%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Lhomme, Jean-Paul
%A Boudhina, N.
%A Masmoudi, M. M.
%A Chehbouni, Abdelghani
%T Estimation of crop water requirements : extending the one-step approach to dual crop coefficients
%D 2015
%L fdi:010064897
%G ENG
%J Hydrology and Earth System Sciences
%@ 1027-5606
%M ISI:000358918200018
%N 7
%P 3287-3299
%R 10.5194/hess-19-3287-2015
%U https://www.documentation.ird.fr/hor/fdi:010064897
%> https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-10/010064897.pdf
%V 19
%W Horizon (IRD)
%X Crop water requirements are commonly estimated with the FAO-56 methodology based upon a two-step approach: first a reference evapotranspiration (ET0) is calculated from weather variables with the Penman-Monteith equation, then ET0 is multiplied by a tabulated crop-specific coefficient (K-c) to determine the water requirement (ETc) of a given crop under standard conditions. This method has been challenged to the benefit of a one-step approach, where crop evapotranspiration is directly calculated from a Penman-Monteith equation, its surface resistance replacing the crop coefficient. Whereas the transformation of the two-step approach into a one-step approach has been well documented when a single crop coefficient (K-c) is used, the case of dual crop coefficients (K-cb for the crop and K-e for the soil) has not been treated yet. The present paper examines this specific case. Using a full two-layer model as a reference, it is shown that the FAO-56 dual crop coefficient approach can be translated into a one-step approach based upon a modified combination equation. This equation has the basic form of the Penman-Monteith equation but its surface resistance is calculated as the parallel sum of a foliage resistance (replacing K-cb) and a soil surface resistance (replacing K-e). We also show that the foliage resistance, which depends on leaf stomatal resistance and leaf area, can be inferred from the basal crop coefficient (K-cb) in a way similar to the Matt-Shuttleworth method.
%$ 072