伊犁河谷春季极端暴雨水汽特征与不稳定机制分析 |
魏娟娟, 万瑜, 潘宁, 肖俊安 |
Analysis of water vapor characteristics and unstable mechanism of extreme rainstorm in spring in Yili River Valley |
WEI Juanjuan, WAN Yu, PAN Ning, XIAO Junʼan |
图3 2022年5月5日08:00 1 000~300 hPa整层水汽通量(填色,单位:kg·m-1·s-1)和风场(风矢,单位:m·s-1)(a)及3—6日伊宁站水汽通量(填色,单位:g·cm-1·hPa-1·s-1)与水汽通量散度(等值线,单位:10-5 g·cm-2·hPa-1·s-1)(b) |
Fig.3 The water vapor flux from 1 000 to 300 hPa throughout the layer (the color shaded, Unit: kg·m-1·s-1), wind field (wind vectors, Unit: m·s-1) at 08:00 on May 5, 2022 (a), water vapor flux (the color shaded, Unit: g·cm-1·hPa-1·s-1), water vapor flux divergence (isolines, Unit: 10-5 g·cm-2·hPa-1·s-1) at Yining Station from May 3 to 6, 2022 (b) |
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