胡伯威. 1981: 副热带天气尺度和次天气尺度系统短期演变的一般机制. 气象学报, (4): 429-440. DOI: 10.11676/qxxb1981.046
引用本文: 胡伯威. 1981: 副热带天气尺度和次天气尺度系统短期演变的一般机制. 气象学报, (4): 429-440. DOI: 10.11676/qxxb1981.046
Hu Bo-wei. 1981: THE GENERAL MECHANISM OF SHORT-RANGE DEVELOPMENT FOR SYNOPTICAL SCALE AND SUBSYNOPTICAL SCALE SYSTEM IN SUBTROPICAL ZONE. Acta Meteorologica Sinica, (4): 429-440. DOI: 10.11676/qxxb1981.046
Citation: Hu Bo-wei. 1981: THE GENERAL MECHANISM OF SHORT-RANGE DEVELOPMENT FOR SYNOPTICAL SCALE AND SUBSYNOPTICAL SCALE SYSTEM IN SUBTROPICAL ZONE. Acta Meteorologica Sinica, (4): 429-440. DOI: 10.11676/qxxb1981.046

副热带天气尺度和次天气尺度系统短期演变的一般机制

THE GENERAL MECHANISM OF SHORT-RANGE DEVELOPMENT FOR SYNOPTICAL SCALE AND SUBSYNOPTICAL SCALE SYSTEM IN SUBTROPICAL ZONE

  • 摘要: 将包含水汽潜热和摩擦因子的平衡模式ω方程适当简化,形式上与准地转方程相似,在简单谐波分布的假定下,由此求得各标准气压层上垂直运动和涡度倾向的近似解析解,它是包含所有各气压层上涡度源变和温度源变(或称“广义平流”)以及地形强迫作用的一组线性多项式。各项的系数分别表现出该项源变或地形强迫作用对某一气压层上垂直运动或涡度倾向的影响。针对几种典型情况,计算出这些影响系数,这有助于定性地诊断天气尺度和次天气尺度系统短期演变的物理过程,适用于副热带情况。

     

    Abstract: In this paper, based on the system of equations quantitatively describing the equilibyium model, with consideration of latent heat and frictional stress, and assuming rmonics, for the horizontal distribution of the field take the form of the approximate analytical solutions of vertical velocity and vorticity tendency on the standard level were obtained.The solutions were a set of linear polynomial in which all the term of thermal advection and vorticity advection were included, the values of these coefficients in the polynomial demonstrated the effect of these advection term on the vertcal velocity or vortcity tendency respectively. The coefficient were calculated for several standard cases. These might be help to explore qualitatively the main physical process of the development of synoptical and subsynoptical scale systems. It seems available in subtropical situation.

     

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