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We hereby present a study on heat and mass transfer between free surface water and the atmosphere in Burkina Faso. We preferentially chose the city of Ouagadougou to conduct this study. One of the major problems in studying evaporation is how to determine water surface temperature and the flow of water evaporated. We calculated this surface temperature using the dichotomy method (Saighi, 2002) applied to the energy balance formula. The calculation of this temperature enabled us to draw thedoi:10.21474/ijar01/5604 fatcat:4si4v5nvwvccrmvqsvgcmjwbmy