Projected changes in meteorological drought over East Africa inferred from bias-adjusted CMIP6 models

被引:0
作者
Brian Ayugi
Zablon Weku Shilenje
Hassen Babaousmail
Kenny T. C. Lim Kam Sian
Richard Mumo
Victor Nnamdi Dike
Vedaste Iyakaremye
Abdelghani Chehbouni
Victor Ongoma
机构
[1] Nanjing University of Information Science and Technology,Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Collaborative Innovation Center of Atmospheric Environment and Equipment Technology, School of Environmental Scienc
[2] University of Information Science and Technology,Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center On Forecast and Eval
[3] Charles University,FEMD)
[4] Kenya Meteorological Department,Department of Atmospheric Physics, Faculty of Mathematics and Physics
[5] Binjiang College of Nanjing University of Information Science and Technology,Department of Mathematics and Statistical Sciences
[6] Botswana International University of Science and Technology,International Center for Climate and Environment Sciences, Institute of Atmospheric Physics
[7] Chinese Academy of Sciences,Energy, Climate, and Environment Science Group
[8] Imo State Polytechnic Umuagwo,International Water Research Institute
[9] Rwanda Meteorology Agency,undefined
[10] Mohammed VI Polytechnic University,undefined
来源
Natural Hazards | 2022年 / 113卷
关键词
Precipitation; Drought; Climate change; Quantile mapping; SSP; East Africa;
D O I
暂无
中图分类号
学科分类号
摘要
The ongoing global warming has caused unprecedented changes in the climate system, leading to an increase in the intensity and frequency of weather and climate extremes. This study uses the sixth phase of Coupled Model Intercomparison Project (CMIP6) data to investigate projected changes in drought events over East Africa (EA) under four Shared Socioeconomic Pathway (SSP) emission scenarios (SSP1-2.6, SSP2-4.5, SSP3-4.0, and SSP5-8.5). The CMIP6 data are bias-corrected using a quantile mapping method, with the Climatic Research Unit's precipitation dataset as reference. Drought is quantified using the standardized precipitation index and different measures of drought are estimated: drought duration, drought frequency, drought severity, and drought intensity. Evaluating the accuracy and reliability of historical data before and after bias correction demonstrates the importance of the approach. The overall distribution after bias correction depicts a close agreement with observation. Moreover, the multi-model ensemble mean demonstrate superiority over individual Global Circulation Models. Projected future changes show enhancement in precipitation over most parts of EA in the far future under different SSP scenarios. However, the arid and semi-arid regions are expected to receive less amount of precipitation, whereas the highlands and lake regions are expected to receive a larger amount of precipitation increase. Furthermore, the dry areas of EA are likely to experience more frequent drought events with longer duration, stronger intensity, and severity in the far future. Overall, this study identifies possible drought hotspots over EA, enabling early preparation for such events.
引用
收藏
页码:1151 / 1176
页数:25
相关论文
共 383 条
  • [1] Abdelmoaty HM(2021)Biases beyond the mean in CMIP6 extreme precipitation: a global investigation Earth’s Future 9 e2021EF002196-2491
  • [2] Papalexiou SM(2017)Centennial drought outlook over the CONUS using NASA-NEX downscaled climate ensemble Int J Climatol 37 2477-686
  • [3] Rajulapati CR(2019)Future drought risk in Africa: integrating vulnerability, climate change, and population growth Sci Total Environ 662 672-475
  • [4] AghaKouchak A(2021)Evaluation of CMIP6 models in simulating the statistics of extreme precipitation over Eastern Africa Atmos Res 254 455-1413
  • [5] Ahmadalipour A(2020)Projected change in temperature and precipitation over Africa from CMIP6 Earth Syst Environ 4 1401-83
  • [6] Moradkhani H(2019)Recent trends of surface air temperatures over Kenya from 1971 to 2010 Meteorol Atmos Phys 131 69-434
  • [7] Svoboda M(2016)Analysis of spatial and temporal patterns of rainfall variations over Kenya Environ Earth Sci 6 421-6496
  • [8] Ahmadalipour A(2018)Circulations associated with variations in boreal spring rainfall over Kenya Earth Syst Environ 2 6474-299
  • [9] Moradkhani H(2021)Comparison of CMIP6 and CMIP5 models in simulating mean and extreme precipitation over East Africa Int J Climatol 41 2358-58
  • [10] Castelletti A(2021)Future changes in precipitation extremes over East Africa based on CMIP6 models Water 13 801-312