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 ...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 circulation systems in the two years. It is found that the difference in E1 Nifio events has shaped the rainfall patterns in the two years of 1998 and 2010. At last, the case of 2010 was compared with the composite of historical E1 Nifio Modoki events, and the results indicate that the impact of E1 Nifio Modoki varies from case to case and is more complicated than previously revealed.展开更多
基金Supported by the National Key Basic Research and Development (973) Program of China (2012CB417403)China Meteorological Administration Special Public Welfare Research Fund (GYHY201006022 and GYHY200906018)
文摘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 circulation systems in the two years. It is found that the difference in E1 Nifio events has shaped the rainfall patterns in the two years of 1998 and 2010. At last, the case of 2010 was compared with the composite of historical E1 Nifio Modoki events, and the results indicate that the impact of E1 Nifio Modoki varies from case to case and is more complicated than previously revealed.
