结果表明：白天晴空一般都是超绝热不稳定状态，并存在一种逆湿现象，造成向下输送的水气通量。
The results show in general the atmosphere is superadiabatic unstable state and there is a phenomenon of inverse humidity forming downward vapour transportation in cloudless daytime.
结果表明：白天晴空一般都是超绝热不稳定状态，并存在一种逆湿现象，造成向下输送的水气通量。
The results show in general the atmosphere is superadiabatic unstable state and there is a phenomenon of inverse humidity forming downward vapour transportation in cloudless daytime.
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