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.