USING LAND COVER CHANGES AND DEMOGRAPHIC DATA TO IMPROVE HYDROLOGICAL MODELLING IN THE SAHEL

To cite this version : Houet, Thomas and Galop, Didier and Mazier, Florence and Sheeren, David and Dejoux, Jean-François Modelling past and future land cover changes. A

The methodology involves using a high level assessment of the footprint that incorporates uncertainty in the inputs based on, for example, publicly available

Despite the varying environmental and climatic conditions of the West African Sahel, we show that it is possible to increase the performance of the GR2M model simulations by

On a daily basis, the average values of the actual evapotranspiration varied between 3 and 4 mm/day and are weak compared to the potential values (about 6 mm/day).

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Land cover mapping using aerial and VHR satellite images for distributed hydrological modelling of periurban catchments: Application to the Yzeron catchment (Lyon, France)2. Journal

Comparison of the evolution over time of the mean monthly snow depth simulated by SnowModel with the 2011–2012 meteorological data with the (1) current vegetation map, those

Interannual evolution of RC for the different types of hydrological behavior: (a) type 1: great basins: strong decrease during drought, long time in recovering RC; (b) type