支树林, 包慧濛, 李婕. FY−4A卫星闪电资料在台风飑线天气监测中的应用能力分析[J]. 云南大学学报(自然科学版), 2019, 41(6): 1178-1190. doi: 10.7540/j.ynu.20180819
引用本文: 支树林, 包慧濛, 李婕. FY−4A卫星闪电资料在台风飑线天气监测中的应用能力分析[J]. 云南大学学报(自然科学版), 2019, 41(6): 1178-1190. doi: 10.7540/j.ynu.20180819
ZHI Shu-lin, BAO Hui-meng, LI Jie. Application ability analyses of FY−4A satellite flashes data in typhoon squall line weather surveillance[J]. Journal of Yunnan University: Natural Sciences Edition, 2019, 41(6): 1178-1190. DOI: 10.7540/j.ynu.20180819
Citation: ZHI Shu-lin, BAO Hui-meng, LI Jie. Application ability analyses of FY−4A satellite flashes data in typhoon squall line weather surveillance[J]. Journal of Yunnan University: Natural Sciences Edition, 2019, 41(6): 1178-1190. DOI: 10.7540/j.ynu.20180819

FY−4A卫星闪电资料在台风飑线天气监测中的应用能力分析

Application ability analyses of FY−4A satellite flashes data in typhoon squall line weather surveillance

  • 摘要: 为更好地开展风云四号气象卫星(FY−4A)闪电资料的业务化应用提供参考,结合地闪和多普勒雷达数据,对受2018年第22号台风“山竹”影响、于9月17日晚间在江西境内形成的台风飑线过程,对比分析了2种闪电资料的空间分布和时间演变差异,以及两者的频数与45 dBz以上强回波面积的时间演变特征,分析了卫星闪电与TBB低值区和地面大风位置的关系. 研究结果发现:地闪的位置多超前于卫星闪电,两者的时间变化趋势基本一致,但卫星闪电的变化幅度远较地闪显著;卫星闪电基本位于TBB≤−72 ℃处及邻近区域;在对流强烈影响阶段,尽管卫星闪电频数的波动较大,但仍与强回波面积有同步增大的特征;伴随的雷暴大风大都发生在卫星闪电密集区的前沿,且偏于移动方向一侧,与相同时段的地闪相似,表明它们对判识雷暴大风的可能发生位置有较好的辅助作用.

     

    Abstract: In order to better carry out the operational application of the Fengyun-4 meteorological satellite (FY−4A) lightning data, and based on the CGs and Doppler radar data, analyses are conducted on the impact features of squall-line processes affecting Jiangxi Province by the 22nd typhoon, "Typhoon Mangkhut" on the evening of Sept. 17th, 2018. Comparative analyses of two types of lightning data are mainly conducted as follows: the difference between their spatial distribution and time evolution, as well as their frequencies and the time evolution features of the radar echo area with reflectivity above 45 dBz. The relationship is analyzed between the satellite lightning and low-value TBB regions as well as the locations of the strong wind on the ground. The results show that: the CGs are mostly prior to the satellite lightning, and their time variation trends are basically the same, but the variation of satellite lightning is far more significant than that of the CGs. Satellite lightning is basically located in the area with TBB ≤−72 °C and adjacent areas. In the stage of severe convection influence, although the satellite lightning frequency fluctuates greatly, the frequency has the characteristics of varying with the enhancement of the severe radar echo area. The accompanying thunderstorm winds mostly occur in the frontier of the satellite lightning-intensive area, and are biased to the side of the moving direction, which is similar to the distribution features of CGs in the same period, indicating that they have a good auxiliary effect for identifying the possible locations of thunderstorm winds.

     

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