@article{fdi:010061938,
  title = {{G}eneralized combination equations for canopy evaporation under dry and wet conditions},
  author = {{L}homme, {J}ean-{P}aul and {M}ontes, {C}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he formulation of canopy evaporation is investigated on the basis of the combination equation derived from the {P}enman equation. {A}ll the elementary resistances (surface and boundary layer) within the canopy are taken into account, and the exchange surfaces are assumed to be subject to the same vapour pressure deficit at canopy source height. {T}his development leads to generalized combination equations: one for completely dry canopies and the other for partially wet canopies. {T}hese equations are rather complex because they involve the partitioning of available energy within the canopy and between the wet and dry surfaces. {B}y making some assumptions and approximations, they can provide simpler equations similar to the common {P}enman-{M}onteith model. {O}ne of the basic assumptions of this down-grading process is to consider that the available energy intercepted by the different elements making up the canopy is uniformly distributed and proportional to their respective area. {D}espite the somewhat unrealistic character of this hypothesis, it allows one to retrieve the simple formulations commonly and successfully used up to now. {N}umerical simulations are carried out by means of a simple one-dimensional model of the vegetation-atmosphere interaction with two different leaf area profiles. {I}n dry conditions and when the soil surface is moist (low surface resistance), there is a large discrepancy between the generalized formulation and its simpler {P}enman-{M}onteith form, but much less when the soil surface is dry. {I}n partially wet conditions, the {P}enman-{M}onteith-type equation substantially underestimates the generalized formulation when leaves are evenly distributed, but provides better estimates when leaves are concentrated in the upper half of the canopy.},
  keywords = {},
  booktitle = {},
  journal = {{H}ydrology and {E}arth {S}ystem {S}ciences},
  volume = {18},
  numero = {3},
  pages = {1137--1149},
  ISSN = {1027-5606},
  year = {2014},
  DOI = {10.5194/hess-18-1137-2014},
  URL = {https://www.documentation.ird.fr/hor/fdi:010061938},
}