Articles | Volume 385
https://doi.org/10.5194/piahs-385-415-2024
https://doi.org/10.5194/piahs-385-415-2024
Post-conference publication
 | 
19 Apr 2024
Post-conference publication |  | 19 Apr 2024

Evaluation and calibration of alternative methods for estimating reference evapotranspiration in the main hydrosystems of Senegal: Senegal, Gambia and Casamance River Basins

Ansoumana Bodian, Papa Malick Ndiaye, Serigne Bassirou Diop, Lamine Diop, Alain Dezetter, Andrew Ogilvie, and Koffi Djaman

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Cited articles

Abtew, W.: Evapotranspiration measurement and modeling for three wetland systems in South Florida, Water Resour. B., 32, 465–473, 1996. 
Bodian, A., Diop, L., Panthou, G., Dacosta, H., Deme, A., Dezetter, A., Ndiaye, P. M., Diouf, I., and Vichel, Th.: Recent Trend in Hydroclimatic Conditions in the Senegal River Basin, Water, 12, 436, https://doi.org/10.3390/w12020436, 2020. 
Bogawski, P. and Bednorz, E.: Comparison and validation of selected evapotranspiration models for conditions in Poland (Central Europe), Water Resour. Manag., 28, 5021–5038, https://doi.org/10.1007/s11269-014-0787-8, 2014. 
Dacosta, H.: Précipitations et écoulements sur le bassin de la Casamance. Dakar: ORSTOM, 278 p. multigr. Th. 3e cycle: Géogr. Phys., Hydrologie, Université Cheikh Anta Diop: Dakar, 1989. 
Dalton, J.: Experimental essays on the constitution of mixed gases; on the force of steam of vapor from waters and other liquids in different temperatures, both in a Torricellian vacuum and in air on evaporation and on the expansion of gases by heat, Memoirs of the Manchester Literary and Philosophical Society, 5, 535–602, 1802. 
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Short summary
Reference evapotranspiration (ET0) is an essential parameter for hydrological modeling, irrigation planning and for studying the impacts of climate change on water resources. This work evaluate 20 alternative methods of estimating ET0 in order to adapt them to the climatic context of the 3 mains basins of Senegal where very little climate data is available. The methods of Valiantzas 1, Doorenboss & Pruitt and Penman are the most robust for the estimation of ET0 in this context.