Pregled bibliografske jedinice broj: 673651
Modelling of bottom anticyclonic circulation in the Adriatic Sea
Modelling of bottom anticyclonic circulation in the Adriatic Sea // Medcoast 05, The Seventh International Conference on the Mediterranean Coastal Environment
Kuşadası, Turska, 2005. (poster, nije recenziran, neobjavljeni rad, ostalo)
CROSBI ID: 673651 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Modelling of bottom anticyclonic circulation in the Adriatic Sea
Autori
Lazar, Martin ; Orlić, Mirko
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, neobjavljeni rad, ostalo
Skup
Medcoast 05, The Seventh International Conference on the Mediterranean Coastal Environment
Mjesto i datum
Kuşadası, Turska, 25.10.2005. - 29.10.2005
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
cyclonic; anticyclonic; circulation; Adriatic Sea
Sažetak
An analytical, diagnostic model, reproducing circulation generated in a marginal sea by variable density, is developed. It is inspired by the winter situation in the northern Adriatic, with a strong vertical mixing present and the density maximum dominating the centre of the basin. The model employs Boussinesq-type parameterisation of friction and linear slip at the bottom. The results obtained reproduce several well known characteristics of the Adriatic circulation (cyclonic surface flow, downwelling in the central part of the basin compensated by upwelling in the coastal zone) but also predict some phenomena that are still not well understood. For a small value of the lateral friction coefficient cyclonic circulation prevails throughout the water column. Increase of lateral friction results in the formation of a new cell in the bottom layer where the circulation is anticyclonic and thus opposed to that in the surface layer. The anticyclonic cell extends along the vertical as the lateral friction coefficient increases and reaches the half depth level for the maximum value of the coefficient. The model also reproduces the west-east asymmetry, with the wider and weaker current being present on the east side of the basin. It is shown that this feature originates in the corresponding asymmetry of density anomaly. Coastal jets are obtained as well.
Izvorni jezik
Engleski
Znanstvena područja
Matematika, Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Matematički odjel, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb