A three-dimensional numerical model was used to model water circulation and
spatial variation of temperature in Lake Sperillen in Norway. A winter sit
uation was simulated, with thermal stratification and ice cover. The numeri
cal model solved the Navier-Stokes equations on a 3D unstructured non-ortho
gonal grid with hexahedral cells. The SIMPLE method was used for the pressu
re coupling and the k-epsilon model was used to model turbulence, with a mo
dification for density stratification due to the vertical temperature profi
le. The results were compared with field measurements of the temperature in
the lake, indicating the location of the water current. Reasonably good ag
reement was found.