复杂地形下一次飑线的组织化过程及成因分析
胡嘉缨, 赵桂香, 闫慧, 徐逸雯, 操俊伟

Organization and causation of a squall line under the complex terrain
HU Jiaying, ZHAO Guixiang, YAN Hui, XU Yiwen, CAO Junwei
图3 2022年7月25日08:00 500 hPa(a)、700 hPa(b)、850 hPa(c)位势高度(黑色实线,单位:dagpm)、温度(红色虚线,单位:℃)和风场(风矢,单位:m·s-1)及海平面气压场(黑色实线,单位:hPa)(d)
Fig.3 The 500 hPa (a), 700 hPa (b) and 850 hPa (c) geopotential height (black soild lines, Unit: dagpm), temperature (red dashed lines, Unit: ℃) and wind (wind vectors, Unit: m·s-1) fields, and sea level pressure field (black soild lines, Unit: hPa) (d) at 08:00 on 25 July 2022