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10 2022年7月25日10:00(a)、11:00(b)、12:00(c)、13:00(d)、14:00(e)、15:00(f)地面1 h负变温场(阴影,虚线间隔3 ℃,单位:℃)和1 h正变压场(蓝色和红色实线分别代表1、2 hPa气压扰动) (红三角为壶关站) |
Fig.10 The surface 1 h negative temperature change (the shaded, Dotted lines are 3 ℃ apart, Unit: ℃) and 1 h positive allobaric field (the blue and red line represent 1 hPa and 2 hPa pressure disturbance, respectively) at 10:00 (a), 11:00 (b), 12:00 (c), 13:00 (d), 14:00 (e), 15:00 (f) on 25 July 2022 (The red triangle indicates Huguan Station) |
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