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中低纬过渡地区潜热影响下中尺度扰动的对称发展
引用本文:吴勇,欧阳首承.中低纬过渡地区潜热影响下中尺度扰动的对称发展[J].大气科学,1995,19(5):631-635.
作者姓名:吴勇  欧阳首承
作者单位:1.四川涪陵地区国土局,四川涪陵 648000
摘    要:本文引入第二科里奥利参数讨论了中低纬过渡地区含非绝热(潜热)作用的对称扰动波包发展问题。结果表明:这一地区扰动波包的发展不仅包含了中高纬度波包发展条件[1],而且与潜热和基本风场梯度经向切变及波包传播的非垂直性有关。过渡地区基本风场的作用是通过第一和第二科里奥利参数完成的。

关 键 词:中低纬过渡带    扰动波包    第二科里奥利参数

On the Symmetric Development of Mesoscale Disturbances with Non-adiabatic Heating in the Transition Zone of Mid-low Latitudes
Wu Yong and Ouyang,Shoucheng.On the Symmetric Development of Mesoscale Disturbances with Non-adiabatic Heating in the Transition Zone of Mid-low Latitudes[J].Chinese Journal of Atmospheric Sciences,1995,19(5):631-635.
Authors:Wu Yong and Ouyang  Shoucheng
Abstract:This paper studies the symmetric development of mesoscale disturbances with non-acsabatic (latent heat) heating in the transition zone of mid-low latitudes. The results show that the synmetric development of disturbances not only contains the conditions of development of the wavepacket inmid-high latitudes, but also is related to the latent heat and non-verticality of basic now shear gradientwith a wave packet speed. The action of the basic flow in the transition zone of mid-low latitudes depends on the first and the second Coriolis parameters.
Keywords:transition zone of mid-low latitudes  disturbance wave packet  second Coriolis parameter  
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