一次伴有极端降水的东北冷涡过程分析
任丽1,2(
), 卜文惠1, 于震宇1, 白俊杰3, 李瑶4
), 卜文惠1, 于震宇1, 白俊杰3, 李瑶4
Analysis of a northeast cold vortex process accompanied by extreme precipitation
REN Li1,2(), BU Wenhui1, YU Zhenyu1, BAI Junjie3, LI Yao4
), BU Wenhui1, YU Zhenyu1, BAI Junjie3, LI Yao4
图6. 2024年11月26日14:00 850 hPa（蓝色箭矢）、925 hPa（黑色箭矢）风场（a，单位：m·s-1，仅显示风速≥16 m·s-1）及降水中心区域26日02:00—27日02:00平均风速随高度的变化（b）
（棕色方框为降水中心区域，棕色垂线为低空急流阈值）
Fig.6. The wind field (a, Unit: m·s-1; only show the wind speed greater than or equal to 16 m·s-1) of 850 hPa (blue arrows) and 925 hPa (black arrows) at 14:00 on 26 and vertical variation of the mean wind speed over the precipitation center region from 02:00 on 26 to 02:00 on 27 (b) November 2024
(The brown box denotes the precipitation center region, the brown vertical line indicates the low-level jet threshold)
