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     It is found that influence of heating on the barotropic unstable disturbances depends on the disposition of the heating and the flow field;
     结果指出,加热场对东西风带正压不稳定扰动的影响与加热和流场的相对配置有关。
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     Theory of Relativity & Theory of Relative Absoluteness
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It is the purpose of this paper to investigate the effect of large-scale heating on the excitation of unstable disturbances. It is found that influence of heating on the barotropic unstable disturbances depends on the disposition of the heating and the flow field; in the westerly current the stationary wave patterm disturbances may be excited by heating and in the easterly current decaying disturbances may be excited only; the horizontal scale of diabatic heating which excite wavepattern disturbances must beAt...

It is the purpose of this paper to investigate the effect of large-scale heating on the excitation of unstable disturbances. It is found that influence of heating on the barotropic unstable disturbances depends on the disposition of the heating and the flow field; in the westerly current the stationary wave patterm disturbances may be excited by heating and in the easterly current decaying disturbances may be excited only; the horizontal scale of diabatic heating which excite wavepattern disturbances must beAt last, the effect of friction on disturbances is. studied.

文中通过一些简化假定,得到了包括非绝热加热的一参数模式。导得加热存在下的正压不稳定的必要条件是β-d~2u/dy~2+q~2u+S~2H/K=0,研究了大尺度加热对东西风带不稳定扰动及定常波型扰动的作用。结果指出,加热场对东西风带正压不稳定扰动的影响与加热和流场的相对配置有关。此外,大尺度加热可以在西风带激发出定常波型扰动,而在东风带只能产生衰减型扰动。激发西风带定常波型扰动的非绝热加热场的水平半径尺度,应大于L_c=(u/β)~(1/2)。最后还考虑了摩擦的作用。

Coupled equations of rotational and divergent Kinetic energy are used to study the mechanisms for generating and maintaining low-level jets in two real cases with and without heavy rain. As they are accountable by the relative height at which upper and lower jets are lying, individual terms in the equations are analysed with respect to their horizontal distribution. Particularly, it is the direction of enetgy converted between the rotational and divergent components rather than the intensity of the jet that...

Coupled equations of rotational and divergent Kinetic energy are used to study the mechanisms for generating and maintaining low-level jets in two real cases with and without heavy rain. As they are accountable by the relative height at which upper and lower jets are lying, individual terms in the equations are analysed with respect to their horizontal distribution. Particularly, it is the direction of enetgy converted between the rotational and divergent components rather than the intensity of the jet that detemines whether it will be acconipanied by heavy rain. A positive Conversion from divergent to rotational kinetic energy appears to be the neceseary but not sufficient condition for the heavy rain to take place. The intensity and direction of energy conversion depends not only on the relative position of vorticity and diversity feild, but also the vertical profile of the jet.

根据KR和KD方程的各项水平分布,着重讨论伴有暴雨和不伴有暴雨两类低空急流维持的动力过程,指出主要差异在于维持机理不同,尤其是能量转换方向相反,从KD向KR的正转换似乎是暴雨发生的必要但非充分的条件,同时能量转换的强度和方向不仅决定于涡度场和散度场的相对配置,还与急流的垂直分布形式直接有关。

 
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