The result shows that the atmosphere response to the ocean is mainly the Gill-type mode and simultaneously, the ocean is affected by Ekman pumping from the wind stress vorticity of the low level atmosphere.

 
  • 结果显示;大气对海洋热力强迫的响应主要是Gill型;而大气又可以通过风应力旋度造成的Ekman抽吸作用来影响海洋;这种海气相互作用影响着ENSO循环的发展.
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