Pregled bibliografske jedinice broj: 296584
Analytical modelling of wintertime coastal jets in the Adriatic Sea
Analytical modelling of wintertime coastal jets in the Adriatic Sea // Continental Shelf Research, 27 (2007), 2; 275-285 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 296584 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Analytical modelling of wintertime coastal jets in the Adriatic Sea
Autori
Lazar, Martin ; Pavić, Marko ; Pasarić, Zoran ; Orlić, Mirko
Izvornik
Continental Shelf Research (0278-4343) 27
(2007), 2;
275-285
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Adriatic Sea; mathematical models; nearshore currents; thermohaline circulation; circulation asymmetry
Sažetak
Two diagnostic models, reproducing circulation generated in a marginal sea by variable density, have been developed. The models' domain is a 2D transverse section for which analytical solutions have been obtained. They describe the winter situation in the northern Adriatic, with a strong vertical mixing present and the density maximum dominating the centre of the basin. Both models employ Boussinesq-type parametrisation of friction and linear slip at the bottom. The first model allows for frictional departure from hydrostatic equilibrium and includes vertical friction only. The second one is hydrostatic but allows for lateral friction as well. The results obtained by the two models are similar and to some extent dependent on the vertical and bottom friction. They reproduce several well known characteristics of the Adriatic circulation (cyclonic surface flow, downwelling in the central and larger part of the basin compensated by upwelling in the coastal zone) but also predict some phenomena that are still not well understood. A conspicuous feature of the model results are coastal jets, which were observed in the Adriatic on several occasions. The present models show that the distance of jets from the coasts depends on lateral friction: it is found to vary from 1 up to 10 km on the Italian side and between 2 and 15 km on the Croatian side. Both models reproduce the west-east asymmetry, with the wider current on the east side of the basin. The asymmetry is a subject on which conflicting empirical results exist in the Adriatic. In the two models cyclonic flow occupies the whole water column, which disagrees with some recent theoretical findings of the near-bottom anticyclonic flow and thus leaves the issue open.
Izvorni jezik
Engleski
Znanstvena područja
Matematika, Geologija
POVEZANOST RADA
Projekti:
119-1193086-3085 - Utjecaj atmosfere i topografske varijabilnosti na procese u moru (Orlić, Mirko, MZOS ) ( CroRIS)
037-0372787-2795 - Titrajuća rješenja parcijalnih diferencijalnih jednadžbi (Antonić, Nenad, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Matematički odjel, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus