朱抱真, 陈嘉滨, 张道民, 李泽椿, 葛霭芬. 1983: 一个修改的σ坐标初始方程斜压模式. 气象学报, (2): 167-182. DOI: 10.11676/qxxb1983.019
引用本文: 朱抱真, 陈嘉滨, 张道民, 李泽椿, 葛霭芬. 1983: 一个修改的σ坐标初始方程斜压模式. 气象学报, (2): 167-182. DOI: 10.11676/qxxb1983.019
Zhu Baozhen, Chen Jiabin, Zhang Daomin, Li Zechun, Ge Aifen. 1983: A 5-LAYER PRIMITIVE EQUATIION MODEL IN A MODIFIEDσ-COORDINATES. Acta Meteorologica Sinica, (2): 167-182. DOI: 10.11676/qxxb1983.019
Citation: Zhu Baozhen, Chen Jiabin, Zhang Daomin, Li Zechun, Ge Aifen. 1983: A 5-LAYER PRIMITIVE EQUATIION MODEL IN A MODIFIEDσ-COORDINATES. Acta Meteorologica Sinica, (2): 167-182. DOI: 10.11676/qxxb1983.019

一个修改的σ坐标初始方程斜压模式

A 5-LAYER PRIMITIVE EQUATIION MODEL IN A MODIFIEDσ-COORDINATES

  • 摘要: 本文提出一个修改的σ坐标初始方程数值模式,在模式大气的下层具有σ坐标特性,而上层保持P坐标性质。用它来发展过去所设计的一个包括地形和非绝热作用的初始方程三层模式1。模式提高了空间分解性能,改变了静力关系的差分方案,并与一般的σ坐标作了比较。在物理因子中除辐射、感热、蒸发和大尺度凝结外,本文进一步包括了积云对流的作用。最后给出了预报个例的结果。

     

    Abstract: A 5-layer primitive equation prediction model is developed in a modified σ-coordinates defined as equation (1)and (2), the upper part of the model atmospnere is equivalent to p-coordinates. The new system of governing equations is obtained as equations (8)-(18). Construction of the finite difference scheme is generally similar as 1, but the difference equations of hydrostatic equations are obtained from differentiating them with respect to time as equations (27)-(28).A combined scheme of the leap-frog method and the time smooth method is employed for the explicit integration.The physical factors of orography, friction, horizontal diffusion and nanadiabatic-heating such as radiation, sensible heating, evaporation, large-scale and cumulus scale condensation are included.The model was tested by using objective analysis and compared with the general σ-coordinates. Finally two examples of 48 hours prediction for winter and summer are given in this paper.

     

/

返回文章
返回