...暖气团(warm air mass) 一团大规模的空气在一地滞留久了之后,因受地面影响,其温度、湿度等物理性质,在水平方面趋向均一,此团空气称为气团(air mass).
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warm air-mass 暖气团
The results indicated that foehn effect in special topography, the maintenance of warm air mass in low-altitude and the urbanization effect had strengthened high-temperature.
通过对典型高温日影响因素的分析发现：特殊地形下的焚风效应、中低空暖气团的维持以及城市化效应，均对高温强度有加剧作用。
The wind, which is a mass of moving air, will be carrying much water vapor, because the air is warm and has just absorbed water from the gulf.
这风是一团移动的空气，将夹带许多水汽，因为空气缓和，刚从海湾吸收过水分。
In the rise process, the atmosphere cools gradually, if in the warm spatial air mass includes the massive moisture contents, will form the rain;
在上升过程中，大气逐渐冷却，如果暖空气团中含有大量的水分，就会形成雨；
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