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《SCIENTIA ATMOSPHERICA SINICA》 2000-04
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Interactions between Subsurface Ocean Temperature Anomalies in the Western Pacific Warm Pool and ENSO Cycle

Mu Mingquan and Li Chongyin (State Key Laboratory of Numerical Modeling Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)  
This paper further studies relationship between anomalies of subsurface ocean temperature in the western Pacific Ocean warm pool and ENSO cycle. Results of composite and correlation analyses disclose that anomalies of subsurface ocean temperature in the warm pool and their eastward propagation have very important and direct effects on the occurrence of ENSO. Actually, the anomalous zonal wind at the equatorial western Pacific is the main force to push the anomalies of subsurface ocean temperature in the warm pool to propagate and expand eastwards. However, the anomalously zonal wind is the result of the anomalous winter monsoon in East Asia in our previous studies. So, it clearly reflects the indirect but important influence of the anomalous winter monsoon in East Asia on the eastward-propagation of the subsurface ocean temperature anomalies in the western Pacific warm pool. Through further analyses, we also find that the anomalies of subsurface ocean temperature propagate westwards and come back from the eastern Pacific Ocean to the warm pool along 10~20 o N after ENSO occurrence, and cause subsurface ocean temperature anomalies in the warm pool. Therefore, the anomalies of subsurface ocean temperature in the western Pacific warm pool strikingly interact with ENSO cycle.
【Fund】: 国家重点基础研究发展规划项目!G1 9980 4 0 90 0项目第一部分;; 国家自然科学基金资助项目!4 963 51 80、4 982 3 0 0 2资助
【CateGory Index】: P732
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