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Estimation de l’évapotranspiration par télédétection spatiale en Afrique de l’Ouest : vers une meilleure connaissance de cette variable clé pour la région

Abstract : West Africa is particularly vulnerable to climate and human-induced changes, exerting increasing pressure on water and plant resources. Sound management of the latter requires substantial scientific progress. In particular, it is essential to better understand energy and matter exchanges through the surface-atmosphere continuum, which are a major driver of the hydrological cycle and of vegetation development. In this respect, evapotranspiration is a key variable, as most of precipitation returns to the atmosphere by evapotranspiration and as it couples the water and energy cycles. In West Africa, current knowledge of this process is still limited because it is mainly based on field measurements that are representative of small spatial scales, or on land surface models that would require considerably more data than available in this region. In this context, this thesis work aims at improving our knowledge of the spatiotemporal variability of evapotranspiration, by analyzing the potential of remote sensing to estimate evapotranspiration in West Africa. The proposed approach is based on an inter-comparison of available remote sensing evapotranspiration products and on the proposal of a new method to generate new estimation products. The study was carried out over three mesoscale sites (~ 104 km2) providing a sample of the eco-climatic conditions encountered in West Africa, namely from North to South: the North-Sahel (in East-Central Mali), the South-Sahel (in South-West Niger) and the Sudanian zone (in North Benin). An improved remote sensing method for estimating daily evapotranspiration and its epistemic uncertainty named EVASPA S-SEBI Sahel (E3S) was developed. E3S was applied to the three study sites using data from the MODIS sensors onboard TERRA and AQUA satellites. Daily evapotranspiration estimates were evaluated against pluriannual observations acquired by the AMMA-CATCH Observatory. This study highlights the potential of E3S for estimating daily evapotranspiration in West Africa. However, these estimates are still subject to hazards of satellite measurements (image quality, cloud cover, large satellite view angle) and are therefore discontinuous. This thesis work also proposes new methods for reconstructing continuous daily evapotranspiration series by the combination of multi-resolution and multi-source estimations. The study shows the capabilities of these reconstruction approaches compared to the standard interpolation methods usually found in the literature. In particular, the proposed approaches allow better depicting the response of terrestrial surfaces to soil drying sequences between rainfall events. The newly generated evapotranspiration products were included in the product inter-comparison together with eight other products available in West Africa at various spatial and temporal resolutions. These products were evaluated at different spatial and temporal scales against local measurements and spatially distributed simulations by twenty land surface models from the ALMIP2 experiment. This study highlights the high inter-product variability especially in the Sahel. It also emphasizes the importance of taking into account information related to water stress in the generation of evapotranspiration products. The kilometric resolution of E3S products gives them a clear advantage in terms of description of the spatial variability of evapotranspiration flux compared to other coarse resolution products. The newly generated products show clear potential for future eco-hydrological and hydrogeological studies in the Sahel.
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Submitted on : Friday, February 22, 2019 - 1:35:14 PM
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Aubin Allies. Estimation de l’évapotranspiration par télédétection spatiale en Afrique de l’Ouest : vers une meilleure connaissance de cette variable clé pour la région. Hydrologie. Université Montpellier, 2018. Français. ⟨NNT : 2018MONTG068⟩. ⟨tel-02045897⟩



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