海温作用与低频振荡
A BAROTROPIC SEMI-GEOSTROPHIC MODEL WITH EVAPORATION-WIND FEEDBACK MECHANKM AND LOW-FREQUENCY OSCILLATION
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摘要: 根据低纬地区地表温度高、蒸发及降水量大、辐合上升运动剧烈等特点,本文构造了一个正压模式的方程组,提示出影响低纬大气波动的一个重要因素——海表温度SST。研究指出:(1)当SST<25℃时,含蒸发风反馈机制的Rossby波向西传播,当SST>25℃时.含蒸发风反馈机制的Rossby波向东传播。(2)SST的数值越高,空气越潮湿,含蒸发风反馈机制的Rossby波传播速度就越小。当SST超过29℃时,会形成周期为30天的低频振荡。Abstract: In consideration of characteristics of low latitude area, such as high surface te perature,large amount of precipitation and evaporation, strong convergence and vertical motion, etc, a set of barotropic equations is presented.An important factor, sea surface temperature (SST), which influences remarkably the atmospheric waves in low latitude, is revealed.It is shown that: (a) when SST<25°C, the Rossby waves with evaporation-wind feedback propagate westward, when SST>25°C, the Rossby waves with evaporation-wind feedback propagate eastward, (b) the warmer the SST, and the wetter the air, the slower the speed of the Rossby waves with evaporation-wind feedback will be; the intraseasonal oscillations with the period of 30-40 day occur for SST>29°C.
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