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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 18, issue 12
Hydrol. Earth Syst. Sci., 18, 5001–5024, 2014
https://doi.org/10.5194/hess-18-5001-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 18, 5001–5024, 2014
https://doi.org/10.5194/hess-18-5001-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Dec 2014

Research article | 10 Dec 2014

Building a field- and model-based climatology of local water and energy cycles in the cultivated Sahel – annual budgets and seasonality

C. Velluet1,2, J. Demarty2, B. Cappelaere2, I. Braud3, H. B.-A. Issoufou4, N. Boulain2, D. Ramier2,5, I. Mainassara6,7, G. Charvet2, M. Boucher2,8, J.-P. Chazarin2, M. Oï2, H. Yahou4,7, B. Maidaji4,6, F. Arpin-Pont9, N. Benarrosh2, A. Mahamane4, Y. Nazoumou7, G. Favreau2, and J. Seghieri2 C. Velluet et al.
  • 1Université Montpellier 2, UMR HSM (CNRS/IRD/UM1/UM2), Montpellier, France
  • 2IRD, UMR HSM (CNRS/IRD/UM1/UM2), Montpellier, France
  • 3IRSTEA, Unit HHLY, Lyon, France
  • 4Université de Maradi, Biology Department, Maradi, Niger
  • 5Cerema, DTer IDF, Trappes-en-Yvelines, France
  • 6IRD, UMR HSM (CNRS/IRD/UM1/UM2), Niamey, Niger
  • 7Université Abdou Moumouni, Geology Department, Niamey, Niger
  • 8IRD, LTHE, Grenoble, France
  • 9CNRS, UMR HSM (CNRS/IRD/UM1/UM2), Montpellier, France

Abstract. In the sub-Saharan Sahel, energy and water cycling at the land surface is pivotal for the regional climate, water resources and land productivity, yet it is still very poorly documented. As a step towards a comprehensive climatological description of surface fluxes in this area, this study provides estimates of long-term average annual budgets and seasonal cycles for two main land use types of the cultivated Sahelian belt: rainfed millet crop and fallow bush. These estimates build on the combination of a 7-year field data set from two typical plots in southwestern Niger with detailed physically based soil–plant–atmosphere modeling, yielding a continuous, comprehensive set of water and energy flux and storage variables over this multiyear period. In the present case in particular, blending field data with mechanistic modeling makes the best use of available data and knowledge for the construction of the multivariate time series. Rather than using the model only to gap-fill observations into a composite series, model–data integration is generalized homogeneously over time by generating the whole series with the entire data-constrained model simulation. Climatological averages of all water and energy variables, with associated sampling uncertainty, are derived at annual to sub-seasonal scales from the time series produced. Similarities and differences in the two ecosystem behaviors are highlighted. Mean annual evapotranspiration is found to represent ~82–85% of rainfall for both systems, but with different soil evaporation/plant transpiration partitioning and different seasonal distribution. The remainder consists entirely of runoff for the fallow, whereas drainage and runoff stand in a 40–60% proportion for the millet field. These results should provide a robust reference for the surface energy- and water-related studies needed in this region. Their significance and the benefits they gain from the innovative data–model integration approach are thoroughly discussed. The model developed in this context has the potential for reliable simulations outside the reported conditions, including changing climate and land cover.

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Long-term average water and energy cycles are described for two main land cover types in the cultivated Sahel (millet crop and fallow bush). Mean seasonal cycles and annual budgets for all component variables were estimated from detailed field and model analysis. Evapotranspiration totals over 80% of rainfall for both covers, but with different time distribution and soil/plant contributions. The remainder is shared between runoff and deep drainage for the crop, but is only runoff for the fallow.
Long-term average water and energy cycles are described for two main land cover types in the...
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