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Diagnostic Analysis on Heavy Rain Process of the Northeast-moving Southwest Vortex

机译:东北移动西南涡大暴雨过程的诊断分析

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The moving path of southwest vortex and the mechanism of heavy rain in the north were studied in order to find out the forecasting point of the northern heavy rain,so as to improve the forecasting ability of the heavy rain disastrous weather.A large-scale heavy rain process in northern China from 18 to 21 July 2010 was diagnostically analyzed using meteorological conventional and intensified observation data and NCEP 1°× 1° reanalysis data.The result showed that the southwest vortex moved northeastward under the guidance of southwest airflow in the periphery of subtropical high,which was the direct influence system of the heavy rainfall.The heavy rainfall occurred on the east side of the symmetrical axis of the 700 hPa low vortex.The southwest jet provided abundant water vapor and potential instability energy for the occurrence of heavy rainfall.The changes of vorticity advection and temperature advection in the lower and middle troposphere were the leading causes of affecting the development and movement of the low vortex.The low vortex moved along the positive vorticity advection increasing region and the warm advection increasing region.The dry and cold air intruded into the low vortex from the middle layer,which promoted the generation and development of the unstable stratification of upper cold and lower warm,and provided unstable and triggering conditions for heavy rain.The water vapor transport from the Yellow Sea and the Bohai Sea was very abundant,and the water vapor flux was very high,reaching 30 g/(s·cm·hPa).It was the main reason for the maximum precipitation in Liaoning Province,which was the farthest from the southwest vortex source.The study deepened the understanding of the structural characteristics of the southwest vortex and revealed the dynamic mechanism of the northeast movement and development of the southwest vortex as well as the cause of rainstorm induced by interaction with other weather systems.It can provide some forecasting ideas and useful references for forecasting the movement of the southwest vortex and the heavy rain weather in the north.
机译:研究了西南涡的运动路径和北部大暴雨的机理,以找出北部大暴雨的预报点,从而提高了暴雨灾害性天气的预报能力。利用常规气象和强化观测数据以及NCEP 1°×1°再分析数据对2010年7月18日至21日中国北方的降雨过程进行了诊断分析,结果表明西南涡在西南气流的引导下向东北移动。副热带高压是强降水的直接影响系统。强降水发生在700 hPa低涡旋对称轴的东侧。西南喷流为暴雨的发生提供了丰富的水汽和潜在的不稳定能量。对流层中低层涡度对流和温度对流的变化是影响对流发展的主要原因低涡的展开和运动。低涡沿着正涡对流增加区和暖对流增加区移动。干冷空气从中层侵入低涡,促进了不稳定涡的产生和发展。上,冷,下暖分层,为大雨提供了不稳定的触发条件。黄海和渤海的水汽输送非常丰富,水汽通量很高,达到30 g /(s· (cm·hPa)。这是辽宁省降水量最大的原因,是距西南涡旋源最远的地方。该研究加深了对西南涡旋结构特征的认识,揭示了东北向运动的动力机制。西南涡的形成和发展以及与其他天气系统相互作用引起的暴雨成因。它可以提供一些预报思路和利用对预测西南涡旋运动和北部大雨天气的参考。

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