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2 2022年5月5日14:00 500 hPa位势高度场(等值线,单位:dagpm)和风场(风矢,单位:m·s-1)(a)、850 hPa风场(风矢,单位:m·s-1)和地形抬升速度(等值线,单位:Pa·s-1)(b)及5日20:00沿44°N的散度(等值线,单位:10-5 s-1)、涡度平流(填色,单位:10-9 s-2)、风场(风矢,单位:m·s-1)(c)与垂直速度(填色,单位:Pa·s-1)和流场(流线)(d)的剖面
(灰色填充区为地形)
Fig.2 The 500 hPa geopotential height field (isolines, Unit: dagpm), wind field (wind vectors, Unit: m·s-1) (a) and 850 hPa wind field (wind vectors, Unit: m·s-1), terrain uplift velocity (isolines, Unit: Pa·s-1) (b) at 14:00 on May 5, 2022, the cross sections of divergence (isolines, Unit:10-5 s-1), vorticity advection (the color shaded, Unit: 10-9 s-2), wind field (wind vectors, Unit: m·s-1) (c) and vertical velocity (the color shaded, Unit: Pa·s-1), flow field (streamlines) (d) at 20:00 on May 5, 2022 along 44°N
(The gray filled area is terrain)