Articles | Volume 383
Proc. IAHS, 383, 69–78, 2020
https://doi.org/10.5194/piahs-383-69-2020
Proc. IAHS, 383, 69–78, 2020
https://doi.org/10.5194/piahs-383-69-2020

Post-conference publication 16 Sep 2020

Post-conference publication | 16 Sep 2020

Extreme Rainfall and Temperature Changes Assessment on late-twenty-first-century over the Mono River Basin, Togo (West-Africa)

Batablinlè Lamboni et al.

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Future changes in precipitation, evapotranspiration and streamflows in the Mono Basin of West Africa
Lamboni Batablinlè, Lawin E. Agnidé, Kodja Domiho Japhet, Amoussou Ernest, and Vissin Expédit
Proc. IAHS, 384, 283–288, https://doi.org/10.5194/piahs-384-283-2021,https://doi.org/10.5194/piahs-384-283-2021, 2021
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Cited articles

Aguilar, E., Barry, A. A., Brunet, M., Ekang, L., Fernandes, A., Massoukina, M., and Zhang, X.: Changes in temperature and precipitation extremes in western central Africa, Guinea Conakry, and Zimbabwe, 1955–2006, J. Geophys. Res.-Atmos., 114, 1–11, https://doi.org/10.1029/2008JD011010, 2009. 
Batablinlè, L., Lawin, E., and Agnide, C. M.: Africa Cordex Simulations Projection of Future Temperature, Precipitation, Frequency and Intensity Indices Over Mono Basin in West Africa, J. Earth Sci. Clim. Change, 9, 490, https://doi.org/10.4172/2157-7617.1000490, 2018. 
Bazyomo, S. D., Ouedraogo, A., and Lawin, E. A.: Seasonal trends solar radiation available at the earth’s surface and implication of future annual power outputs changes on the photovoltaic systems with one and two tracking axes, J. Clim. Weather Forecast., 5, 1–9, 2017. 
Bigot, P.: Variability climatic, interaction and modification environnement, Variabilite climatique, Interaction et Modification, Environ. J. Hydrol., 4, 8141, 2003. 
Diallo, I. and Camara, M.: Comparaison du climat et de la variabilite interannuelle de la pluie simulée au Sahel par les modèles climatiques regionaux (Comparison of climate and interannual variability of rainfall simulated in the Sahel by regional climate models), 24, 96–106, 2013. 
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The first reason which led to study this area is that Mono basin shows a sharp increase in population and local economic growth generally projected to accelerate. Another reason is that the Mono basin is already facing the consequences of climate change, with recurrent and localized droughts and flash floods years. These conditions would expected to be exacerbated in the future. Such results could help to anticipate the future impacts of climate changes on agriculture, water resources.