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dc.contributor.authorZhu, Yuanzhuo
dc.contributor.authorZhang, Zhihua
dc.contributor.authorCrabbe, M. James C.
dc.date.accessioned2021-02-18T09:20:14Z
dc.date.available2021-02-08T00:00:00Z
dc.date.available2021-02-18T09:20:14Z
dc.date.issued2021-02-08
dc.identifier.citationZhu Y, Zhang Z, Crabbe MJC (2021) 'Extreme climate response to marine cloud brightening in the arid Sahara-Sahel-Arabian Peninsula zone', International Journal of Climate Change Strategies and Management, (), pp.-.en_US
dc.identifier.issn1756-8692
dc.identifier.doi10.1108/IJCCSM-06-2020-0051
dc.identifier.urihttp://hdl.handle.net/10547/624827
dc.description.abstractPurpose Climatic extreme events are predicted to occur more frequently and intensely and will significantly threat the living of residents in arid and semi-arid regions. Therefore, this study aims to assess climatic extremes’ response to the emerging climate change mitigation strategy using a marine cloud brightening (MCB) scheme. Design/methodology/approach Based on Hadley Centre Global Environmental Model version 2-Earth System model simulations of a MCB scheme, this study used six climatic extreme indices [i.e. the hottest days (TXx), the coolest nights (TNn), the warm spell duration (WSDI), the cold spell duration (CSDI), the consecutive dry days (CDD) and wettest consecutive five days (RX5day)] to analyze spatiotemporal evolution of climate extreme events in the arid Sahara-Sahel-Arabian Peninsula Zone with and without MCB implementation. Findings Compared with a Representative Concentration Pathways 4.5 scenario, from 2030 to 2059, implementation of MCB is predicted to decrease the mean annual TXx and TNn indices by 0.4–1.7 and 0.3–2.1°C, respectively, for most of the Sahara-Sahel-Arabian Peninsula zone. It would also shorten the mean annual WSDI index by 118–183 days and the mean annual CSDI index by only 1–3 days, especially in the southern Sahara-Sahel-Arabian Peninsula zone. In terms of extreme precipitation, MCB could also decrease the mean annual CDD index by 5–25 days in the whole Sahara and Sahel belt and increase the mean annual RX5day index by approximately 10 mm in the east part of the Sahel belt during 2030–2059. Originality/value The results provide the first insights into the impacts of MCB on extreme climate in the arid Sahara-Sahel-Arabian Peninsula zone.en_US
dc.description.sponsorshipThis research was partially supported by the Second Tibetan Plateau Scientific Expedition and Research No 2019QZKK0906; European Commission Horizon2020 Flagship Project “ePIcenter”; Taishan Distinguished Professorship Fund.en_US
dc.language.isoenen_US
dc.publisherEmeralden_US
dc.relation.urlhttps://www.emerald.com/insight/content/doi/10.1108/IJCCSM-06-2020-0051/full/htmlen_US
dc.rights
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectclimate changeen_US
dc.subjectclimate projectionsen_US
dc.subjectclimatic extremesen_US
dc.subjectmarine cloud brightening schemeen_US
dc.subjectSahara-Sahel-Arabian Peninsula zoneen_US
dc.subjectspatiotemporal evolutionen_US
dc.subjectSubject Categories::F851 Applied Environmental Sciencesen_US
dc.titleExtreme climate response to marine cloud brightening in the arid Sahara-Sahel-Arabian Peninsula zoneen_US
dc.typeArticleen_US
dc.contributor.departmentShandong Universityen_US
dc.contributor.departmentBeijing Normal Universityen_US
dc.contributor.departmentOxford Universityen_US
dc.contributor.departmentUniversity of Bedfordshireen_US
dc.contributor.departmentShanxi Universityen_US
dc.identifier.journalInternational Journal of Climate Change Strategies and Managementen_US
dc.date.updated2021-02-18T09:16:03Z
dc.description.noteopen access


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