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饱和湿空气动力学的基本方程和主要特征
引用本文:王两铭,罗会邦.饱和湿空气动力学的基本方程和主要特征[J].气象学报,1980,38(1):44-50.
作者姓名:王两铭  罗会邦
作者单位:中央气象局气象科学研究院天气气候研究所 (王两铭),中山大学气象系(罗会邦)
摘    要:本文从大气热力学的基本特征出发,引入了代表饱和湿空气焓的特征量的广义温度,并推导了一组饱和湿空气动力学方程组。还提出了温平衡风(或称湿地转风)、假相当位温风(或称湿热成风)的概念;对低空急流等若干基本特征也作了探讨。

收稿时间:1979/3/29 0:00:00
修稿时间:7/6/1979 12:00:00 AM

THE BASIC DYNAMIC EQUATIONS AND THE MAIN PROPERTIES OF THE SATURATED MOIST AIR
Wang Liang-ming and Luo Hui-bang.THE BASIC DYNAMIC EQUATIONS AND THE MAIN PROPERTIES OF THE SATURATED MOIST AIR[J].Acta Meteorologica Sinica,1980,38(1):44-50.
Authors:Wang Liang-ming and Luo Hui-bang
Institution:Research Institute of Weather and Climate, Central Meteorological Service;Department of Meteorology, Zhongshan University
Abstract:By use of the so-called generalized temperature of the saturated moist air, a characteristic quantity representing the enthalpy of the air and a set of dynamic equations are derived. On the basis of them, the concept of the moistbalanced wind (or moist geostrophic wind) and that of pseudoequivalent temperature wind (or moist thermal wind) are suggested, Finally, some fundamental behaviours of low-level jet streams are studied.
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