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Impacts of Coastal SST Variability on the East Asian Summer Monsoon

Impacts of Coastal SST Variability on the East Asian Summer Monsoon

作     者:黄安宁 张耀存 高新房 

作者机构:Department of Atmospheric Sciences Nanjing University 

出 版 物:《Advances in Atmospheric Sciences》 (大气科学进展(英文版))

年 卷 期:2007年第24卷第2期

页      面:259-270页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

基  金:We are grateflu to NCEP/NCAR for releasing the reanalysis data.The constructive comments and suggestions from two anonymous reviewers inproved the quality of paper treatly .This word was supported by the National Natural Science Foundation of China(Grant No.40333026) 

主  题:SST variability coastal oceans East Asian monsoon numerical simulations 

摘      要:The impacts of the seasonal and interannual SST variability in the East Asia coastal regions (EACRSST) on the East Asian summer monsoon (EASM) have been examined using a regional climate model (PδRCM9) in this paper. The simulation results show that the correlation between the EACRSST and the EASM is strengthened after the mid-1970s and also the variability of the EACRSST forcing becomes much more important to the EASM interannual variability after the mid-1970s. The impacts of the EACRSST on the summer precipitation over each sub-region in the EASM region become weak gradually from south to north, and the temporal evolution features of the summer precipitation differences over North and Northeast China agree well with those of the index of EASM (IEASM) differences. The mechanism analyses show that different EACRSST forcings result in the differences of sensible and latent heat flux exchanges at the air-sea interface, which alter the heating rate of the atmosphere. The heating rate differences induce low level air temperature differences over East Asia, resulting in the differences of the land-sea thermal contrast (LSTC) which lead to 850 hPa geopotential height changes. When the 850 hPa geopotential height increases over the East Asian continent and decreases over the coast of East China and the adjacent oceans during the weakening period of weakens consequently. On the contrary, the EASM enhances during the strengthening period of the LSTC.

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