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) |
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