in megadeltas where natural ground subsidence is enhanced by human activities, such as in Bangkok in the Chao Phraya delta, Shanghai in the Changjiang delta, Tianjin in the old Huanghe delta ( (Nguyen et al., 2000; ) Li et al., 2004a [SRC] ;( Jiang, 2005; ) Li et al., 2005 [SRC] ; Woodroffe et al., 2006 [NPR, SRC] ). Climate change together with human activities could also enhance erosion that has, for example, caused the Lena delta to retreat at a rate of 3.6 to 4.5 m/yr ( Leont’yev, 2004 [MoS] ) and has affected the progradation and retreat of megadeltas fed by rivers originating from the Tibetan Plateau ( Li et al., 2004b [SRC] ; Thanh et al., 2004 [SRC] ;( Shi et al., 2005; ) Woodroffe et al., 2006 [NPR, SRC] ). The adverse impacts of salt-water intrusion on water supply in the Changjiang delta and Zhujiang delta, mangrove forests, agriculture production and freshwater fish catch, resulting in a loss of US$125x106 per annum in the Indus delta could also be aggravated by climate change ( IUCN, 2003a [NPR] , b; Shen et al., 2003 [NPR] ;( Huang and Zhang, 2004 ) ).
Externally, the sediment supplies to many megadeltas have been reduced by the construction of dams and there are plans for many more dams in the 21st century ( Chapter 6 , Box 6.3 Woodroffe et al., 2006 [NPR, SRC] ). Reduction of sediment supplies make these systems much more vulnerable to climate change and sea-level rise. When considering all the non-climate pressures, there is very high confidence that the group of populated Asian megadeltas is highly threatened by climate change and responding to this threat will present important challenges (see also Chapter 6 , Box 6.3 ). The sustainability of megadeltas in Asia in a warmer climate will rest heavily on policies and programmes that promote integrated and co-ordinated development of the megadeltas and upstream areas, balanced use and development of megadeltas for conservation and production goals, and comprehensive protection against erosion from river flow anomalies and sea-water actions that combines structural with human and institutional capability building measures ( (Du and Zhang, 2000; ) Inam et al., 2003 [NPR] ; Li et al., 2004b [SRC] ; Thanh et al., 2004 [SRC] ; Saito, 2005 [NPR, SRC] ; Wolanski, 2007 [NPR, 2007] ; Woodroffe et al., 2006 [NPR, SRC] ).
|Area (103 km2)||43.6||36.3||66.9||10||16||62.5||18||20.6||100||29.5||18.5|
|Water discharge (109 m3/yr)||520||33.3||905||326||120||470||30||430||1330||185||46|
|Sediment load (106 t/yr)||18||849||433||76||130||160||11||260||1969||400||100|
|Delta growth (km2/yr)||--||21.0||16.0||11.0||3.6||1.2||10.0||5.5 to 16.0||PD30|
|Mangroves (103 km2)||None||None||None||None||5.2||2.4||4.2||10||1.6||None|
|Population (106) in 2000||0.000079||24.9 (00)||76 (03)||42.3 (03)||13.3||15.6||11.5||10.6||130||3.0||0.4|
|Population increase by 2015||None||18||-||176||21||21||44||15||28||45||--|
|GDP (US$109)||58.8 (00)||274.4 (03)||240.8 (03)||9.2 (04)||7.8 (04)||--||--||--||--||--|
|Ground subsidence (m)||None||2.6 to 2.8||2.0 to 2.6||X||XX||--||0.2 to 1.6||--||0.6 to 1.9 mm/a||--|
|SLR (cm) in 2050||10 to 90 (2100)||70 to 90||50 to 70||40 to 60||--||--||--||--||--||20 to 50||--|
|Salt-water intrusion (km)||--||--||100||--||30 to 50||60 to 70||--||--||100||80||--|
|Natural hazards||--||FD||CS, SWI, FD||CS, FD, SWI||CS, FD, SWI||SWI||--||--||CS, FD, SWI||CS, SWI||--|
|Area inundated by SLR (103 km2). Figure in brackets indicates amount SLR.||--||21.3 (0.3m)||54.5 (0.3m)||5.5 (0.3m)||5 (1m)||20 (1m)||--||--||--||--||--|
|Coastal protection||No protection||Protected||Protected||Protected||Protected||Protected||Protected||Protected||Protected||Partial Protection||Partial protection|
Himalayan glaciers cover about three million hectares or 17% of the mountain area as compared to 2.2% in the Swiss Alps. They form the largest body of ice outside the polar caps and are the source of water for the innumerable rivers that flow across the Indo-Gangetic plains. Himalayan glacial snowfields store about 12,000 km3 of freshwater. About 15,000 Himalayan glaciers form a unique reservoir which supports perennial rivers such as the Indus, Ganga and Brahmaputra which, in turn, are the lifeline of millions of people in South Asian countries (Pakistan, Nepal, Bhutan, India and Bangladesh). The Gangetic basin alone is home to 500 million people, about 10% of the total human population in the region.
Glaciers in the Himalaya are receding faster than in any other part of the world (see Table 10.9 ) and, if the present rate continues, the likelihood of them disappearing by the year 2035 and perhaps sooner is very high if the Earth keeps warming at the current rate. Its total area will likely shrink from the present 500,000 to 100,000 km2 by the year 2035 ( WWF, 2005 [NPR] ).
|Glacier||Period||Retreat of||Average retreat|
|snout (metre)||of glacier (metre/year)|
|Triloknath Glacier (Himachal Pradesh)||1969 to 1995||400||15.4|
|Pindari Glacier (Uttaranchal)||1845 to 1966||2,840||135.2|
|Milam Glacier (Uttaranchal)||1909 to 1984||990||13.2|
|Ponting Glacier (Uttaranchal)||1906 to 1957||262||5.1|
|Chota Shigri Glacier (Himachal Pradesh)||1986 to 1995||60||6.7|
|Bara Shigri Glacier (Himachal Pradesh)||1977 to 1995||650||36.1|
|Gangotri Glacier (Uttaranchal)||1977 to 1990||364||28.0|
|Gangotri Glacier (Uttaranchal)||1985 to 2001||368||23.0|
|Zemu Glacier (Sikkim)||1977 to 1984||194||27.7|
The receding and thinning of Himalayan glaciers can be attributed primarily to the global warming due to increase in anthropogenic emission of greenhouse gases. The relatively high population density near these glaciers and consequent deforestation and land-use changes have also adversely affected these glaciers. The 30.2 km long Gangotri glacier has been receding alarmingly in recent years ( Figure 10.6 ). Between 1842 and 1935, the glacier was receding at an average of 7.3 m every year; the average rate of recession between 1985 and 2001 is about 23 m per year ( Hasnain, 2002 [NPR] ). The current trends of glacial melts suggest that the Ganga, Indus, Brahmaputra and other rivers that criss-cross the northern Indian plain could likely become seasonal rivers in the near future as a consequence of climate change and could likely affect the economies in the region. Some other glaciers in Asia – such as glaciers shorter than 4 km length in the Tibetan Plateau – are projected to disappear and the glaciated areas located in the headwaters of the Changjiang River will likely decrease in area by more than 60% ( Shen et al., 2002 [MoS, ARC] ).
Chapter 20 , Section 20.1 of this volume uses the succinct definition of the Bruntland Commission to describe sustainable development as “development that meets the needs of the present without compromising the ability of future generations to meet their own needs”. Sustainable development represents a balance between the goals of environmental protection and human economic development and between the present and future needs. It implies equity in meeting the needs of people and integration of sectoral actions across space and time. This section focuses mainly on how the impacts of projected climate change on poverty eradication, food security, access to water and other key concerns described above will likely impinge on the pursuit of sustainable development in Asia. In most instances, the reference to sustainable development will be confined to a specific country or sub-region, primarily due to the existing difficulty of aggregating responses to climate change and other stressors across the whole of Asia.
A significant proportion of the Asian population is living below social and economic poverty thresholds. Asia accounts for more than 65% of all people living in rural areas without access to sanitation, of underweight children, of people living on less than a dollar a day and of TB cases in the world. It accounts for over 60% of all malnourished people, people without access to sanitation in urban areas and people without access to water in rural areas ( UN-ESCAP, 2006 [NPR] ). Most of the world’s poor reside in South Asia and, within South Asia, the majority resides in rural areas ( (Srinivasan, 2000 ) ). Greater inequality could both undermine the efficiency with which future growth could reduce poverty and make it politically more difficult to pursue pro-poor policies ( Fritzen, 2002 [MoS] ).
Coupled with illiteracy, poverty subverts the ability of the people to pursue the usually long-term sustainable development goals in favour of the immediate goal of meeting their daily subsistence needs. This manifests in the way poverty drives poor communities to abusive use of land and other resources that lead to onsite degradation and usually macroscale environmental deterioration. In the absence of opportunities for engaging in stable and gainful livelihood, poverty stricken communities are left with no option but to utilise even the disaster-prone areas, unproductive lands and ecologically fragile lands that have been set aside for protection purposes such as conservation of biodiversity, soil and water. With climate change, the poor sectors will be most vulnerable and, without appropriate measures, climate change will likely exacerbate the poverty situation and continue to slow down economic growth in developing countries of Asia ( Beg et al., 2002 [JoC, ARC] ).
Rapid economic growth characterised by increasing urbanisation and industrialisation in several countries of Asia (i.e., China, India and Vietnam) will likely drive the increase in the already high demand for raw materials such as cement, wood, steel and other construction materials in Asia. Consequently, the use of forests, minerals and other natural resources will increase along with the increase in carbon emission. The challenge here is finding the development pathways wherein GHG emission is minimised while attaining high economic growth ( (Jiang et al., 2000 ) ). Equally vital in this regard is the promotion of equity in spreading the benefits that will arise from economic growth so as to uplift the condition of the poor sector to a state of enhanced capacity to adapt to climate change. Another concern related to economic growth is the increase in the value of land to a level where it becomes economically less profitable to farm agricultural land than using the land for industrial and commercial purposes. In the absence of appropriate regulatory intervention, this can undermine the production of adequate food supply and further jeopardise the access of the poor to food support.
Sustaining economic growth in the context of changing climate in many Asian countries will require the pursuit of enhancing preparedness and capabilities in terms of human, infrastructural, financial and institutional dimensions with the aim in view of reducing the impacts of climate change on the economy. For instance, in many developing countries, instituting financial reforms could likely result in a more robust economy that is likely to be less vulnerable to changing climate ( (Fase and Abma, 2003 ) ). In countries with predominantly agrarian economies, climate change, particularly an increase in temperature and reduction in precipitation, could, in the absence of adequate irrigation and related infrastructural interventions, dampen the economic growth by reducing agricultural productivity ( Section 10.4.1 ).
Many countries in Asia are signatories to one or more of the Multilateral Environmental Agreements (MEAs) that seek to address common concerns such as biodiversity conservation and sustainable forest management, climate change, international water resources, over-exploitation of regional fisheries, trans-boundary air pollution, and pollution of regional seas. Some of these MEAs include the United Nations Framework Convention on Climate Change (UNFCCC), the Convention on Biological Diversity (CBD), the Convention to Combat Desertification (CCD), the Convention on International Trade of Endangered Fauna and Flora (CITES), the Ramsar Convention to protect Mangroves and Wetlands, the Montreal and Kyoto Protocols to address problems of the breakdown in the Earth’s protective ozone layer and global warming, International Tropical Timber Organization (ITTO) that governs the exploitation of tropical forests and conservation of biodiversity, and International Convention for the Prevention of Pollution from Ships for control of pollution of regional seas. The major challenge for Asian countries is how to take advantage of opportunities in designing integrated and synergistic responses in adherence to and compliance with the terms and conditions of MEAs and improve environmental quality without unduly hampering economic development ( Beg et al., 2002 [JoC, ARC] ).
Natural resources utilisation could intensify in several parts of Asia in response to increasing demands. In South-East Asia, intensification of forest utilisation could likely increase further the already high rate of deforestation that could lead to the loss of much of its original forests and biodiversity by 2100 ( (Sodhi et al., 2004 ) ). To sustain development in this region, measures to minimise deforestation and enhance restoration of degraded forests will be required. The challenge in Asia will be in countries with developing economies where the need to maximise production could lead to increased perturbations of the ecosystems and the environment that could be aggravated by climate change. In the same manner, the use of water will continue to increase as the population and economies of countries grow. This will likely put more stress on water that could be exacerbated by climate change as discussed above. Integrated responses to cope with the impacts of climate change and other stressors on the supply and demand side will likely contribute in the attainment of sustainable development in many countries in the West, South and South-East Asia.
The base for future climate change studies is designing future social development scenarios by various models and projecting future regional and local changes in climate and its variability, based on those social development scenarios so that most plausible impacts of climate change could be assessed. The emission scenarios of greenhouse gases and aerosols are strongly related to the socio-economics of the countries in the region and could be strongly dependent on development pathways followed by individual nations. Inaccurate description on future scenarios of socio-economic change, environmental change, land-use change and technological advancement and its impacts will lead to incorrect GHG emissions scenarios. Therefore factors affecting design of social development scenarios need to be examined more carefully to identify and properly respond to key uncertainties.
The large natural climate variability in Asia adds a further level of uncertainty in the evaluation of a climate change simulation. Our current understanding of the precise magnitude of climate change due to anthropogenic factors is relatively low, due to imperfect knowledge and/or representation of physical processes, limitations due to the numerical approximation of the model’s equations, simplifications and assumptions in the models and/or approaches, internal model variability, and inter-model or inter-method differences in the simulation of climate response to given forcing. Current efforts on climate variability and climate change studies increasingly rely upon diurnal, seasonal, latitudinal and vertical patterns of temperature trends to provide evidence for anthropogenic signatures. Such approaches require increasingly detailed understanding of the spatial variability of all forcing mechanisms and their connections to global, hemispheric and regional responses.
Uncertainty in assessment methodologies per se is also one of the main sources of uncertainty. In model-based assessments, results on impacts of climate change, in fact, accumulate errors from the methodologies for establishment of socio-economic scenarios, environmental scenarios, climate scenarios and climate impact assessment ( Challinor et al., 2005 [JoC, MoS, ARC] ).
The vulnerability of key sectors to the projected climate change for each of the seven sub-regions of Asia based on currently available scientific literature referred to in this assessment have been assigned a degree of confidence which is listed in Table 10.11 . The assigned confidence levels could provide guidance in weighing which of the sectors ought to be the priority concerns based on the most likely future outcomes. However, some of the greatest concerns emerge not from the most likely future outcomes but rather from possible ‘surprises’. Growing evidence suggests the ocean-atmosphere system that controls the world’s climate can lurch from one state to another, such as a shutdown of the ‘ocean conveyor belt’ in less than a decade. Certain threshold events may become more probable and non-linear changes and surprises should be anticipated, even if they cannot be predicted with a high degree of confidence. Abrupt or unexpected changes pose great challenges to our ability to adapt and can thus increase our vulnerability to significant impacts ( Preston et al., 2006 [NPR] ).
The spotlight in climate research is shifting from gradual to rapid or abrupt change. There is some risk that a catastrophic collapse of the ice sheet could occur over a couple of centuries if polar water temperatures warm by a few degrees. Scientists suggest that such a risk has a probability of between 1 and 5% ( Alley, 2002 [JoC] ). Because of this risk, as well as the possibility of a larger than expected melting of the Greenland Ice Sheet, a recent study estimated that there is a 1% chance that global sea level could rise by more than 4 metres in the next two centuries ( Hulbe and Payne, 2001 [MoS] ).
|Sub-regions||Food and fibre||Biodiversity||Water resource||Coastal||Human health||Settlements||Land|
|North Asia||+1 / H||-2 / M||+1 / M||-1 / M||-1 / M||-1 / M||-1 / M|
|Central Asia and West Asia||-2 / H||-1 / M||-2 / VH||-1 / L||-2 / M||-1 / M||-2 / H|
|Tibetan Plateau||+1 / L||-2 / M||-1 / M||Not applicable||No information||No information||-1 / L|
|East Asia||-2 / VH||-2 / H||-2 / H||-2 / H||-1 / H||-1 / H||-2 / H|
|South Asia||-2 / H||-2 / H||-2 / H||-2 / H||-2 / M||-1 / M||-2 / H|
|South-East Asia||-2 / H||-2 / H||-1 / H||-2 / H||-2 / H||-1 / M||-2 / H|
A number of fundamental scientific questions relating to the build-up of greenhouse gases in the atmosphere and the behaviour of the climate system need to be critically addressed. These include (a) the future usage of fossil fuels, (b) the future emissions of methane ( Slingo et al., 2005 [JoC] ; Challinor et al., 2006 [NPR] ), (c) the fraction of the future fossil-fuel carbon that will remain in the atmosphere and provide radiative forcing versus exchange with the oceans or net exchange with the land biosphere, (d) details of the regional and local climate change given an overall level of global climate change, (e) the nature and causes of the natural variability of climate and its interactions with forced changes, and (f) the direct and indirect effects of the changing distributions of aerosols.
An effective strategy for advancing the understanding of adverse impacts of climate change in Asia will require strengthening the academic and research institutions to conduct innovative research on the response of human and natural systems to multiple stresses at various levels and scales. Key specific research-related priorities for Asia are:
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Tao, F., M. Yokozawa, Y. Hayashi and E. Lin, 2003a: Changes in agricultural water demands and soil moisture in China over the last half-century and their effects on agricultural production. Agr. Forest Meteorol., 118, 251–261. Clean
Tao, F., M. Yokozawa, Y. Hayashi and E. Lin, 2003b: Future climate change, the agricultural water cycle, and agricultural production in China. Agriculture, Ecosystems and Environment, 95, 203-215. [MoS]
Tao, F., M. Yokozawa, Z. Zhang, Y. Hayashi, H. Grassl and C. Fu, 2004: Variability in climatology and agricultural production in China in association with the East Asia summer monsoon and El Niño South Oscillation. Climate Res., 28, 23-30. Clean
Teranishi, L., Y. Kenda, T. Katoh, M. Kasuya, E. Oura and H. Taira, 2000: Possible role of climate change in the pollen scatter of Japanese cedar Cryptomeria japonica in Japan. Climate Res., 14, 65-70. Clean
TERI, 1996: The economic impact of a one-metre sea level rise on the Indian coastline: method and case studiesTata Energy Research Institute, New Delhi, Report No 93/GW/52, submitted to the Ford Foundation. [NPR]
Tong, S.L. and L.V. Ying, 2000: Global Climate Change and Epidemic Disease. Journal of Disease Control, 4, 17-19. Clean
Tran, V.L., D.C. Hoang and T.T. Tran, 2005: Building of climate change scenario for Red River catchments for sustainable development and environmental protection. Preprints, Science Workshop on Hydrometeorological Change in Vietnam and Sustainable Development, Hanoi, Vietnam, Ministry of Natural Resource and Environment, Hanoi, 70-82. [NPR]
Troadec, J.P., 2000: Adaptation opportunities to climate variability and change in the exploitation and utilisation of marine living resources. Environ. Monit. Assess., 61, 101-112. Clean
Tserendash, S., B. Bolortsetseg, P. Batima, G. Sanjid, M. Erdenetuya, T. Ganbaatar and N. Manibazar, 2005: Climate change impacts on pasture. Climate Change Impacts, P. Batima and B. Bayasgalan, Eds., Admon publishing, Ulaanbaatar, 59-115. [NPR, ARC]
Vermaat, J. and U. Thampanya, 2006: Mangroves mitigate tsunami damage: a further response. Estuar. Coast. Shelf S., 69, 1-3. Clean
Vlek, P.L.G., K.G. Rodriguez and R. Sommer, 2004: Energy use and CO2 production in tropical agriculture and means and strategies for reduction or mitigation. Environment Development and Sustainability, 6, 213-233. Clean
Vorobyov, Y., 2004: Climate change and disasters in Russia. Proc. World Climate Change Conference, Moscow, Y. Izrael, G. Gruza, S. Semenov and I. Nazarov, Eds., Institute of Global Climate and Ecology, Moscow, 293-298. [NPR]
Wada, N., K. Watanuki, K. Narita, S. Suzuki, G. Kudo and A. Kume, 2004: Climate change and shoot elongation of Alpine Dwarf Pine (Pinus Pumila): comparisons among six Japanese mountains. 6th International Symposium on Plant Responses to Air Pollution and Global Changes, Tsukuba, 215. [NPR]
Walsh, K.J.E., 2004: Tropical cyclones and climate change: unresolved issues. Climate Res., 27, 77-84. Clean
Wang, F.T., 2002: Advances in climate warming impacts research in China in recent ten years. Journal of Applied Meteorological Science, 13, 766. Clean
Wang, G.Z., 2005: Global sea-level change and coral reefs of China. Journal of Palaeogeography, 7, 483-492 (in Chinese with an English abstract). Clean
Wang, M., Y. Li and S. Pang, 2004a: Influences of climate change on sustainable development of the hinterland of Qinghai-Tibet Plateau, Chinese Journal of Population, Resources and Environment, 14, 92-95. Clean
Wang, T., 2003: Study on desertification in China, 2 - Contents of desertification research. Journal of Desert Research, 23, 477-482. Clean
Wang, X.C. and P.K. Jin, 2006: Water shortage and needs for wastewater re-use in the north China. Water Sci. Technol., 53, 35-44. Clean
Wang, Y.B., G.X. Wang and J. Chang, 2004b: Impacts of human activity on permafrost environment of the Tibetan Plateau. Journal of Glaciology and Geocryology, 26, 523-527. Clean
Wang, Z.W. and P.M. Zhai, 2003: Climate change in drought over northern China during 1950–2000. Acta Geographica Sinica, 58, 61–68 (in Chinese). Clean
Wassmann, R., N.X. Hien, C.T. Hoanh and T.P. Tuong, 2004: Sea level rise affecting the Vietnamese Mekong Delta: water elevation in the flood season and implications for rice production. Climatic Change, 66, 89-107. [JoC]
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Wu, Z.F., 2003: Assessment of ecoclimatic suitability and climate change impacts on broad leaved Korean pine forest in Northeast China. Chinese Journal of Applied Ecology, 14, 771-775. Clean
Xue, X.Z., H.S. Hong and A.T. Charles, 2004: Cumulative environmental impacts and integrated coastal management: the case of Xiamen, China. J. Environ. Manage., 71, 271-283. Clean
Yao, T.D., X.D. Liu, N.L. Wang and Y.F. Shi, 2000: Amplitude of climatic changes in Qinghai-Tibetan Plateau. Chinese Sci. Bull., 45, 98-106. Clean
Yasukevich, V.V. and S.M. Semenov, 2004: Simulation of climate-induced changes in natural habitats of malaria in Russia and neighboring countries, Proc. Intl. Conf. on Climate Change and Public Health in Russia, N.F. Izmerov, B.A. Revich and E.I. Korenberg, Eds., Russian Academy of Sciences, Moscow, 147-153. [NPR, ARC]
Yoshino, M., 1996: Change of global environment and insurance. Saigaino-kennkyuu, 26, 84-100 (in Japanese). Clean
Yoshino, M., 2000: Problems in climatology of dust storm and its relation to human activities in Northwest China. Journal of Arid Land Studies, 10, 171-181. Clean
Yoshino, M., 2002: Kosa (Asian dust) related to Asian Monsoon System. Korean Journal of Atmospheric Sciences, 5, S93-S100. Clean
Yoshio, M. and M. Ishii, 2001: Relationship between cold hardiness and northward invasion in the great mormon butterfly, Papilio memnon L. (Lepidoptera: Papilionidae) in Japan. Appl. Entomol. Zool., 36, 329-335. Clean
Zafar, A., 2005: Training and capacity building for managing our mangroves resources- UNU’s role to meet regional challenges. Environment and Sustainable Development Programme, Tokyo, Japan, Technical Notes of United Nations University, 5 pp. http://www.inweh.unu.edu/inweh/Training/UNU_Man groves_course.pdf . [NPR]
Zalikhanov, M., 2004: Climate change and sustainable development in the Russian Federation. Proc. World Climate Change Conference, Moscow, September 29-October 2003, Yu. Izrael, G. Gruza, S. Semenov and I. Nazarov, Eds., Institute of Global Climate and Ecology, Moscow, 466-477. [NPR]
Zeqiang, F., C. Yunlong, Y. Youxiao and D. Erfu, 2001: Research on the relationship of cultivated land change and food security in China. Journal of Natural Resources, 16, 313-319. Clean
Zhai, P.M., 2004: Climate change and meteorological disasters. Science and Technology Reviews, 7, 11-14. Clean
Zhang, J.W. and B.L. Du, 2000: The trend of tidal range enlarging along the coast of the Yellow Sea. Marine Science Bulletin, 19, 1-9. Clean
Zhang, Q. and G. Guo, 2004: The spatial and temporal features of drought and flood disasters in the past 50 years and monitoring and warning services in China. Science and Technology Reviews, 7, 21-24. [SRC]
Zhang, Y., W. Chen and J. Cihlar, 2003: A process-based model for quantifying the impact of climate change on permafrost thermal regimes. J. Geophys. Res., 108, 4695 doi:10.1029/2002JD003354. [JoC, MoS]
Zhao, L., C.L. Ping, D. Yang, G. Cheng, Y. Ding and S. Liu, 2004: Changes of climate and seasonally frozen ground over the past 30 years in Qinghai–Xizang (Tibetan) Plateau, China. Global Planet. Change, 43, 19-31. Clean
Zhou, Y.H., 2003: Characteristics of weather and climate during drought periods in South China. Journal of Applied Meteorological Science, 14, S118-S125. Clean
Zolotov, P.A. and Caliberny, 2004: Human physiological functions and public health Ultra-Continental Climate. Proc. Intl. Conf. on Climate Change and Public Health in Russia, N.F. Izmerov, B.A. Revich and E.I. Korenberg, Eds., Russian Academy of Sciences, Moscow, 212-222.[NPR]
Person of Concern Key individual involved in CRU emails as defined in this spreadsheet.
Journal of Concern A Journal which has published articles by one or more PoCs (Person of Concern)
Model or Simulation Reference appears to be a model or simulation, not observation or experiment.
Non Peer Reviewed Reference has no Journal or no Volume or no Pages or it has Editors.
Self Reference Concern Author of a chapter containing references to own work.
Paper authored or co-authored by person who is also in list of Authors of another chapter.
Paper dated 2007, when IPCC policy stated cutoff was December 2005
The reference was probably peer reviewed.
NOTE: In the Summary of Reviewer Comments,
Accepted includes only those responses that were unambiguously Accepted.
There are other categories of responses that we have not yet quantified
due to inconsistencies of usage.
|Reviewer||Total Comments||Accepted||IPCC Roles||Papers|
|Government of Japan||41||0||0||0|
|Republic of Korea||33||0||0||0|
|Government of India||26||0||0||2|
|Government of Australia||12||1||0||0|
|Government of Pakistan||10||0||0||0|
|Government of Netherlands||8||0||0||0|
|Government of Thailand||6||0||0||0|
|Government of China||4||0||0||0|
|Government of Finland||4||0||0||0|
|Government of Oman||1||0||0||0|
|Reviewer Type||Total Comments||Accepted||% Accepted|