摘要
本文提出用二次随机振动的海气相互作用的模式解释了关于存在太平洋地区海温准三年及半年周期振荡的物理机制,探讨在模式中各个反馈系数之间的关系和作用。认为云在准三年周期振荡过程中起着重要作用,而在准半年周期振荡中自身反馈过程则是主要的过程。
In this paper,by using the second order stochastic fluctuational model,the physical mechanism of the quasi three-yearly and half-yearly oscillation of the sea surface temperature in the North-Western Pacific Ocean is given.It is found that clouds play an important role in the feedback process of quasi three-yearly oscillation,and that the self feedback process is important in the quasi halfyearly oscillation.
作者
李麦村
黄嘉佑
Li Maicun;Huang Jiayou(Institute of Atmospheric Physics,Academia Sinica;Department of Geographics,Peking University)
出处
《气象学报》
1984年第2期168-176,共9页
Acta Meteorologica Sinica
