Pregled bibliografske jedinice broj: 206677
Analytic Modelling of Thermohaline Circulation and Quasi-geostrophic Flow in the Adriatic Sea
Analytic Modelling of Thermohaline Circulation and Quasi-geostrophic Flow in the Adriatic Sea // Zbornik sažetaka postera znanstvenih novaka, prikazanih u inozemstvu 2002., 2003 i 2004. godine / Prvi kongres hrvatskih znanstvenika iz domovine i inozemstva, Zagreb-Vukovar, 15-19. studenog 2004.
Zagreb: Akademija tehničkih znanosti Hrvatske (HATZ), 2004. (poster, nije recenziran, sažetak, znanstveni)
CROSBI ID: 206677 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Analytic Modelling of Thermohaline Circulation and Quasi-geostrophic Flow in the Adriatic Sea
Autori
Lazar, Martin ; Pavić, Marko ; Pasarić, Zoran ; Orlić, Mirko
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Zbornik sažetaka postera znanstvenih novaka, prikazanih u inozemstvu 2002., 2003 i 2004. godine / Prvi kongres hrvatskih znanstvenika iz domovine i inozemstva, Zagreb-Vukovar, 15-19. studenog 2004.
/ - Zagreb : Akademija tehničkih znanosti Hrvatske (HATZ), 2004
Skup
Prvi kongres hrvatskih znanstvenika iz domovine i inozemstva
Mjesto i datum
Vukovar, Hrvatska; Zagreb, Hrvatska, 15.11.2004. - 19.11.2004
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
thermohaline circulation; quasi-geostrophic flow; analytic modelling; friction parametrization
Sažetak
The winter situation in a shallow land-locked basin modelling the Adriatic Sea is considered. During the winter the maximum of density is usually observed in the central part of the Adriatic, supporting thermohaline circulation characterized by upwelling along the coasts and downwelling prevailing over a greater part of the sea. Due to deflecting influence of the Coriolis force, long-shore currents appear as well. The present work encompasses two models having different types of friction parametrization. The first one allows for the vertical component of turbulent friction only, the other includes lateral friction as well. Both models give similar results and predict cyclonic circulation in the horizontal plane and downwelling in a greater part of the basin compensated by upwelling along the coasts, in fair agreement with the obesrvations. The modelling results are discussed for varying coefficients of bottom friction, vertical friction and lateral friction.
Izvorni jezik
Engleski
Znanstvena područja
Matematika, Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Matematički odjel, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb