经典大气热力学中的湿绝热过程和假绝热膨胀过程也只是它的一种特殊情况。
Of course, the moist adiabatic process and the pseudo adiabatic process in classical atmosphere thermodynamics are also its special instance.
以湿绝热过程的变态方程为积分方程，由卫星TBB资料反演出大气中各等压面层湿度场。
Taking the wet-adiabatic equation as integral equation, the humidity field on each standard isobaric surface derived from satellite TBB-data is used to improve the model initial conditions.
以湿绝热过程的变态方程为积分方程，由卫星TBB资料反演出大气中各等压面层湿度场。
Taking the wet-adiabatic equation as integral equation, the humidity field on each standard isobaric surface derived from satellite TBB-data is used to improve the model initial conditions.
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