Naslov
Dense water formation in the coastal northeastern Adriatic Sea: the NAdEx 2015 experiment

Autori
Vilibić, Ivica ; Mihanović, Hrvoje ; Janeković, Ivica ; Denamiel, Clea ; 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

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, neobjavljeni rad, znanstveni

Skup
10th HyMeX Workshop

Mjesto i datum
Barcelona, Španjolska, 04.07.2017. - 07.07.2017

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
dense water formation ; northern Adriatic ; multi-platform experiment

Sažetak
The paper investigates 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 have been collected by a variety of instruments and platforms (ADCPs, CTDs, glider, profiling float), and have been accompanied by atmospheric-ocean ALADIN/ROMS modelling system. Research focus has been put on dense water formation, thermal changes and 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, dense water formed in this coastal region has, due to lower salinities, lower densities than dense water formed at the open Adriatic. Since the sea is deeper in the coastal area than at the open Adriatic, dense waters from the open Adriatic occasionally enter the coastal area near the bottom of the connecting passages, while the surface flow is mostly outward from the coastal area. Median residence time of the coastal area is estimated to be about 1-2 months, indicating that the coastal area may be relatively quickly renewed by the open Adriatic waters. The model significantly underestimates currents and transports in connecting channels, which may be a result of a too coarse resolution of atmospheric forcing, misrepresentation of bathymetry or absence of the air-sea feedback in the model. Obtained data represents a comprehensive marine dataset, pointing to a number of interesting phenomena to be investigated in the future.

Izvorni jezik
Engleski

Znanstvena područja
Geofizika

POVEZANOST RADA