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

dc.contributor.authorAyugi, Brian
dc.contributor.authorShilenje, Zablon Weku
dc.contributor.authorBabaousmail, Hassen
dc.contributor.authorSian, Kenny Lim Kam
dc.contributor.authorMumo, Richard
dc.contributor.authorDike, Victor Nnamdi
dc.contributor.authorIyakaremye, Vedaste
dc.contributor.authorChehbouni, Abdelghani
dc.contributor.authorOngoma, Victor
dc.date.accessioned2024-06-14T06:31:40Z
dc.date.available2024-06-14T06:31:40Z
dc.date.issued2022-04-09
dc.description.abstractThe 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.en_US
dc.description.accessibilityunrestricteden_US
dc.description.departmentmssen_US
dc.description.levelphden_US
dc.description.sponsorshipAcknowledge the infrastructural support provided by Nanjing University of Information Science and Technology.en_US
dc.identifier.citationAyugi,A. at.el. (2022) Projected changes in meteorological drought over East Africa inferred from bias-adjusted CMIP6 models. Natural Hazards, https://doi.org/10.1007/s11069-022-05341-8en_US
dc.identifier.issn15730840
dc.identifier.urihttps://repository.biust.ac.bw/handle/123456789/577
dc.language.isoenen_US
dc.publisherSpringer Natureen_US
dc.subjectPrecipitationen_US
dc.subjectDroughten_US
dc.subjectClimate changeen_US
dc.subjectQuantile mappingen_US
dc.subjectSSPen_US
dc.subjectEast Africaen_US
dc.titleProjected changes in meteorological drought over East Africa inferred from bias‑adjusted CMIP6 modelsen_US

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