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Pregled bibliografske jedinice broj: 933326

Wintertime dynamics in the coastal northeastern Adriatic Sea: the NAdEx 2015 experiment


Vilibić, Ivica; Mihanović, Hrvoje; Janeković, Ivica; Denamiel, Cléa; Poulain, Pierre-Marie; Orlić, Mirko; Dunić, Natalija; Dadić, Vlado; Pasarić, Miroslava; Muslim, Stipe et al.
Wintertime dynamics in the coastal northeastern Adriatic Sea: the NAdEx 2015 experiment // Ocean science, 14 (2018), 2; 237-258 doi:10.5194/os-14-237-2018 (međunarodna recenzija, članak, znanstveni)


Naslov
Wintertime dynamics in the coastal northeastern Adriatic Sea: the NAdEx 2015 experiment

Autori
Vilibić, Ivica ; Mihanović, Hrvoje ; Janeković, Ivica ; Denamiel, Cléa ; Poulain, Pierre-Marie ; Orlić, Mirko ; Dunić, Natalija ; Dadić, Vlado ; Pasarić, Miroslava ; Muslim, Stipe ; Gerin, Riccardo ; Matić, Frano ; Šepić, Jadranka ; Mauri, Elena ; Kokkini, Zoi ; Tudor, Martina ; Kovač, Žarko ; Džoić, Tomislav

Izvornik
Ocean science (1812-0784) 14 (2018), 2; 237-258

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
Adriatic Sea ; dense water formation ; in situ data

Sažetak
The paper investigates the wintertime dynamics of the coastal northeastern Adriatic Sea and is based on numerical modelling and in situ data collected through field campaigns executed during the winter and spring of 2015. The data were collected with a variety of instruments and platforms (acoustic Doppler current profilers, conductivity– temperature–depth probes, glider, profiling float) and are accompanied by the atmosphere–ocean ALADIN/ROMS modelling system. The research focused on the dense-water formation (DWF), thermal changes, circulation, and water exchange between the coastal and open Adriatic. According to both observations and modelling results, dense waters are formed in the northeastern coastal Adriatic during cold bora outbreaks. However, the dense water formed in this coastal region has lower densities than the dense water formed in the open Adriatic due to lower salinities. Since the coastal area is deeper than the open Adriatic, the observations indicate (i) balanced inward–outward exchange at the deep connecting channels of denser waters coming from the open Adriatic DWF site and less-dense waters coming from the coastal region and (ii) outward flow of less-dense waters dominating in the intermediate and surface layers. The latter phenomenon was confirmed by the model, even if it significantly underestimates the currents and transports in the connecting channels. The median residence time of the coastal area is estimated to be approximately 20 days, indicating that the coastal area may be renewed relatively quickly by the open Adriatic waters. The data that were obtained represent a comprehensive marine dataset that can be used to calibrate atmospheric and oceanic numerical models and point to several interesting phenomena to be investigated in the future.

Izvorni jezik
Engleski

Znanstvena područja
Geofizika, Interdisciplinarne prirodne znanosti



POVEZANOST RADA


Projekt / tema
FP7-312762
HHRZZ-IP-2013-11-5928
HRZZ-IP-2013-11-2831 - Klima jadranske regije u njenom globalnom kontekstu (Mirko Orlić, )
HRZZ-IP-2014-09-3606 - Morski plankton kao alat za procjenu klimatsdkog i antropogenog utjecaja na morski ekosustav (Živana Ninčević Gladan, )
HRZZ-IP-2014-09-5747 - Sklerokronologija kao alat za otkirvanje dugoročnih okolišnih promjena na Jadranu (Melita Peharda Uljević, )
HRZZ-IP-2016-06-1955 - Višegodišnje i dekadne oscilacije Jadranskog mora: opažanja, modeliranje i posljedice (Ivica Vilibić, )
IPACBC-1◦ STR/0005

Ustanove
Institut za oceanografiju i ribarstvo, Split,
Državni hidrometeorološki zavod,
Institut "Ruđer Bošković", Zagreb,
Prirodoslovno-matematički fakultet, Zagreb

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


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