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用1976～1989年的地球自转速度、赤道东太平洋海温和气压及大气角动量资料,研究了地气之间角动量交换与ENSO循环的关系结果表明:固体地球自转速度、赤道东太平洋海温、不同纬带及全球大气角动量之间存在着协同的变化关系;低纬局地海气相互作用通过Hadley环流可形成类似ENSO事件的循环;固体地球和全球海气相互作用通过山脉力矩和地转变速摩擦力矩形成了固体地球-海洋-大气系统中各个方面出现的非周期行为和非同步振荡;实际出现的ENSO循环是固海气相互作用反映在太平洋洋盆上的一种现象.
The relationship between the angular momentum exchange and the ENSO cycle was studied using the earth’s rotation velocity from 1976 to 1989, the sea surface pressure and the atmospheric angular momentum data of the eastern equatorial Pacific. Results show that the rotation speed of the solid earth, the SST in the equatorial eastern Pacific, There is a synergistic relationship between different latitudinal latitudes and the global atmospheric angular momentum. At low latitudes, the sea-atmosphere interaction can form a circulation similar to the ENSO event through the Hadley circulation. The interaction between the solid earth and the global air-sea changes through the mountain torque and the transition The instantaneous friction moment forms aperiodic and unsynchronized oscillations in all aspects of the solid Earth-Ocean-Atmosphere system. The actual ENSO cycle is a phenomenon in which the solid-sea interaction is reflected in the Pacific Ocean basin.