The boundary layer development over the Central sites of HAPEX-Sahel h
as been simulated for 4 individual days. The study is divided into two
parts. In the first part a surface scheme is calibrated for the domin
ant land cover of the area, the fallow savanna. This calibration is pe
rformed for a period of 54 days encompassing the transition from wet t
o dry. A comparison is then made with another more detailed surface sc
heme. The model, in spite of its drastic simplification of reality, is
able to reproduce the overall water balance for the period. In terms
of relative contribution of soil evaporation and vegetation transpirat
ion it does not depart significantly from the more complex scheme. In
the second part, the surface scheme is coupled to a one-dimensional ve
rsion of the ARPEGE model (operational forecast model at Meteo-France)
. The importance of the direct heating of the boundary layer by aeroso
ls is stressed. With minor modifications of calibration parameters fro
m the first phase, boundary layer profiles of temperature and also mix
ing ratio are reproduced with a good accuracy.