Journal of Arid Meteorology ›› 2022, Vol. 40 ›› Issue (4): 549-566.DOI: 10.11755/j.issn.1006-7639(2022)-04-0549
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WANG Ying1(), ZHANG Qiang1,2(
), WANG Jinsong1, HAN Lanying1,3, WANG Suping1, ZHANG Liang1, YAO Yubi1,4, HAO Xiaocui1, WANG Sheng1
Received:
2022-04-03
Revised:
2022-06-01
Online:
2022-08-31
Published:
2022-09-21
Contact:
ZHANG Qiang
王莺1(), 张强1,2(
), 王劲松1, 韩兰英1,3, 王素萍1, 张良1, 姚玉璧1,4, 郝小翠1, 王胜1
通讯作者:
张强
作者简介:
王莺(1984—),女,研究员,博士,从事干旱灾害风险评估研究. E-mail: wangyn924@163.com。
基金资助:
CLC Number:
WANG Ying, ZHANG Qiang, WANG Jinsong, HAN Lanying, WANG Suping, ZHANG Liang, YAO Yubi, HAO Xiaocui, WANG Sheng. New progress and prospect of drought research since the 21st century[J]. Journal of Arid Meteorology, 2022, 40(4): 549-566.
王莺, 张强, 王劲松, 韩兰英, 王素萍, 张良, 姚玉璧, 郝小翠, 王胜. 21世纪以来干旱研究的若干新进展与展望[J]. 干旱气象, 2022, 40(4): 549-566.
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URL: http://www.ghqx.org.cn/EN/10.11755/j.issn.1006-7639(2022)-04-0549
Fig.1 The monitoring accuracy of each drought index for different regions and different seasons (cited from literature [31]) (a) spring, (b) summer, (c) autumn, (d) winter
Fig.2 Spatial distributions of the trend of SPI from 1960 to 2011 (cited from literature [35])(○ and ▲ represent passing the confidence level of 99.9% and 95%, respectively) (a) the whole year, (b) spring, (c) summer, (d) autumn, (e) winter
Fig.3 Variation of drought severity (a), frequency (b) and duration (c) before and after temperature abrupt change in China (cited from literature [37])
Fig.5 Drought disaster chain in southwestern China (a) and South China (b) (modified from literature [47]) (The color labels represent the corresponding disaster-affected body by drought disaster with different levels)
Fig.6 The trends for the three key climate factors (monthly total precipitation, mean temperature and MCI) and their relationships to crop growth and development periods (cited from literature [48])
Fig.7 Probability of drought disaster under precipitation deficit at different cumulative time scales (Unit: %) (a) 1 month, (b) 2 months, (c) 3 months, (d) 1-3 months, (e) 4-6 months
Fig.8 Conceptual model of drought disaster risk formation mechanism (cited from literature [46]) (solid lines for direct impact, and dotted lines for indirect impact)
Fig.11 Characteristics of drought disaster risk in South China and southwestern China before (a) and after (b) temperature abrupt change (cited from literature [46])
Fig.12 Changes of the average comprehensive loss rate of agriculture drought before and after the increases of annual average temperature in northern, southern China and the whole China (cited from literature [18])
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