江西省副高影响下的强天气形势分析

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Abstract By means of basic statistical methods,morphological analysis and comparative analysis of several cases,using MICAPS routine weather map data,provincial regional station data and sounding data,this paper analyzes the weather situation of hot thunderstorm weather on the edge of Jiangxi subtropical high.The results show that as obvious thunderstorm under subtropical high control type,attention should be paid to capturing the boundary convergence line (shear line) or ground convergence line.When the boundary layer convergence line has obvious southward pressure,it would occur strong convective weather such as strong thunderstorms and lightning,heavy precipitation near the convergence line.The thermal thunderstorms on the edge of subtropical high often cooperate with the convergence line (shear line).If there are more obvious shear lines in the multi-layers,the intensity and scope of thunderstorms will obviously expand,and even lead to strong weather such as heavy rainfall,rainstorms or heavy rainstorms.High-altitude trough is still an important influence system of thunderstorm at the edge of subtropical high.When low-altitude trough approaches,it may appear obvious convective weather due to the upward motion of the front of low-altitude trough.Under the weather background controlled or influenced by subtropical high,typhoon activities often bring strong thunder and lightning weather.

Key words： Jiangxi subtropical high hot thunderstorm thunderstorm gale short-term heavy rainfall

Received: 08 April 2020

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P458.121.1

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	Articles by authors
	Zheng Kani
	Ma Zhongyuan
	Chen Baofa

Cite this article:

Zheng Kani,Ma Zhongyuan,Chen Baofa. Analysis on strong weather situation affected by Jiangxi subtropical high[J]. Meteorological Hydrological and Marine Instrument, 2020, 37(2): 6-10.

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http://www.qxswhy.com/EN/ OR http://www.qxswhy.com/EN/Y2020/V37/I2/6

[1]	姜俊玲,张雪冬,江敦双,等.多种探测产品在副高边缘一次短时预报中的应用[J].气象,2008,34(S1):230-233.
[2]	周雨华,黄小玉,黎祖贤,等.副高边缘暴雨的多普勒雷达回波特征[J].气象,2006,32(1):12-17.
[3]	周淑玲,王仁胜,张丰启.一次副高边缘强对流天气的水汽图像特征[J].气象,2000,26(6):48-51.
[4]	杨熠,简茂球,谢和林.副高外围影响下遵义市区域性暴雨的高空形势场特征研究[J].中低纬山地气象,2018,42(6):15-21.
[5]	金晓青,李江波,于雷,等.河北中部一次具有后向传播特征的副高外围暖区暴雨过程分析[J].沙漠与绿洲气象,2018,12(4):7-14.
[6]	苏永玲,马秀梅,马元仓,等.高空冷涡和副高背景下青海冰雹特征对比分析[J].沙漠与绿洲气象,2018,12(4):22-29.
[7]	张湘华,彭月,张湘玲.副高北侧一次典型强降水过程分析[J].气象水文海洋仪器,2016,33(2):35-38.