On the gradient observational data of the atmospheric surface layer from Se
ptember 1997 to December 1998 collected by two sets of Automatic Weather St
ation (AWS) installed in Gaize and Shiquanhe on the western Tibetan Plateau
, mean surface roughness lengths at the two stations above are determined t
o be 2.7 and 2.9 cm, respectively. The bulk transfer coefficients each day
are computed by the profile-flux method, means of the bulk transfer coeffic
ient for momentum (i.e. drag coefficient) in 1998 are 4.83x10(-3) and 4.75x
10 (3) at the two stations. The surface fluxes of momentum, sensible heat a
nd latent heat each day are further estimated by the bulk formulas, annual
mean of these fluxes is 3.4x10(-2) and 1.8x10 (2) N/m(2), 73.1 and 67.2 W/m
(2) 15.4 and 2.9 W/m(2), respectively. The diurnal and seasonal variations
are obtained by a composite method and the relationships among the heat tra
nsfers between land and atmosphere, plateau monsoon and plateau rain season
are also discussed.