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Simulation of the future change of East Asian monsoon climate using the IPCC SRES A2 and B2 scenarios 被引量:33

Simulation of the future change of East Asian monsoon climate using the IPCC SRES A2 and B2 scenarios
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摘要 In this paper, we applied the newest emission scenarios of the sulfur and greenhouse gases, i.e. Intergovernmental Panel on Climate Change (IPCC) Special Report on Emission Scenarios (SRES) A2 and B2 scenarios, to investigating the change of the East Asian climate in the last three decades of the 21st century with an atmosphere-ocean coupled general circulation model. The global warming enlarges the land-sea thermal contrast and, hence, enhances (reduces) the East Asian summer (winter) monsoon circulation. The precipitation from the Yangtze and Huaihe river valley to North China increases significantly. In particular, the strong rainfall increase over North China implies that the East Asian rainy area would expand northward. In addition, from the southeastern coastal area to North China, the rainfall would increase significantly in September, implying that the rainy period of the East Asian monsoon would be prolonged about one month. In July, August and September, the interannual variability of the precipitation enhances evidently over North China, meaning a risk of flooding in the future. In this paper, we applied the newest emission scenarios of the sulfur and greenhouse gases, i.e. Intergovernmental Panel on Climate Change (IPCC) Special Report on Emission Scenarios (SRES) A2 and B2 scenarios, to investigating the change of the East Asian climate in the last three decades of the 21st century with an atmosphere-ocean coupled general circulation model. The global warming enlarges the land-sea thermal contrast and, hence, enhances (reduces) the East Asian summer (winter) monsoon circulation. The precipitation from the Yangtze and Huaihe river valley to North China increases significantly. In particular, the strong rainfall increase over North China implies that the East Asian rainy area would expand northward. In addition, from the southeastern coastal area to North China, the rainfall would increase significantly in September, implying that the rainy period of the East Asian monsoon would be prolonged about one month. In July, August and September, the interannual variability of the precipitation enhances evidently over North China, meaning a risk of flooding in the future.
出处 《Chinese Science Bulletin》 SCIE EI CAS 2003年第10期1024-1030,共7页
基金 supported by the Key Project of the Chinese Academy of Sciences(Grant Nos.KZCX2-SW-210 and KZCX2-203) the National Key Programme for Developing Basic Sciences(Grant No.G1998040904) the National Natural Science Foundation of China(Grant No.40105006).
关键词 模拟 亚洲东方 季风 气侯变化 大气循环模型 East Asian monsoon, Climate change, IPCC SRES A2 and B2 scenarios.
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