丽江机场强降水天气特征分析

Characteristic Analysis of Heavy Rainfall at Lijiang Airport

  • 摘要: 利用丽江机场自动观测站资料、NCEP再分析资料,引入HYSPLIT轨迹模式,对丽江机场2007—2019年出现的强降水天气特征进行分析。结果表明,丽江机场强降水日数年际差异较大,年平均强降水日数为7.8d,最大日降水量为92.3mm。强降水天气有明显的季节变化特征,雨季6—9月的强降水日数占比90%,暴雨主要分布在7—8月。根据500hPa高度上主要的影响系统,总结出7种丽江机场强降水天气形势,其中切变冷锋型和两高合并型是丽江机场强降水的最主要天气形势,占比40%。强降水期间丽江机场上空整层为垂直上升速度大值区。水汽主要来自700hPa高度,低层水汽辐合,高层辐散,有利于水汽向上垂直运动。通过HYSPLIT模式分析,丽江机场雨季水汽输送通道共有3条,其中西南路径占比最大,孟加拉湾地区的水汽输送是丽江机场雨季最主要的水汽来源;7—8月副热带高压强盛、台风活动频繁,因此有一定的南海方向水汽输送,即东南路径;8—9月受川滇切变线和西南涡影响,有少量来自川渝地区的水汽输送,即东北路径。

     

    Abstract: Based on the automatic observation station data of Lijiang Airport, NCEP reanalysis data, and the HYSPLIT trajectory model, the characteristics of heavy rainfall at Lijiang Airport from 2007 to 2019 were analyzed.The results show that the number of heavy rainfall days at Lijiang Airport varies greatly between years, with an annual average of 7.8 days and a maximum daily precipitation of 92.3 mm.The heavy rainfall weather patterns exhibit obvious seasonal variation characteristics.The number of heavy rainfall days from June to September, namely the rainy season, accounts for 90% of the total, and the rainstorms mainly occur in July and August.According to the main impact systems of 500 hPa, seven kinds of heavy rainfall weather situations are summarized at Lijiang Airport.Among the seven types, the shear cold front and two high convergence zone are the most dominating weather patterns of heavy rainfall, accounting for 40%.During the period of heavy rainfall, the whole layer over Lijiang Airport is featured with large vertical velocity.The water vapor mainly comes from the height of 700 hPa, with convergence in the lower layer and divergency in the upper layer.It is conducive to the upward vertical movement of the water vapor.According to the analysis of HYSPLIT model, there are three water vapor transport channels at Lijiang Airport during the rainy season, among which the southwest route accounts for the largest proportion, and the water vapor transport in the Bay of Bengal is the major water vapor source during the rainy season.From July to August, the strong subtropical high and the frequent typhoon activities result in the water vapor transport from the South China Sea, namely the southeast path.Influenced by the Sichuan-Yunnan shear line and southwest vortex, a small amount of water vapor is transported from Sichuan-Chongqing region in August to September, namely the northeast path..

     

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