基于北斗三号和风云四号A星的大通“817”极端降雨特征分析

Analysis of extreme rainfall characteristics of Datong “817” based on BDS-3 and FY-4A

  • 摘要: 充足的水汽和云相态变化是降雨发生的两个必要条件. 北斗三号卫星导航系统(BeiDou-3 Navigation Satellite System,BDS-3)可以反演水汽,具有时间分辨率高、精度高的优点;风云四号A星(FY-4A)可提供分辨率为15 min的云相态参数. 本文使用BDS-3和FY-4A数据分析了2022-08-17大通降水发生前后的大气可降水和云相态的时空变化规律,通过对比得到了大通“817”极端降雨三个特征:一是降雨前1 h大气可降水量(perceptible water vapor,PWV)快速上升,速率达到3.17 mm/h,显著超过同期一般降雨水平;二是降雨前云类型存在多层云与不透明冰云的多次变换,最后以不透明冰云形式发生极端降雨;三是极端降雨云顶高度通常大于10 000 m.

     

    Abstract: Adequate water vapor and cloud phase changes are two necessary conditions for rainfall to occur. Based on the BeiDou-3 satellite navigation system, water vapor can be retrieved, which has the advantages of high time resolution and accuracy; FY-4A can provide cloud phase parameters with a resolution of 15 minutes. This article uses the BDS-3 and FY-4A data to analyze the spatiotemporal changes in atmospheric precipitation and cloud phase before and after the occurrence of all precipitation in August 2022. Through comparison, three characteristics of extreme rainfall in Datong “817” were obtained: firstly, the perceptible water vapor increased one hour before rainfall, reaching a rate of 3.17 mm/h, significantly exceeding the general rainfall level of the same period; before the second rainfall, there were multiple changes in cloud types between multi-layer clouds and opaque ice clouds, and eventually extreme rainfall occurred in the form of opaque ice clouds; the third reason is that the height of extreme rainfall cloud tops is usually greater than 10000 meters.

     

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