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柯元惠, 马明明, 郑艳, 冯文. 2022: 海南岛雷暴大风天气形势和环境参数特征分析. 暴雨灾害, 41(1): 86-93. DOI: 10.3969/j.issn.1004-9045.2022.01.010
引用本文: 柯元惠, 马明明, 郑艳, 冯文. 2022: 海南岛雷暴大风天气形势和环境参数特征分析. 暴雨灾害, 41(1): 86-93. DOI: 10.3969/j.issn.1004-9045.2022.01.010
KE Yuanhui, MA Mingming, ZHENG Yan, FENG Wen. 2022: Analysis of synoptic situation and environmental parameters of thunderstorm gales in Hainan. Torrential Rain and Disasters, 41(1): 86-93. DOI: 10.3969/j.issn.1004-9045.2022.01.010
Citation: KE Yuanhui, MA Mingming, ZHENG Yan, FENG Wen. 2022: Analysis of synoptic situation and environmental parameters of thunderstorm gales in Hainan. Torrential Rain and Disasters, 41(1): 86-93. DOI: 10.3969/j.issn.1004-9045.2022.01.010

海南岛雷暴大风天气形势和环境参数特征分析

Analysis of synoptic situation and environmental parameters of thunderstorm gales in Hainan

  • 摘要: 利用海南岛区域加密自动站资料和海口站探空资料,结合ERA-Interim再分析资料对2014—2018年海南岛雷暴大风的强度、时空分布、环流形势和物理量参数特征进行分析研究。结果表明:(1) 海南岛雷暴大风主要出现在5—8月的午后到傍晚时段,最大阵风风速大部分在8级及以上。(2) 雷暴大风的环流形势可以分为三类,即西南热低压型、季风槽型和冷锋型,其中季风槽型根据槽线位置可以分为华南沿海槽型和南海低压槽型。(3) 西南热低压型雷暴大风的大气不稳定能量最大,上干下湿,垂直风切变较小;冷锋型的大气不稳定能量最小,上干下湿,垂直风切变最大;季风槽型的大气不稳定能量较大,整层较湿,垂直风切变最小。(4) 季风槽天气形势下发生雷暴大风时,较容易伴随短时强降水天气,西南热低压型的雷暴大风风力比其他类型更大。

     

    Abstract: In this study we analyzed the intensity, temporal and spatial distribution, circulation situation and environmental parameters of thunderstorm gale during 2014-2018 in Hainan using regional encrypted automatic station data and sounding data at Haikou, combining with ERA-Interim reanalysis data. The results are as follows. (1) The thunderstorm gales in Hainan mainly occurred in the afternoon to evening period from May to August. The maximum gust wind speed was mostly at level 8 or above. (2) The circulation situation of thunderstorm gales could be divided into three patterns: southwest trough, monsoon trough and cold air. The monsoon trough could be divided into South China coastal trough and South China sea trough according to the location of the trough. (3) The southwest trough pattern has the largest unstable energy and small vertical wind shear. Its dry upper-layer and wet lower-layer characteristic was obvious. In the cold air pattern, unstable energy was the minimum and dry upper-layer and wet lower-layer characteristics was obvious. The pattern has the largest vertical wind shear. In the monsoon trough pattern, unstable energy was relatively large and the whole layer was wet, and there was the smallest vertical wind shear. (4) Thunderstorm gales accompanied by short-term heavy rainfall sometimes in monsoon trough. The wind-force in southwest trough was higher than those in other types.

     

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