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Formation of the Anomalous Summer Precipitation in East China in 2010 and 1998: A Comparison of the Impacts of Two Kinds of El Nio

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Acta meteorologica Sinica 2012年第6期26卷 665-682页

作者：王钦李双林付建建李国平 Chengdu University of Information Technology College of Atmospheric Science Nansen-Zhu International Research Centre Institute of Atmospheric Physics Chinese Academy of Sciences Civil Aviation Flight University of China

In the summers of 1998 and 2010, severe floods occurred in the middle and lower reaches of the Yangtze River. Although an El Nifio event took place preceding each of the summer floods, significant differences between the two summer floods and the two E1 Nifio events were identified. The 1997/98 E1 Nifio is a conventional one with strongest warming in the central-eastern pacific, whereas the 2009/10 event is an E1 Nifio Modoki with strongest warming in the central pacific. In this study, summer rainfall anomalies （SRA） in the two years were first compared based on the rainfall data at 160 stations in China's Mainland, and a significant difference in SRA was found. To understand the underlying mechanism for the difference, the atmospheric circulation systems, particularly the western north pacific anticyclone （WNPAC）, the western pacific subtropical high （WPSH）, and the low-level air flows, were compared in the two years by using the NCEP/NCAR reanalysis data. The results display that the WNPAC was stronger in 2010 than in 1998, along with a northwestward shift, causing weakened southwesterly from the Bay of BengM to the South China Sea but intensified southerly in eastern China. This resulted in less water vapor transport from the tropical Indian Ocean and the South China Sea but more from the subtropical western pacific to East Asia. Subsequently, the rainband in 2010 shifted northward. The difference in the WNPAC was causedby the anomalous ascending motion associated with the warming location in the two E1 Nifio events. ~rthermore, the role of tropical sea surface temperature （SST） in modulating these differences was investigated by conducting sensitivity experiments using GFDL AM2.1 （Geophysical Fluid Dynamics Laboratory Atmospheric Model）. Two experiments were performed, one with the observed monthly SST and the other with June SST persisting through the whole summer. The results suggest that the model well reproduced the primary differences in the atmospheric ci

关键词： E1 Nifio and E1 Nifio Modoki summer rainfall in the middle and lower reaches of the YangtzeRiver western north pacific anticyclone AGCM sensitivity experiments

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The ENSO’s Effect on Eastern China Rainfall in the Following Early Summer

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Advances in Atmospheric Sciences 2009年第2期26卷 333-342页

作者：林中达陆日宇 Center for Monsoon System Research Institute of Atmospheric Physics Chinese Academy of Sciences

ENSO＇s effect on the rainfall in eastern China in the following early summer is investigated by using station precipitation data and the ERA-40 reanalysis data from 1958 to 2002. In June, after the E1 Nifio peak, the precipitation is significantly enhanced in the Yangtze River valley while suppressed in the Huaihe River-Yellow River valleys. This relationship between ENSO and the rainfall in eastern China is established possibly through two teleconnections： One is related to the western north pacific （WNP） anticyclonic anomaly in the lower troposphere leading to enhanced precipitation in the Yangtze River valley, and the other is related to the southward displacement of the Asian jet stream （AJS） in the upper troposphere resulting in suppressed precipitation in the Huaihe River-Yellow River valleys. This southward displacement of the AJS is one part of ENSO＇s effect on the zonal flow in the whole northern Hemisphere. After the E1 Nifio peak, the ENSO-related warming in the tropical troposphere persists into the following early summer, increasing the meridional temperature gradient and through the thermal wind balance, leads to the enhancement of westerly flow in the subtropics south of the westerly jet stream and results in a southward displacement of the westerly jet stream.

关键词： ENSO eastern China rainfall early summer Asian jet stream western north pacific anticyclone

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The ENSO effect on eastern China rainfall in the following early summer

The ENSO effect on eastern China rainfall in the following e...

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第七次全国动力气象学术会议

作者： Zhongda LIN and Riyu LU Center for Monsoon System Research,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,100029.

＜正＞ENSO’s effect on the rainfall in eastern China in the following early summer is investigated by using station precipitation data and the ERA-40 reanalysis data from 1958 to *** June,after the El Ni（?）o peak,the precipitation is significantly enhanced in the Yangtze River valley while suppressed in the Huai-Yellow River *** relationship between ENSO and the rainfall in eastern China is possibly established through two teleconnections:One is related to the western north pacific（WNP）anticyclonic anomaly in the lower troposphere leading to enhanced precipitation in the Yangtze River valley,and the other is related to the southward displacement of the Asian jet stream（AJS）in the upper troposphere resulting in suppressed precipitation in the Huai-Yellow River valley. This southward displacement of the AJS is one part of ENSO’s effect on the zonal flow in the whole northern *** the El Ni（?）o peak,the ENSO-related warming in the tropical troposphere persists into the following early summer,increasing the meridional temperature gradient and through the thermal wind balance,leads to the enhancement of westerly flow in the subtropics south of the westerly jet stream and results in a southward displacement of the westerly jet stream.

关键词： ENSO eastern China rainfall early summer Asian jet stream western north pacific anticyclone

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