不同层等压面之间温度水平分布不均匀，使地转风随高度产生的变化，称为热成风（关系）。
大气扰动以热成风的方向运动过程。
The movement of an atmospheric disturbance in the direction of the nearest thermal wind.
用热成风适应物理过程来解释这种天气区分布的原因。
This distributions of weather can be explained by the adjustment physical process of thermal wind.
本文根据热成风适应原理，分析了中亚低压的东移问题。
According to the principle of the thermal wind adjustment, the problem of Central Asia depression moving to east have been discussed.
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