| 饱和湿空气热力学的基本特征 |
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| 引用本文： | 王两铭.饱和湿空气热力学的基本特征[J].气象学报,1980,38(2):106-110. |
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| 作者姓名： | 王两铭 |
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| 作者单位： | 中央气象局气象科学研究院 |
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| 摘 要： | 本文把凝结过程的初期看作是系统的一种广义绝热过程,而把凝结潜热看作是系统总位能的一个部分。从这个基本思想出发,探讨了饱和湿空气中一些热力学的基本特征。结果表明:当把测量温度T改用广义温度T~*作为独立变量后,干空气中的热力学基本特征都将在饱和湿空气中得到对应的结果。这对研究我国夏季汛期降水以及对大气数值模式的设计,或许有所裨益。
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| 收稿时间： | 1979/3/29 0:00:00 |
| 修稿时间： | 9/1/1989 12:00:00 AM |
SOME FUNDAMENTAL THERMODYNAMIC PROPERTIES OF THE SATURATED MOIST AIR |
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| Wang Liang-ming.SOME FUNDAMENTAL THERMODYNAMIC PROPERTIES OF THE SATURATED MOIST AIR[J].Acta Meteorologica Sinica,1980,38(2):106-110. |
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| Authors: | Wang Liang-ming |
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| Institution: | Academy of Meteorological Science, Central Meteorological Service |
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| Abstract: | Considering the condensation process at the initial stage as a generalized adiabatic process and the latent heat of condensation as an inseparable part of the total potential energy of a closed system, we have studied the fundamental thermodynamic properties of the saturated moist air. The results show that all the properties of the dry air could he retained in the saturated moist air, provided the air temperature T is replaced by the so-called generalized temperature T* as an independent variable. |
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