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dc.contributor.authorArnault, Joël
dc.contributor.authorMwanthi, Anthony Musili
dc.contributor.authorPortele, Tanja
dc.contributor.authorLi, Lu
dc.contributor.authorRummler, Thomas
dc.contributor.authorFersch, Benjamin
dc.contributor.authorHassan, Mohammed Abdullahi
dc.contributor.authorBahaga, Titike Kassa
dc.contributor.authorZhang, Zhenyu
dc.contributor.authorMortey, Eric Mensah
dc.contributor.authorAchugbu, Ifeany Chukwudi
dc.contributor.authorMoutahir, Hassane
dc.contributor.authorSy, Souleymane
dc.contributor.authorWei, Jianhui
dc.contributor.authorLaux, Patrick
dc.contributor.authorSobolowski, Stefan Pieter
dc.contributor.authorKunstmann, Harald
dc.date.accessioned2023-11-24T12:01:17Z
dc.date.available2023-11-24T12:01:17Z
dc.date.created2023-11-08T09:19:07Z
dc.date.issued2023
dc.identifier.citationFrontiers in Climate. 2023, 5 .en_US
dc.identifier.issn2624-9553
dc.identifier.urihttps://hdl.handle.net/11250/3104540
dc.description.abstractAfforestation as a climate change mitigation option has been the subject of intense debate and study over the last few decades, particularly in the tropics where agricultural activity is expanding. However, the impact of such landcover changes on the surface energy budget, temperature, and precipitation remains unclear as feedbacks between various components are difficult to resolve and interpret. Contributing to this scientific debate, regional climate models of varying complexity can be used to test how regional climate reacts to afforestation. In this study, the focus is on the gauged Nzoia basin (12,700 km2) located in a heavily farmed region of tropical Africa. A reanalysis product is dynamically downscaled with a coupled atmospheric-hydrological model (WRF-Hydro) to finely resolve the land-atmosphere system in the Nzoia region. To overcome the problem of Nzoia river flooding over its banks we enhance WRF-Hydro with an overbank flow routing option, which improves the representation of daily discharge based on the Nash-Sutcliffe efficiency and Kling-Gupta efficiency (from −2.69 to 0.30, and −0.36 to 0.63, respectively). Changing grassland and cropland areas to savannas, woody savannas, and evergreen broadleaf forest in three synthetic numerical experiments allows the assessment of potential regional climate impacts of three afforestation strategies. In all three cases, the afforestation-induced decrease in soil evaporation is larger than the afforestation-induced increase in plant transpiration, thus increasing sensible heat flux and triggering a localized negative feedback process leading to more precipitation and more runoff. This effect is more pronounced with the woody savannas experiment, with 7% less evapotranspiration, but 13% more precipitation, 8% more surface runoff, and 12% more underground runoff predicted in the Nzoia basin. This study demonstrates a potentially large impact of afforestation on regional water resources, which should be investigated in more detail for policy making purposes.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleRegional water cycle sensitivity to afforestation: synthetic numerical experiments for tropical Africaen_US
dc.title.alternativeRegional water cycle sensitivity to afforestation: synthetic numerical experiments for tropical Africaen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.rights.holder© 2023 Arnault, Mwanthi, Portele, Li, Rummler, Fersch, Hassan, Bahaga, Zhang, Mortey, Achugbu, Moutahir, Sy, Wei, Laux, Sobolowski and Kunstmannen_US
dc.description.versionpublishedVersionen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.3389/fclim.2023.1233536
dc.identifier.cristin2193649
dc.source.journalFrontiers in Climateen_US
dc.source.volume5en_US
dc.source.pagenumber0en_US
dc.relation.projectEC/H2020/869730en_US


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