Pregled bibliografske jedinice broj: 523700
Coastal sea responses to atmospheric forcings at two different resolutions
Coastal sea responses to atmospheric forcings at two different resolutions // Ocean science, 7 (2011), 521-532 doi:10.5194/os-7-521-2011 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 523700 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Coastal sea responses to atmospheric forcings at two different resolutions
Autori
Bencetić Klaić, Zvjezdana ; Pasarić, Zoran ; Beg Paklar, Gordana ; Oddo, Paolo
Izvornik
Ocean science (1812-0784) 7
(2011);
521-532
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
ALADIN; bora; ECMWF; model; sirocco
Sažetak
We investigated coastal sea responses to three, multi-day strong wind episodes that occurred in the middle Adriatic during the Target Operational Period (TOP) of the European COastal sea OPerational observing and forecasting system (ECOOP) project. A high-resolution oceanographic model (1 km horizontal, 16 vertical layers) based on the modified Princeton Ocean Model (POM) was applied to a highly complex domain located in the coastal area of the eastern Adriatic Sea. The oceanographic model was nested into the Adriatic REGional model (AREG-2) covering the entire Adriatic Sea. Meteorological forcing was prepared by two atmospheric models. The coarser model was the European Centre for Medium-range Weather Forecast model (ECMWF, with horizontal and temporal resolutions of 0.25 and 6 h, respectively), and the finer one was the Aire Limit´ee Adaptation dynamique D´eveloppement InterNational model (ALADIN, with horizontal and temporal resolutions of 8 km and 3 h, respectively, and winds dynamically adapted to a horizontal resolution of 2 km). The results show that smallscale atmospheric features, which arise due to the orographically complex mainland and the number of islands and were not reproduced by the coarser atmospheric model, substantially affected surface currents, mass transports, sea surface temperature (SST) and surface salinity in the coastal area during strong Bora. For strong Sirocco, the atmospheric model’s resolution was important for currents on the lee sides of islands.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
001-0013077-1118 - Kooscilacije atmosfere i mora važne za ekosustav Jadrana (Morović, Mira, MZOS ) ( CroRIS)
001-0013077-1122 - Istraživanje i sustavi praćenja neuobičajene dinamike Jadrana (Vilibić, Ivica, MZOS ) ( CroRIS)
119-1193086-1323 - Kakvoća zraka nad kompleksnom topografijom (Bencetić-Klaić, Zvjezdana, MZOS ) ( CroRIS)
119-1193086-3085 - Utjecaj atmosfere i topografske varijabilnosti na procese u moru (Orlić, Mirko, MZOS ) ( CroRIS)
Ustanove:
Institut za oceanografiju i ribarstvo, Split,
Prirodoslovno-matematički fakultet, Zagreb
Poveznice na cjeloviti tekst rada:
Pristup cjelovitom tekstu rada doi www.ocean-sci.net www.ocean-sci.netCitiraj 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