基于新型观测资料的徒骇-马颊河流域“8·26”极端降水过程分析

高雷娜, 翟亮, 张琳, 王忠石, 韩亚静, 焦洋

Analysis of the“8·26”extreme precipitation event in the Tuhai-Majia River Basin based on new observational data

GAO Leina, ZHAI Liang, ZHANG Lin, WANG Zhongshi, HAN Yajing, JIAO Yang

图6 2024年8月26日模拟轨迹聚类（a，绿、蓝、红线为轨迹线）、26日16：00 925 hPa流线（蓝色）与水汽通量散度（填色，单位：kg·m-2·hPa-1·s-1）（b），庆云站风场（风矢，单位：m·s-1）、相对湿度（填色，单位：％）及比湿（黑色线，单位：g·kg-1）时间-高度剖面（c）

Fig.6 Simulated trajectory clustering on 26 August 2024 (a, green, blue, and red lines for trajectory lines), streamlines (blue lines) and water vapor flux divergence (the color shaded, Unit: kg·m-2·hPa-1·s-1) at 925 hPa at 16:00 on 26 August (b), and the time-height section of wind field (wind vectors, Unit: m·s-1), relative humidity (the color shaded, Unit: %) and specific humidity (black lines, Unit: g·kg-1) at Qingyun Station