@article{PAR00004212,
  title = {{C}ombined analysis of energy and water balances to estimate latent heat flux of a sudanian small catchment},
  author = {{G}uyot, {A}. and {C}ohard, {J}. {M}. and {A}nquetin, {S}. and {G}alle, {S}ylvie and {L}loyd, {C}. {R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A}ctual evapotranspiration is one of the major components of both energy and water budgets, but is often difficult to monitor over long period with sufficient accuracy. {W}ithin the framework of the "{AMMA}-{CATCH}" program, a project dedicated to the study of the {W}est {A}frican {M}onsoon, a large aperture scintillometer has been installed in a small catchment (12 km(2)), located in the {N}orth of {B}enin. a region exposed to sudanian climate. {T}he present study is an attempt to estimate the latent heat flux over this small but heterogeneous catchment based on scintillation and ground observations. {T}he analysis covers the end of the dry season (lasting from {F}ebruary to {A}pril 2006). {D}uring this period two isolated rainfall events occurred, giving a unique opportunity to study energy and water budgets simultaneously. {T}he comparison between the average sensible heat flux derived from scintillometer observations and the one obtained with conventional eddy correlation shows a relatively good agreement, where the scattering is mainly explained by differences in footprint associated with both instruments. {A} relevant hourly residual latent heat flux is then obtained through the energy balance equation, with careful attention brought to the net radiation, and the ground heat fluxes. {T}he residual of the energy budget equation is compared to soil water losses from vadose zone and water table, in order to evaluate whether this estimation is consistent with the water budget of the ground. {D}aily soil water depletion within the first meter of the surface shows a similar dynamic as the one calculated from the energy balance equation, but exhibits a constant 1 mm/day lag. {T}he excess of actual evapotranspiration is supposed to be explained by water table losses and root extraction by trees. {F}inally, this study shows how combined energy and water budget analysis can help to better understand water transfers at the watershed scale.},
  keywords = {{E}nergy balance closure ; {W}ater balance closure ; {A}ctual evapotranspiration ; {S}cintillometry ; {S}oil water storage ; {W}est {A}frica},
  booktitle = {},
  journal = {{J}ournal of {H}ydrology},
  volume = {375},
  numero = {1-2},
  pages = {227--240},
  ISSN = {0022-1694},
  year = {2009},
  DOI = {10.1016/j.jhydrol.2008.12.027},
  URL = {https://www.documentation.ird.fr/hor/{PAR}00004212},
}