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9 2022年7月25日12:48长治雷达组合反射率(单位:dBZ)(a)、径向速度沿图(a)黑线的剖面(单位:m·s-1)(b),13:39基本反射率因子(2.4°仰角)(c)及反射率因子沿图(c)黑线的剖面(d)(单位:dBZ)和0.5°(e)、1.5°(f)仰角径向速度(单位:m·s-1) |
Fig.9 The composite reflectivity (Unit: dBZ) (a) and the cross-section (b) of radial velocity along the black line in fig.a (Unit: m·s-1) at 12:48, reflectivity (Unit: dBZ) at 2.4° elevation (c) , the cross-section of reflectivity (Unit: dBZ) along the black line in fig.c (d), and radial velocity (Unit: m·s-1) at 0.5°(e) and 1.5° (f) elevation at 13:39 of Changzhi radar on 25 July 2022 |
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