亚欧大陆波列模态与热带对流对长江流域2024年夏末秋初复合高温干旱事件的协同影响 |
| 沈诗荐, 李金建, 马鹤翟, 李兴, 孟庆怡, 李霄宇 |
|
Synergistic impacts of Eurasian wave train mode and tropical convection on the compound hot and drought event in the Yangtze River Basin in late summer and early autumn in 2024 |
| SHEN Shijian, LI Jinjian, MA Hedi, LI Xing, MENG Qingyi, LI Xiaoyu |
| 图8 2024年8月21日—9月20日第一旬(a、b)、第二旬(c、d)及第三旬(e、f)200 hPa流函数距平场(填色,单位:106 m2·s-1)和T-N波作用通量(矢量,单位:m2·s-2)(a、c、e),及105°E—120°E经向平均垂直速度剖面(负值表示上升运动,单位:Pa·s-1)(b、d、f) |
| Fig.8 Anomalous 200 hPa stream function (the color shaded, Unit: 106 m2·s-1) and T-N wave activity flux (vectors, Unit: m2·s-2) (a, c, e) and the meridional mean vertical velocity cross section averaged over 105°E—120°E (negative values indicate upward motion, Unit: Pa·s-1) (b, d, f) for the first (a, b), second (c, d), and third (e, f) ten-day periods during August 21-September 20 in 2024 |
|