Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa

<p>The impact of climate change on precipitation and water availability is of major concern for policy makers in the Mono Basin of West Africa, whose economy mainly depends on rainfed agriculture and hydropower generation. The objective of this study is to project rainfall, flows and evapotran...

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Autores principales: L. Batablinlè, L. E. Agnidé, K. D. Japhet, A. Ernest, V. Expédit
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Lenguaje:EN
Publicado: Copernicus Publications 2021
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spelling oai:doaj.org-article:6c118ad4b16b473f8c523691eaaeb7cf2021-11-16T07:19:12ZFuture changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa10.5194/piahs-384-283-20212199-89812199-899Xhttps://doaj.org/article/6c118ad4b16b473f8c523691eaaeb7cf2021-11-01T00:00:00Zhttps://piahs.copernicus.org/articles/384/283/2021/piahs-384-283-2021.pdfhttps://doaj.org/toc/2199-8981https://doaj.org/toc/2199-899X<p>The impact of climate change on precipitation and water availability is of major concern for policy makers in the Mono Basin of West Africa, whose economy mainly depends on rainfed agriculture and hydropower generation. The objective of this study is to project rainfall, flows and evapotranspiration (ET) in the future period and understand their changes across Mono River Basin. Observed data were considered for the historical period 1980–2010, and a Multi-model ensemble for future projections data of eight selected Regional Climate Models under RCP 4.5 and RCP 8.5 over the periods 2011–2100 was used. The GR4J model was used to simulate daily flows of the Mono watershed. The ensemble mean shows a decrease and increase streamflows between <span class="inline-formula">−54</span> % and 42 %, <span class="inline-formula">−58</span> % and 31 %​​​​​​​ under the RCP4.5, RCP8.5 scenario, respectively. The greatest decreases of high flows is projected to occur in the near term under RCP8.5, whereas the greatest decrease of low flows is projected to occur in the long term under the same RCP. For the rainfall and ET, the both scenarios (RCP4.5 and RCP8.5) predict an increase of ET while the rainfall will decrease. The results of this study of would be very useful in the choice of management and adaptation policies for water resources management.</p>L. BatablinlèL. E. AgnidéK. D. JaphetA. ErnestV. ExpéditCopernicus PublicationsarticleEnvironmental sciencesGE1-350GeologyQE1-996.5ENProceedings of the International Association of Hydrological Sciences, Vol 384, Pp 283-288 (2021)
institution DOAJ
collection DOAJ
language EN
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
L. Batablinlè
L. E. Agnidé
K. D. Japhet
A. Ernest
V. Expédit
Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
description <p>The impact of climate change on precipitation and water availability is of major concern for policy makers in the Mono Basin of West Africa, whose economy mainly depends on rainfed agriculture and hydropower generation. The objective of this study is to project rainfall, flows and evapotranspiration (ET) in the future period and understand their changes across Mono River Basin. Observed data were considered for the historical period 1980–2010, and a Multi-model ensemble for future projections data of eight selected Regional Climate Models under RCP 4.5 and RCP 8.5 over the periods 2011–2100 was used. The GR4J model was used to simulate daily flows of the Mono watershed. The ensemble mean shows a decrease and increase streamflows between <span class="inline-formula">−54</span> % and 42 %, <span class="inline-formula">−58</span> % and 31 %​​​​​​​ under the RCP4.5, RCP8.5 scenario, respectively. The greatest decreases of high flows is projected to occur in the near term under RCP8.5, whereas the greatest decrease of low flows is projected to occur in the long term under the same RCP. For the rainfall and ET, the both scenarios (RCP4.5 and RCP8.5) predict an increase of ET while the rainfall will decrease. The results of this study of would be very useful in the choice of management and adaptation policies for water resources management.</p>
format article
author L. Batablinlè
L. E. Agnidé
K. D. Japhet
A. Ernest
V. Expédit
author_facet L. Batablinlè
L. E. Agnidé
K. D. Japhet
A. Ernest
V. Expédit
author_sort L. Batablinlè
title Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
title_short Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
title_full Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
title_fullStr Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
title_full_unstemmed Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
title_sort future changes in precipitation, evapotranspiration and streamflows in the mono basin of west africa
publisher Copernicus Publications
publishDate 2021
url https://doaj.org/article/6c118ad4b16b473f8c523691eaaeb7cf
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