湖北农业科学 ›› 2021, Vol. 60 ›› Issue (7): 15-23.doi: 10.14088/j.cnki.issn0439-8114.2021.07.003

• 资源·环境 • 上一篇    下一篇

安徽省高山站与周边站暴雨及其大气环流特征分析

丁从慧, 邱学兴, 杨祖祥   

  1. 安徽省气象台,合肥 230061
  • 收稿日期:2020-06-22 出版日期:2021-04-10 发布日期:2021-04-25
  • 作者简介:丁从慧(1990-),女,江苏盐城人,工程师,硕士,主要从事短时天气预报研究工作,(电话)18156092326(电子信箱)dconghui45@sina.com。
  • 基金资助:
    气象局预报员专项(kY201612); 国家自然科学基金项目(41805080)

Analysis of rainstorm and its atmospheric circulation characteristics in high station and its surrounding stations in Anhui province

DING Cong-hui, QIU Xue-xing, YANG Zu-xiang   

  1. Anhui Meteorological Observatory, Hefei 230061, China
  • Received:2020-06-22 Online:2021-04-10 Published:2021-04-25

摘要: 利用安徽省近年来黄山站、九华山站(高山站)及其周边站逐日降水资料,统计分析高山站和周边站降水特征指标、风场分布,使用正交经验分解(EOF)分析安徽省暴雨高度场特征。结果表明,高山站的降水指标均高于周边站,降水多集中在6—8月,黄山、九华山多年平均降水量(降雨日)分别为2 290.3 mm(197.7 d)、2 077.6 mm(187.7 d),多年平均暴雨强度(暴雨日)分别为83. 3 mm/d(8.5 d)、79.6 mm/d(7.7 d),其中主要影响高山站暴雨为700 hPa偏西风,一定海拔内的地形对降雨起到促进作用;对500、850 hPa高度平均场进行EOF分析,黄山、九华山500 hPa第一模态主要分别呈纬向、经向型分布,850 hPa第一模态均呈经向型分布,其中500、850 hPa环流形势分别对黄山、九华山暴雨影响更大,因此通过探讨高山站与周边站降水、大气环流等特征研究,以期为山区降水预报提供科学的指导。

关键词: 暴雨, 降水指标, 正交经验分解(EOF), 黄山, 九华山

Abstract: By using the daily precipitation data of Huang mountain station, Jiuhua mountain station (high stations) and surrounding stations in Anhui province in recent years, the precipitation characteristics and wind field distribution of high stations and surrounding stations were statistically analyzed, and then using the empirical orthogonal function method (EOF) to analyze the height field characteristics of heavy rain in Anhui province. The results showed that the precipitation indices of high stations were higher than that of surrounding stations, most of the precipitation was from June to August, the average annual rainfall (rainfall days) of the Huang mountain station and Jiuhua mountain station were 2 290.3 mm (197.7 d) and 2 077.6 mm(187.7 d) respectively, the average annual heavy rainfall intensities (storm days) were 83.3 mm/d (8.5 d) and 79.6 mm/d (7.7 d) respectively, the main impact of the heavy rain at the high stations was 700 hPa westerly wind, the terrain had an impact on the precipitation and played a role of rainfall increase within a certain height. The EOF analysis was performed on the mean field of 500 hPa and 850 hPa altitude circulation. The first modes of 500 hPa in Huang mountain and Jiuhua mountain were mainly zonal and meridional, and the first mode of 850 hPa were all in meridional. The 500 hPa and 850 hPa circulation had a greater impact on the heavy rains of Huang mountain and Jiuhua mountain respectively. Therefore, by exploring the characteristics of precipitation and atmospheric circulation at the high station and surrounding stations, it was expected to provide scientific guidance for the precipitation forecast in the mountainous area.

Key words: rainstorm, precipitation index, empirical orthogonal function method(EOF), Huang mountain, Jiuhua mountain

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