Naslov
Small-scale variability in the coastal atmospheric boundary layer

Autori
Grisogono, Branko ; Strom, L. ; Tjernstrom, M.

Izvornik
Boundary-Layer Meteorology (0006-8314) 88 (1998), 1; 23-46

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
coastal jet; marine atmospheric boundary layer; mesoscale eddy; sea breeze; sea-breeze front; thermal mesoscale circulations; numerical-model; meteorological processes; turbulence structure; complex terrain; Baltic coast; cold-front; simulations; closure

Sažetak
The influence of the main large-scale wind directions on thermally driven mesoscale circulations at the Baltic southwest coast, southeast of Sweden, is examined. The aim of the study is to highlight small-scale alterations in the coastal atmospheric boundary layer. A numerical three-dimensional mesoscale model is used in this study, which is focused on an overall behaviour of the coastal jets, drainage flows, sea breezes, and a low-level eddy-type flow in particular. It is shown that synoptic conditions, together with the moderate terrain of the southeast of Sweden (max. height h(0) less than or equal to 206 m), governs the coastal mesoscale dynamics triggered by the land-sea temperature difference Delta T. The subtle nature of coastal low-level jets and sea breezes is revealed ; their patterns are dictated by the interplay between synoptic airflow, coastline orientation, and Delta T. The simulations show that coastal jets typically occur during nighttime and vary in height, intensity and position with respect to the coast ; they interact with downslope flows and the background wind. For the assigned land surface temperature (varying +/-8 K from the sea temperature) and the opposing constant geostrophic wind 8 m s(-1), the drainage flow is more robust to the opposing ambient flow than the sea breeze later on. Depending on the part of the coast under consideration, and the prevailing ambient wind, the sea breeze can be suppressed or enhanced, stationary at the coast or rapidly penetrating inland, locked up in phase with another dynamic system or almost independently self-evolving. A low-level eddy structure is analyzed. It is governed by 'tilting', 'divergence' and horizontal advection terms. The horizontal extent of the coastal effects agrees roughly with the Rossby radius of deformation.

Izvorni jezik
Engleski

POVEZANOST RADA