绝热增温
jué rè zēnɡ wēn
- 名adiabatic heating
绝热增温-
当这种环状波动模处于正位相时，异常增强的绝热下沉增温效应和减弱的冷空气活动共同使得高原上空对流层中、低层气温异常偏暖。
When this annular-wave mode in its positive phase , the integrated effect of the weakened cold air intrusion and enhanced adiabatic descent leads to the anomalous warm in the mid-and lower-troposphere over the plateau .
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可以说，安徽沿江地区局地温度的增温主要来自于非绝热项，增温比例常常超过95%，它对局地温度的升高具有举足轻重的作用。
The local temperature increment in Anhui is mainly from non-adiabatic term , and it takes significant role in local temperature increment .