Pregled bibliografske jedinice broj: 295924
Wintertime buoyancy forcing, changing seawater properties, and two different circulation systems produced in the Adriatic
Wintertime buoyancy forcing, changing seawater properties, and two different circulation systems produced in the Adriatic // Journal of geophysical research, 111 (2006), C3; C03S07, 21 doi:10.1029/2005JC003271 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 295924 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Wintertime buoyancy forcing, changing seawater
properties, and two different circulation systems
produced in the Adriatic
Autori
Orlić, Mirko ; Dadić, Vlado ; Grbec, Branka ; Leder, Nenad ; Marki, Antun ; Matić, Frano ; Mihanović, Hrvoje ; Beg Paklar, Gordana ; Pasarić, Miroslava ; Pasarić, Zoran ; Vilibić, Ivica
Izvornik
Journal of geophysical research (0148-0227) 111
(2006), C3;
C03S07, 21
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
buoyancy forcing ; circulation ; Adriatic
Sažetak
Measurements performed in winter 2002/2003 and spring 2003 off the east Adriatic coast showed that the East Adriatic Current (EAC) peaked in January/February (as expected from previous findings) and again in May (not expected). The first maximum corresponded with the considerable cross-shore variability of seawater properties, the colder, fresher water prevailing close to the coast, the warmer, saltier water dominating the open sea. The second maximum coincided with the massive intrusion of warm, saline water from the south Adriatic. Meteorological and hydrologic forcing was anomalous over the measurement interval: during winter 2002/2003 the cooling and river outflows were strong, during spring 2003 the pronounced warming coincided with exceptional dryness. In order to interpret the two EAC maxima a simple numerical model reproducing response of the Adriatic-Mediterranean system to the wintertime forcing was developed. It was found that the first maximum could be related to the coastal freshwater input and offshore evaporation in the Adriatic area, and that the second maximum was probably due to the wintertime surface cooling of the Adriatic while warmer conditions prevailed above the Mediterranean. The resulting horizontal density gradients supported two different circulation systems, one within the Adriatic, the other between the Adriatic and east Mediterranean, and they differed not only in spatial but also in temporal scales, therefore supporting the occurrence of two distinctive EAC maxima.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
MZOS-001-0013077-1122 - Istraživanje i sustavi praćenja neuobičajene dinamike Jadrana (Vilibić, Ivica, MZOS ) ( CroRIS)
MZOS-119-1193086-3085 - Utjecaj atmosfere i topografske varijabilnosti na procese u moru (Orlić, Mirko, MZOS ) ( CroRIS)
MZOS-001-0013077-1118 - Kooscilacije atmosfere i mora važne za ekosustav Jadrana (Morović, Mira, MZOS ) ( CroRIS)
Ustanove:
Institut za oceanografiju i ribarstvo, Split,
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Ivica Vilibić
(autor)
Zoran Pasarić
(autor)
Miroslava Pasarić
(autor)
Vlado Dadić
(autor)
Mirko Orlić
(autor)
Nenad Leder
(autor)
Branka Grbec
(autor)
Gordana Beg Paklar
(autor)
Frano Matić
(autor)
Antun Marki
(autor)
Hrvoje Mihanović
(autor)
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