This study investigates to what extent monthly mean surface meteorolog
ical variables can be used to estimate surface turbulent fluxes in the
equatorial Pacific. The two-year data from the TOGA TAO moored buoy a
rray are used to compute the monthly mean surface fluxes using both da
ily mean and monthly mean data as input to the bulk aerodynamic formul
as. A unique feature of the dataset is that it covers the western Paci
fic warm pool, a region of climatologically low surface winds and acti
ve convection. The results show that the ocean surface sensible and la
tent heat fluxes can be estimated using the monthly mean data to a ver
y high accuracy and that the momentum flux is generally underestimated
by about 10% when the monthly mean data instead of daily data is used
. This study, together with previous studies by other researchers, sug
gests that the monthly mean data such as those derived from satellite
measurements can be used to estimate the surface heat, moisture, and m
omentum fluxes over the global oceans.