首页> 外文会议>Atmospheric and Environmental Remote Sensing Data Processing and Utilization II: Perspective on Calibration/Validation Initiatives and Strategies >Air-sea coupling features from the warm phase to the cold phase of ENSO cycles in the seventies to the eighties
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Air-sea coupling features from the warm phase to the cold phase of ENSO cycles in the seventies to the eighties

机译:从70到80年代ENSO周期的暖期到冷期的海海耦合特征

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摘要

Using the sea surface temperature (SSTA) and wind anomalies (SSWA) of the tropical Pacific from January 1970 to December 1989,main spatial patterns of tropical Pacific SSTA and SSWA coupling features in the transform course from the warm phase to the cold phase of El Nino-southern oscillation (ENSO) cycles are discussed. The main conclusions are as follows: 1) air-sea coupling patterns at the mature stage of El Nino (La Nina) are main spatial ones of tropical Pacific SSWA and SSTA coupling; 2) at the mature stage of El Nino, the interaction of the anticgclonic anomaly wind,generated by the forcing of distinct meridional SSTA gradient in the northern Hemisphere tropical central Pacific, with the California cold current and SSTA is mainly responsible for weakening of El Nino; 3) the second sea temperature increase along the south American coast in the decaying course of El Nino results from the eastward movement of the weakened positive SSTA in the tropical central-eastern Pacific forced by anomalous west wind stress; 4) La Nina results from the joint effect of Walker circulation, Ekman drift and negative SSTA in the tropical central-eastern Pacific.
机译:利用1970年1月至1989年12月热带太平洋海表温度(SSTA)和风距平(SSWA),热带太平洋SSTA和SSWA耦合的主要空间格局在从El的暖相到冷相的转换过程中具有特征。讨论了南南振荡(ENSO)周期。主要结论如下:1)厄尔尼诺(La Nina)成熟期的海-海耦合模式是热带太平洋SSWA和SSTA耦合的主要空间模式; 2)在厄尔尼诺现象的成熟阶段,北半球热带中太平洋北部经向子午SSTA梯度的强迫产生的背斜异常风与加利福尼亚的冷流和SSTA的相互作用是厄尔尼诺现象减弱的主要原因。 ; 3)在厄尔尼诺现象的衰减过程中,沿南美海岸的第二次海温上升是由于西风异常导致热带正中太平洋减弱的正SSTA向东运动所致; 4)拉尼娜是热带中东部太平洋沃克环流,埃克曼漂移和负SSTA共同作用的结果。

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