@article{fdi:010078676, title = {{T}rend and sensitivity analysis of reference evapotranspiration in the {S}enegal {R}iver basin using {NASA} meteorological data}, author = {{N}diaye, {P}.{M}. and {B}odian, {A}. and {D}iop, {L}. and {D}eme, {A}. and {D}ezetter, {A}lain and {D}jaman, {K}. and {O}gilvie, {A}ndrew}, editor = {}, language = {{ENG}}, abstract = {{U}nderstanding evapotranspiration and its long-term trends is essential for water cycle studies, modeling and for water uses. {S}patial and temporal analysis of evapotranspiration is therefore important for the management of water resources, particularly in the context of climate change. {T}he objective of this study is to analyze the trend of reference evapotranspiration ({ET}0) as well as its sensitivity to climatic variables in the {S}enegal {R}iver basin. {M}ann-{K}endall's test and {S}en's slope were used to detect trends and amplitude changes in {ET}(0)and climatic variables that most influence {ET}0. {R}esults show a significant increase in annual {ET}(0)for 32% of the watershed area over the 1984-2017 period. {A} significant decrease in annual {ET}(0)is observed for less than 1% of the basin area, mainly in the {S}ahelian zone. {O}n a seasonal scale, {ET}(0)increases significantly for 32% of the basin area during the dry season and decreases significantly for 4% of the basin during the rainy season. {A}nnual maximum, minimum temperatures and relative humidity increase significantly for 68%, 81% and 37% of the basin, respectively. {H}owever, a significant decrease in wind speed is noted in the {S}ahelian part of the basin. {T}he wind speed decrease and relative humidity increase lead to the decrease in {ET}(0)and highlight a "paradox of evaporation" in the {S}ahelian part of the {S}enegal {R}iver basin. {S}ensitivity analysis reveals that, in the {S}enegal {R}iver basin, {ET}(0)is more sensitive to relative humidity, maximum temperature and solar radiation.}, keywords = {{EVAPOTRANSPIRATION} ; {EVOLUTION} ; {METEOROLOGIE} ; {ANALYSE} {SPATIALE} ; {TEMPERATURE} ; {HUMIDITE} {RELATIVE} ; {VENT} ; {VARIATION} {ANNUELLE} ; {VARIATION} {SAISONNIERE} ; {FACTEUR} {CLIMATIQUE} ; {BASSIN} {VERSANT} ; {COURS} {D}'{EAU} ; {CHANGEMENT} {CLIMATIQUE} ; 1984 2017 ; {SENEGAL} ; {FLEUVE} {SENEGAL} {VALLEE} ; {MAURITANIE} ; {ZONE} {GUINEENNE} ; {ZONE} {SAHELIENNE} ; {ZONE} {SOUDANOGUINEENNE} ; {ZONE} {SOUDANOSAHELIENNE} ; {SENEGAL} {BASSIN} {VERSANT}}, booktitle = {}, journal = {{W}ater}, volume = {12}, numero = {7}, pages = {art. no 1957 [19 en ligne]}, ISSN = {2073-4441}, year = {2020}, DOI = {10.3390/w12071957}, URL = {https://www.documentation.ird.fr/hor/fdi:010078676}, }