The boundary line between stability and instability is the dry adiabatic lapse rate line.

稳定的和不稳定的界限就是干的绝热垂直率线。

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Several calculation methods of the thickness of atmospheric mixed layer, such as national standards method, dry adiabatic method, Nozaki method, were studied in this paper.

论述了大气混合层厚度的多种计算方法如国标法、干绝热法、罗氏法等，并分析了大气混合层厚度的各种影响因子。

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Several calculation methods of the thickness of atmospheric mixed layer, such as national standards method, dry adiabatic method, Nozaki method, were studied in this paper.

论述了大气混合层厚度的多种计算方法如国标法、干绝热法、罗氏法等，并分析了大气混合层厚度的各种影响因子。

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