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急流的的英文

  • rushing

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  • 例句与用法
  • Strongly strengthening of the low level jet and releasing of the latent heat of condensation have effect on the occurrance of the disturbance of the moist potential vorticity in low lever , which is important conditions to the genesis and development of mesoscale vortex
    低空急流的加强以及凝结潜热的释放均可以影响到低层湿位涡扰动的产生,从而有利于中尺度低涡的生成和发展。减弱低空急流的对比实验证明了低空急流在对流层中低层中尺度低涡的生成和发展过程中起着关键性作用。
  • The trend of high level jet had great relation to the motion of southwest vortex . when the east of china lay in the region of northwest jet , the southwest vortex was stable because this influence benefited for maintaining the eastern ridge . when the east of china lay in the region of west jet , the ridge moved to the east and the southwest vortex moved to the east rapidly
    高空急流的走向与西南涡的活动关系密切,当我国东部位于西北风急流时,由于这种形势有利于东部高脊的维持,所以西南低涡稳定少动:西风急流时,高脊东移,西南涡也快速东移;西南风急流时,西南涡加强,移速减慢。
  • The results show that there are two centers of occurrence of llsw respectively in dong bei and jiang nan ; the regional torrential rain over the yangtze river basin is closely associated with llsw during the major periods of heavy rainfall ; the diurnal variation of the number of occurrence in the middle and low reaches of the yangtze river is the strongest in china there are some significant differences between llj and nallsw in positive season , spatial variation , diurnal variation and field of pressure . by the way , the important effect of inertial stability on heavy rainfall with both low level south - westerly jet and high level northerly strong flow is analyzed theoretically . the results show that the existence of the maximum of inertial stability in the left font of the low level jet is favor of the accumulation of the moist thermal energy , and conditional symmetric instability or convective instability can be expected in this region
    另外,惯性稳定性的作用以往不受重视,本文通过对西南低空急流左前方和高空偏北大风轴右后方的惯性稳定性和对称稳定性的理论分析和实例计算,表明惯性稳定性在伴有高低空急流的暴雨中有重要意义,揭示了梅雨暴雨的一种新的高低空急流耦合机制:低空急流左前方惯性稳定度大值区的存在,有利于低层湿热能量的积累,使低层倾斜对流的不稳定发展更多期望于条件性对称不稳定或对流不稳定;高空偏北大风轴(西风急流)的存在,是其右后方(右侧)出现对称不稳定的有利条件,高空相对容易出现干对称不稳定;惯性稳定性的作用,使低层的倾斜对流更偏向于垂直方向,有利于对流发展,使高层的倾斜对流更偏向于水平方向,有利于高层辐散。
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