本文主要研究内容
作者（2019）在《Multi-scale Analysis of a Hailstorm and Short-time Heavy Rainfall Process in Hohhot City》一文中研究指出：Based on the conventional observation data,satellite,radar,automatic observation and other refined monitoring data,the severe hail weather in Hohhot City on July 29,2015 was analyzed at multiple scales. The results showed that from the perspective of synoptic-scale system,high-altitude cold air invaded Mongol shortwave trough,and the North China small high pressure and the subtropical high formed a warm shear line;the surface convergence line triggered severe convection weather. Unstable vertical structure,continuous increase of low-level humidity,more drier of high altitudes and the wind direction shear at 180° triggered hailstorm and lightning weather in Hohhot. α-scale convective cloud clusters were maintained in Hohhot,and the ground " herringbone" shear line oscillated violently between the north and the south. Strong lightning and big hails appeared on the ground. The " herringbone" shear line lifted slowly to the north,and there was short-time heavy precipitation on the ground. Radar products showed " bow echo",and the echo had a hanging structure; a mesoscale cyclone was formed 3 km away from the ground. On the radar wind profile,it can be seen that low-layer warm advection and strong wind shear triggered strong hailstorm in Hohhot. The disappearance of lowlevel warm advection and the maintenance of strong vertical shear of wind produced short-time heavy precipitation. There was a small difference between short-time heavy precipitation and hail in echo top height,but the coverage was significantly reduced. In Hohhot City,vertically integrated liquid water content quickly increased during the hail,and decreased during the short-time heavy precipitation.
Abstract
Based on the conventional observation data,satellite,radar,automatic observation and other refined monitoring data,the severe hail weather in Hohhot City on July 29,2015 was analyzed at multiple scales. The results showed that from the perspective of synoptic-scale system,high-altitude cold air invaded Mongol shortwave trough,and the North China small high pressure and the subtropical high formed a warm shear line;the surface convergence line triggered severe convection weather. Unstable vertical structure,continuous increase of low-level humidity,more drier of high altitudes and the wind direction shear at 180° triggered hailstorm and lightning weather in Hohhot. α-scale convective cloud clusters were maintained in Hohhot,and the ground " herringbone" shear line oscillated violently between the north and the south. Strong lightning and big hails appeared on the ground. The " herringbone" shear line lifted slowly to the north,and there was short-time heavy precipitation on the ground. Radar products showed " bow echo",and the echo had a hanging structure; a mesoscale cyclone was formed 3 km away from the ground. On the radar wind profile,it can be seen that low-layer warm advection and strong wind shear triggered strong hailstorm in Hohhot. The disappearance of lowlevel warm advection and the maintenance of strong vertical shear of wind produced short-time heavy precipitation. There was a small difference between short-time heavy precipitation and hail in echo top height,but the coverage was significantly reduced. In Hohhot City,vertically integrated liquid water content quickly increased during the hail,and decreased during the short-time heavy precipitation.
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