In this study, turbulent heat flux data from two sites within the Baltic Se
a are compared with estimates from two models. The main focus is on the lat
ent heat flux. The measuring sites are located on small islands close to th
e islands of Bornholm and Gotland. Both sites have a wide wind direction se
ctor with undisturbed over-water fetch. Mean parameters and direct fluxes w
ere measured on masts during May to December 1998.
The two models used in this study are the regional-scale atmospheric model
HIRLAM and the ocean model PROBE-Baltic. It is shown that both models overe
stimate the sensible and latent heat fluxes. The overestimation can, to a l
arge extent, be explained by errors in the air-water temperature and humidi
ty differences. From comparing observed and modelled data, the estimated 8-
month mean errors in temperature and humidity are up to 1 degreesC and 1 g
kg(-1),respectively. The mean errors in the sensible and latent heat fluxes
for the same period are approximately 15 and 30 W m(-2), respectively.
Bulk transfer coefficients used for calculating heat and humidity fluxes at
the surface were shown to agree rather well with the measurements, at leas
t for the unstable data. For stable stratification, the scatter in data is
generally large, and it appears that the bulk formulation chosen overestima
tes turbulent heat fluxes.