Projected Meteorological Drought over Asian Drylands under Different CMIP6 Scenarios

被引:37
作者
Li, Hongwei [1 ,2 ]
Li, Zhi [1 ]
Chen, Yaning [1 ]
Liu, Yongchang [1 ,2 ]
Hu, Yanan [1 ,2 ]
Sun, Fan [1 ,2 ]
Kayumba, Patient Mindje [1 ,2 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
CMIP6; SSPs; Asia; drylands; drought; CLIMATE-CHANGE; VEGETATION; PRECIPITATION; EVAPORATION;
D O I
10.3390/rs13214409
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Asia currently has the world's largest arid and semi-arid zones, so a timely assessment of future droughts in the Asian drylands is prudent, particularly in the context of recent frequent sandstorms. This paper assesses the duration, frequency, and intensity of drought events in the Asian drylands based on nine climate models of the Coupled Model Intercomparison Project Phase 6 (CMIP6). The results show that a high percentage of land area is experiencing significant drought intensification of 65.1%, 89.9%, and 99.8% under Shared Socioeconomic Pathways (SSP)126, SSP245, and SSP585 scenarios, respectively. Furthermore, the data indicate that future droughts will become less frequent but longer in duration and more intense, with even more severe future droughts predicted for northwest China and western parts of Uzbekistan and Kazakhstan. Drought durations of 10.8 months and 13.4 months are anticipated for the future periods of 2021-2060 and 2061-2100, respectively, compared to the duration of 6.6 months for the historical period (1960-2000). Meanwhile, drought intensity is expected to reach 0.97 and 1.37, respectively, for future events compared to 1.66 for the historical period. However, drought severity under SSP245 will be weaker than that under SSP126 due to the mitigating effect of precipitation. The results of this study can provide a basis for the development of adaptation measures in Asian dryland nations.
引用
收藏
页数:18
相关论文
共 57 条
[51]   Arid Central Asia saw mid-Holocene drought [J].
Xu, Hai ;
Zhou, Kang'en ;
Lan, Jianghu ;
Zhang, Guilin ;
Zhou, Xinying .
GEOLOGY, 2019, 47 (03) :255-258
[52]   Decreased vegetation growth in response to summer drought in Central Asia from 2000 to 2012 [J].
Xu, Hao-jie ;
Wang, Xin-ping ;
Zhang, Xiao-xiao .
INTERNATIONAL JOURNAL OF APPLIED EARTH OBSERVATION AND GEOINFORMATION, 2016, 52 :390-402
[53]  
Yevjevich V., 1967, J HYDROL, V7, P353, DOI [10.1016/0022-1694(69)90110-3, DOI 10.1016/0022-1694(69)90110-3]
[54]   Future drought characteristics through a multi-model ensemble from CMIP6 over South Asia [J].
Zhai, Jianqing ;
Mondal, Sanjit Kumar ;
Fischer, Thomas ;
Wang, Yanjun ;
Su, Buda ;
Huang, Jinlong ;
Tao, Hui ;
Wang, Guojie ;
Ullah, Waheed ;
Uddin, Md. Jalal .
ATMOSPHERIC RESEARCH, 2020, 246
[55]   Dependence of trends in and sensitivity of drought over China (1961-2013) on potential evaporation model [J].
Zhang, Jie ;
Sun, Fubao ;
Xu, Jijun ;
Chen, Yaning ;
Sang, Yan-Fang ;
Liu, Changming .
GEOPHYSICAL RESEARCH LETTERS, 2016, 43 (01) :206-213
[56]   Tree-ring-based precipitation reconstruction in southern Kazakhstan, reveals drought variability since AD 1770 [J].
Zhang, Ruibo ;
Shang, Huaming ;
Yu, Shulong ;
He, Qing ;
Yuan, Yujiang ;
Bolatov, Kainar ;
Mambetov, Bulkajyr T. .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2017, 37 (02) :741-750
[57]  
Zhu CM, 2015, J GEOPHYS RES-ATMOS, V120, P5504, DOI [10.1002/2015JD023618, 10.1002/2015JD023611]