海河流域“16·7”大暴雨洪水成因初步分析
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魏琳(1983-),女,山东冠县人,硕士,主要从事水文气象情报预报工作。 E-mail: linweihhu@qq.com

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P333.2

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Analysis of “2016·7” Storm Flood in Haihe River Basin
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    摘要:

    采用气象资料对海河流域2016年7月1820日大暴雨进行成因分析,并与历史上"63.8"及"96.8"两次大暴雨对比分析,结果表明:西南涡东移北上,与中纬度高空槽结合并加深,低空急流带来源源不断的水汽,加之地形的有利条件,造成了此次大暴雨。从历史上海河流域大暴雨成因看,主要是由西南涡东移北上及台风北上倒槽系统影响,且移动路径均沿太行山呈西南-东北走向,本次暴雨依然遵循这一规律,整体移动路径介于"63.8"与"96.8"之间。

    Abstract:

    This paper studied the cause of rainstorm occurred in the Haihe River Basin during 18-20 July, 2016 based on the meteorological data, and made comparison between the “1963.8” and “1996.8” storms. The results show that the rainstorm was caused by superimposing of different weather systems and special terrain. It is closely related to water vapor transmission from the South China Sea and East China. The moving path of the rainstorm was from southwest to northeast along the Taihang Mountains. The main influence weather system was similar to the “1963.8” storm, but different from the “96.8” storm. The moving path was between the “1963.8” and “1996.8” storms.

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  • 收稿日期:2016-12-07
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  • 在线发布日期: 2022-06-22
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