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在热对流初期，对流高度逐渐抬高，伴有较强上升速度的热对流泡逐渐升高的现象。
At the beginning of the heat convection, thermal bubbles associated with a stronger updraft move upward to a higher level.
假设自由对流高度为云底高度，考虑模式模拟次网格尺度降雨的云下拖曳清除作用。
Supposing that the level of free convection is equal to the cloud bottom level, we considered the pulling effects of simulated sub-grid scale precipitation, which is under clouds.
一达到对流层，温度就停止随高度上升。
As soon as the tropopause is reached, temperature stops decreasing with height.
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