A three-dimensional, non-hydrostatic mesoscale model is used to study boundary-layer structure over an area characterized by the city of Copenhagen, the Bresund strait, and adjacent coastal farmland. Simulations are compared with data obtained on June 5, 1984 during the Oresund experiment.
Under moderately strong wind conditions, a stable internal boundary layer (IBL) developed over the 0resund strait during the day. Near-surface winds decelerate over water due to diminished vertical momentum transfer.
The turbulent kinetic energy field closely reflects the surface roughness distribution due to the imposed relatively strong wind forcing. TKE budgets over water, farmland and a city area are discussed by inspection of vertical profiles of the individual terms. The buoyancy term is used to indicate IBL heights because it changes sign at the boundary between different stability regimes. Measured and simulated dissipation rates show a decrease in the transition zone as the air travels over water and an abrupt increase when the IBL over a downwind city area is intersected. The top of the stable IBL is characterized by a minimum in the vertical TKE profile.