Napredna pretraga

Pregled bibliografske jedinice broj: 307822

West Adriatic coastal water summertime excursion into the East Adriatic


Vilibić, Ivica; Orlić, Mirko; Beg Paklar, Gordana; Book, J.; Dadić, Vlado; Grbec, Branka; Martin, P.; Matić, Frano; Mihanović, Hrvoje; Morović, Mira et al.
West Adriatic coastal water summertime excursion into the East Adriatic // Rapid environmental assesment (REA07) Confetrence "Coastal Processes : Challenges for Monitoring and Prediction" : Abstracts
Lerici, Italija: NURC, 2007. str. 97-97 (predavanje, međunarodna recenzija, sažetak, znanstveni)


Naslov
West Adriatic coastal water summertime excursion into the East Adriatic

Autori
Vilibić, Ivica ; Orlić, Mirko ; Beg Paklar, Gordana ; Book, J. ; Dadić, Vlado ; Grbec, Branka ; Martin, P. ; Matić, Frano ; Mihanović, Hrvoje ; Morović, Mira ; Pasarić, Miroslava ; Tudor, Martina

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Rapid environmental assesment (REA07) Confetrence "Coastal Processes : Challenges for Monitoring and Prediction" : Abstracts / - : NURC, 2007, 97-97

Skup
Rapid Environmental Assessment Conference "Costal Processes : Challenges for Monitoring and Prediction"

Mjesto i datum
Lerici, Italija, 25.-27.09.2007

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Adriatic Sea; summertime excursion; coastal water

Sažetak
A pool of less saline surface waters has been observed in late June 2006 at the northern edge of the South Adriatic Pit. Three possible sources have been assumed: (1) Albanian rivers, (2) middle Adriatic rivers, or (3) West Adriatic Current (WAC). Through the examination of ADCP data collected within DART and ITHACA projects, and of satellite images, source (3) appears to be the likely culprit. Such an extended excursion is especially surprising as rather low winds and stable conditions prevailed in mid/late June. However, quite strong Etesian winds occurred in first 12 days in June, with a maximum close to the western shore. Therefore, it is suspected that these winds enhanced the WAC and inclined sea level along the western shore, resulting in a transversal eddy-like circulation when the winds later relaxed. These WAC eddies grew and reached middle east-Adriatic waters for about two weeks and were successfully simulated by the Navy Coastal Ocean Model. Finally, we quantify the role of various bathymetrical features on the WAC transversal dynamics through idealized modelling studies.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekt / tema
001-0013077-1118 - Kooscilacije atmosfere i mora važne za ekosustav Jadrana (Mira Morović, )
001-0013077-1122 - Istraživanje i sustavi praćenja neuobičajene dinamike Jadrana (Ivica Vilibić, )
119-1193086-3085 - Utjecaj atmosfere i topografske varijabilnosti na procese u moru (Mirko Orlić, )

Ustanove
Institut za oceanografiju i ribarstvo, Split,
Prirodoslovno-matematički fakultet, Zagreb