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《大气科学进展(英文版)》 2001-04
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Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle

LiChongyin LASG, Institute of Atmospheric Physics, Beijing 100029 Sun Shuqing Institute of Atmospheric Physics, Beijing 100080 Mu Mingquan LASG, Institute of Atmospheric Physics, Beijing 100029  
Based on the data analyses by using NCEP/ NCAR reanalysis data and other data (OLR, precipitation and temperature), it is shown that the tropospheric circulation and climate in East Asia and the northwestern Pacific region have the evident quasi-biennial oscillation (TBO) feature. It is also shown that anomalous East Asian winter monsoon can impact the atmospheric circulation and climate variations in the following summer, particularly in East Asian region; there is clear interaction between anomalous East Asian winter monsoon and ENSO cycle. The continuous strong (weak) East Asian winter monsoon can excite El Ni o (La Ni a) through the air-sea interaction, the El Ni o (La Ni a) event can lead the East Asian winter monsoon to be weak (strong) through the teleconnections or remote responses. The strong or weak winter monsoon and ENSO cycle are linked each other. It can be suggested that interaction between anomalous East Asian winter monsoon and ENSO cycle is a fundamental origin of the TBO.
【Fund】: National Key Basic Science Program in China (G1998040900);; NSFC (49823002).
【CateGory Index】: P732
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