The authors present a numerical and experimental study on heat and mass tra
nsfers by forced convection in a channel with a sinusoidal protuberance and
by natural convection in a reservoir full of water. The numerical study ha
s been carried out for Reynolds numbers in a range of 35 to 350, several de
nsities of heat flux and protuberance amplitude range of 0.005 to 0.02 m. R
esults show that the vapour diffusion in the air modifies the stream functi
on profiles which become convex over the free surface of the water. In addi
tion, the evaporation reduces the perturbation caused by the protuberance a
nd increases the heat transfer rate in the channel. The visualisation of th
e flow, using smoke, an argon laser and a videocamera, shows the complexity
of the interaction between the flow of vapour caused by the evaporation, t
he flow in the channel and the heat losses across the lateral walls. Theore
tical and experimental results are in good qualitative agreement.