Analysis on the Impact of Typhoon HAITANG on Heilongjiang Province

Xiaoxue Wang, Jiaying Zhao, Mei Zhao, N. Zhao
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Abstract

In August 2017, Heilongjiang Province was affected by the weakening of the typhoon HAITANG, which turned into a low-pressure system northward, causing a heavy rainstorm. The data used in this paper was obtained from the 2.5°×2.5°NCEP reanalysis dataset, conventional observation data and FY-2C2D satellite images. Starting from the large-scale circulation situation, analyze the physical mechanism of the heavy rain in Heilongjiang Province and the characteristics of satellite images. The results show that typhoon HAITANG degenerates into a low pressure system that carries lots of warm and humid air northward, which is combined with the cold air in the north. Heilongjiang Province is affected by the interaction of warm and cold air. The large value area of water vapor convergence overlaps with the center of pressure and moves northeast with it. At the same time, the water vapor convergence gradient is relatively large, which is a good corresponding relationship with the appearance of heavy rainfall areas. The low-level convergent and high-level divergent circulation conditions are conducive to the maintenance of low-level ascending movement and provide favorable conditions for the occurrence of heavy rainstorms. Heavy rainstorms mainly occur in areas where the cloud system is thicker and densely structured, where the upward movement is relatively strong. Key words: Typhoon HAITANG, water vapor convergence, satellite images
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台风“海棠”对黑龙江省的影响分析
2017年8月,黑龙江省受台风“海棠”减弱影响,向北转变为低压系统,造成大暴雨。本文使用的数据来自2.5°×2.5°NCEP再分析数据集、常规观测数据和FY-2C2D卫星图像。从大尺度环流形势出发,分析了黑龙江省此次暴雨的物理机制和卫星图像特征。结果表明:台风海棠退化为一个带大量暖湿空气北上的低压系统,并与北方冷空气结合。黑龙江省受冷暖空气相互作用的影响。水汽辐合大值区与气压中心重叠,并随气压中心向东北移动。同时,水汽辐合梯度较大,与强雨区出现有较好的对应关系。低层辐合和高层辐散的环流条件有利于低层上升运动的维持,为强暴雨的发生提供了有利条件。强暴雨主要发生在云系较厚、结构较密、上升运动较强的地区。关键词:台风海棠,水汽辐合,卫星图像
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