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大气热力强迫和动力强迫的调配及平均经圈环流的仿真模拟
引用本文:吴国雄,蔡雅萍.大气热力强迫和动力强迫的调配及平均经圈环流的仿真模拟[J].Acta Meteorologica Sinica,1994,52(2):138-148.
作者姓名:吴国雄  蔡雅萍
作者单位:大气科学和地球流体力学国家重点实验室,中国科学院大气物理研究所
基金项目:国家基础性研究重大关键项目,"气候动力学和气候预测理论的研究"的资助
摘    要:通过研究平均经围环流(MMC)及其所受的内外强迫作用的相互配置,指出对MMC的热力和动力强迫满足确定的调配率。这一调配率受大气内在的斜压性、静力稳定度及绝对涡度制约。利用辐射加热和凝结加热参数化方案,结合欧洲中期天气预报中心(ECMWF)的分析资料,对1月份平均经围环流进行数值仿真模拟。结果表明,热带对流加热可以形成双层Hadley环流结构;涡动动量输送对双Hadley环流的形成也有一定影响。中高纬度的MMC则主要由外动量强迫及大气的动量和热量输送特征决定。

关 键 词:平均经圈环流,热力强迫,动力强迫
收稿时间:1992/3/11 0:00:00
修稿时间:1992/6/11 0:00:00

MODULATION OF ATMOSPHERIC THERMAL AND MECHANICAL FORCING AND NUMERICAL MODELING OF MEAN MERIDIONAL CIRCULATION
Wu Guoxiong and Cai Yaping.MODULATION OF ATMOSPHERIC THERMAL AND MECHANICAL FORCING AND NUMERICAL MODELING OF MEAN MERIDIONAL CIRCULATION[J].Acta Meteorologica Sinica,1994,52(2):138-148.
Authors:Wu Guoxiong and Cai Yaping
Institution:Laboratory of Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100080;Laboratory of Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100080
Abstract:Upon investigating the relative locations of internal and external forcing and the resultant mean meridional circulation, it is found that thermal forcing and mechanical forcing for the formation of atmospheric mean meridional circulation are modulated by a certain ratio. This ratio is determined by the inherent baroclinity, static stability and absolute vorticity of the atmosphere.By employing a parameterization scheme for radiative heating and condensation heating, together with the analysis data of the European Center for Medium-range Weather Forecasts, the mean meridional circulation for January was simulated numerically. It was found that latent heat release in the tropics may result in the formation of double-layered Hadley circulation, so may the eddy momentum transfer processes. On the other hand, mean meridional circulations in extra-tropics are mainly determined by external momentum forcing and atmospheric properties of eddy momentum and heat transfer.
Keywords:Mean meridional circulation  Thermal forcing  Mechanical forcing    
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