Gash's analytical model of rainfall interception is reformulated, with
improved boundary conditions, to give a better description of the eva
poration from sparse forest. The model is tested against data from Les
Landes Forest collected during HAPEX-MOBILHY. The new formulation req
uires an estimate of the evaporation per unit area of canopy, rather t
han per unit ground area. When the evaporation per unit area of canopy
is equated with the estimates of evaporation derived from the Penman-
Monteith equation there is an improved description of the observations
.