Pregled bibliografske jedinice broj: 149545
Shallow water fronts, river plumes and strong forcing ; preliminary results from intensive surveys of the northern Adriatic
Shallow water fronts, river plumes and strong forcing ; preliminary results from intensive surveys of the northern Adriatic // Rapport du Commission Internationale pour l'Exploration Scientifique de la Mer Mediterranee, 2004. (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
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Naslov
Shallow water fronts, river plumes and strong forcing ; preliminary results from intensive surveys of the northern Adriatic
Autori
Lee, Craig ; Jones, Burton ; Arnone, Robert ; Gobat, Jason ; Marini, Mauro ; Orlić, Mirko ; Pasarić, Zoran ; Peters, Hartmut ; Poulain, Pierre ; Thaler, Dietmar ; Viličić, Damir
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Rapport du Commission Internationale pour l'Exploration Scientifique de la Mer Mediterranee
/ - , 2004
Mjesto i datum
,
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Adriatic Sea; fronts; mesoscale; optics; watermass formation
Sažetak
Quasi-synoptic, three-dimensional surveys of physical and optical variability characterize the mesoscale features that dominate the Northern and Central Adriatic, following their response to strong forcing events. During winter (February), sampling emphasized the response to episodic bora wind events. Although springtime (May) measurement program was designed to sample during the Po River spring freshette, freshwater discharge rates were more than a standard deviation below the 12-year mean and winds remained weakthroughout the survey period, leading to a study of weakly forced dynamics in a strongly stratified, shallow water regime. Wintertime sampling included survays of a strong shallow-water front and a prominent extension of the Po River plume. The surveys captured the evolution of a nearly vertical, compensated front that tilts as the strong bora winds weaken. A broad survey of the northern basin characterized the structure of a bora-driven po plume extension and reveals cyclonic (anticyclonic) circulation to the north (south) of the plume, consistent with the response found in previous numerical experiments.
Izvorni jezik
Engleski
Znanstvena područja
Biologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb