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《Chinese Journal of Geophysics》 2008-06
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Mei-yu,Arctic Oscillation and stratospheric circulation anomalies

LI Chong-Yin1,2,GU Wei1,3,PAN Jing11 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China2 Meteorological College,PL A University of Science and Technology,Nanjing 211101,China3 Climate Center,China Meteorological Administration,Beijing 100081,China  
How about the influence of stratospheric process on the climate as a scientific problem has been paid more attentions in the world.So that there is a special subproject-SPARC in the WCRP.Based on the data analyses,it is shown in this paper that mei-yu precipitation may be influenced by the stratospheric atmosphere circulation anomaly through the Arctic Oscillation(AO) in the troposphere.The stratospheric atmosphere circulation in February is closely related to the AO in March.It may affect the AO through the downward propagating wave activity anomalies.The EOF1st and EOF3rd leading modes of 30hPa geopotential height in February are significantly associated with anomalous downward E-P flux in the subtropics and the polar region,respectively.The AO in March may in turn exert an influence on summertime circulation in East Asia,which is closely related to the summertime thermal condition of the tropospheric atmosphere over East Asia.The changes of thermal condition and the circulation over East Asia can then lead to anomalous convergence/divergence in Yangtze River Valley,and the anomaly of mei-yu precipitation.
【Fund】: 国家自然科学基金项目(40705023);; 科技部国家973项目(2007CB411805)资助
【CateGory Index】: P434
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