crta
Hrvatska znanstvena Sekcija img
bibliografija
3 gif
 Naslovna
 O projektu
 FAQ
 Kontakt
4 gif
Pregledavanje radova
Jednostavno pretraživanje
Napredno pretraživanje
Skupni podaci
Upis novih radova
Upute
Ispravci prijavljenih radova
Ostale bibliografije
Slični projekti
 Bibliografske baze podataka

Pregled bibliografske jedinice broj: 741320

Zbornik radova

Autori: Mihanovic, Hrvoje; Janekovic, Ivica; Vilibic, Ivica; Tudor, MArtina
Naslov: Dense water formation in the eastern coastal Adriatic during an extreme cooling event
( Dense water formation in the eastern coastal Adriatic during an extreme cooling event )
Izvornik: European Geosciences Union General Assembly 2014 / Sandro Carniel | Co-Conveners: Agustín Sánchez-Arcilla , Judith Wolf , Emil Stanev , Georg Umgiesser (ur.). - Vienna, Austria : Copernicus gmbh , 2014. .
Skup: European Geosciences Union General Assembly 2014
Mjesto i datum: Beč, Austrija, 27 April – 02 May 2014
Ključne riječi: dense water; Adriatic; cold air outbreak
( dense water; Adriatic; cold air outbreak )
Sažetak:
Dense water formation (DWF) that occurred in both open and coastal waters of the Adriatic Sea during extreme cooling event in January/February 2012 was reproduced by coupled high-resolution atmosphere-ocean modelling system. Regional Ocean Modeling System (ROMS) ocean model has been applied with resolution of 2 km and with lateral boundaries coming from the operational AREG Adriatic model. The model has been forced at the sea surface by the operational NWP model ALADIN/HR, providing winds at 2 km spatial resolution via dynamical adaptation technique every 3 hours, while other bulk variables were computed at 8 km resolution and used every 3 hours. Two model experiments were conducted (simulations starting in 2008): the first with real river fluxes in January 2011 – July 2012 period, for Po River, all available Croatian rivers and power-plants outflows and recently compiled Slovenian river data, together with mean year daily fluxes for other Adriatic rivers. The second experiment used climatological perpetual river fluxes computed from all available hydrological data throughout the model run. Eastern Adriatic coastal river fluxes turned out to have a dramatically lower both perpetual and real freshwater fluxes compared to traditionally used climatological river fluxes documented by Raicich (1994) and mostly used in previous Adriatic modelling studies
Vrsta sudjelovanja: Predavanje
Vrsta prezentacije u zborniku: Sažetak
Vrsta recenzije: Međunarodna recenzija
Izvorni jezik: eng
Kategorija: Znanstveni
Znanstvena područja:
Geologija
Puni text rada: 741320.EGU2014-4992-1.pdf (tekst priložen 15. Pro. 2014. u 15:49 sati)
URL Internet adrese: http://meetingorganizer.copernicus.org/EGU2014/EGU2014-4992-1.pdf
http://meetingorganizer.copernicus.org/EGU2014/orals/14438
Upisao u CROSBI: Martina Tudor (tudor@cirus.dhz.hr), 15. Pro. 2014. u 15:49 sati



Verzija za printanje   za tiskati


upomoc
foot_4