Journal of Arid Meteorology ›› 2022, Vol. 40 ›› Issue (5): 733-747.DOI: 10.11755/j.issn.1006-7639(2022)-05-0733
• Research on Severe Drought in the Yangtze River Basin in 2022 • Previous Articles Next Articles
LI Yiping1(), ZHANG Jinyu1, YUE Ping1(), WANG Suping1, ZHA Pengfei2, WANG Lijuan1, SHA Sha1, ZHANG Liang1, ZENG Dingwen1, REN Yulong1, HU Die1
Received:
2022-09-02
Revised:
2022-09-08
Online:
2022-10-31
Published:
2022-11-10
Contact:
YUE Ping
李忆平1(), 张金玉1, 岳平1(), 王素萍1, 查鹏飞2, 王丽娟1, 沙莎1, 张良1, 曾鼎文1, 任余龙1, 胡蝶1
通讯作者:
岳平
作者简介:
李忆平(1981—),女,副研究员,主要从事极端气候事件的监测预测工作.E-mail:liyiping532@163.com。
基金资助:
CLC Number:
LI Yiping, ZHANG Jinyu, YUE Ping, WANG Suping, ZHA Pengfei, WANG Lijuan, SHA Sha, ZHANG Liang, ZENG Dingwen, REN Yulong, HU Die. Study on characteristics of severe drought event over Yangtze River Basin in summer of 2022 and its causes[J]. Journal of Arid Meteorology, 2022, 40(5): 733-747.
李忆平, 张金玉, 岳平, 王素萍, 查鹏飞, 王丽娟, 沙莎, 张良, 曾鼎文, 任余龙, 胡蝶. 2022年夏季长江流域重大干旱特征及其成因研究[J]. 干旱气象, 2022, 40(5): 733-747.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2022)-05-0733
Fig.3 The distribution of high temperature days (a, Unit: d), maximum air temperature (b, Unit: ℃), percentage of evapotranspiration anomalies (c, Unit: %) from June 1 to August 20, 2022 in China and evolution of percentage of evapotranspiration anomalies in the Yangtze River Basin during 1960-2022 (d)
Fig.5 Differences of ten-day’s soil volumetric water content of natural vegetation in area with the most severe drought over the Yangtze River Basin between the summer of 2022 and the same period of 2021 (a), the incremental soil moisture in summer of 2022 (the difference of volumetric soil water content between the right now ten-day and the former one) (b), the yearly variation of the incremental soil moisture in July-August (the difference between the average of the volumetric soil water content in July-August each year and the value in May of the current year) during 2014-2022 (c)
Fig.6 The 0-100 cm soil moisture anomaly from ERA5 reanalysis data in summer of 2022 (Unit: m3·m-3) (a) June, (b) July, (c) August, (d) mean value of summer 2022
Fig.7 The ten-day soil moisture percentile anomaly averaged in area with the most severe drought over the Yangtze River Basin in summer of 2022 simulated by CABLE model
Fig.8 Ten-day evolution of 100 hPa geopotential height field (black contours) and its anomaly (the color shaded) from early July to late August in 2022 (Unit: gpm) (The red line is the 16 800 gpm contour, and the green line is its climatological state) (a) the first ten-day of July, (b) the middle ten-day of July, (c) the last ten-day of July, (d) the first ten-day of August, (e) the middle ten-day of August, (f) the last ten-day of August
Fig.9 Daily evolution of area (a, c) and intensity (b, d) of the northern hemisphere polar vortex (a, b) and the Asian zone polar vortex (c, d) at 500 hPa in summer of 2022
Fig.10 Ten-day evolution of 500 hPa geopotential height field (black contours) and its anomaly (the color shaded) from early July to late August in 2022 (The red line is the 5880 gpm contour, and the green line is it’s climatological state) (a) the first ten-day of July, (b) the middle ten-day of July, (c) the last ten-day of July, (d) the first ten-day of August, (e) the middle ten-day of August, (f) the last ten-day of August
Fig.11 Ten-day variation of integrated water vapor flux (vectors, Unit: kg·m-1·s-1) and water vapor flux divergence anomaly (the color shaded, Unit: 10-5kg·m-2·s-1) in the whole troposphere (1000-300 hPa) from early July to late August in 2022 (a) the first ten-day of July, (b) the middle ten-day of July, (c) the last ten-day of July, (d) the first ten-day of August, (e) the middle ten-day of August, (f) the last ten-day of August
Fig.13 The distribution of snow cover anomalies on the Tibetan Plateau in May (a), June (b) and July (c) 2022 (Unit: %) (The dotted areas are more than 1 times standard deviation)
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