在积云中，每秒几米的对流上升速度造成的冷却速率为每分钟几度。

In cumulus convection ascent rates of several metres a second give a cooling rate of a few degrees per minute.

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本文利用FACE（佛罗里达积云试验）1978年夏季积云飞机实测资料，对微物理过程的垂直连续性及其和上升气流的关系进行了研究。

An experiment to examine the vertical continuity of microphysical processes in relation to the supporting updrafts was conducted during the Florida Area Cumulus Experiment (FACE) in 1978.

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