Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Two Different Circulation Systems Produced By Wintertime Buoyancy Forcing Of The Adriatic (CROSBI ID 506931)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa

Orlić, Mirko ; Dadić, Vlado ; Grbec, Branka ; Leder, Nenad ; Matić, Frano ; Mihanović, Hrvoje ; Beg Paklar, Gordana ; Pasarić, Miroslava ; Pasarić, Zoran ; Vilibić, Ivica Two Different Circulation Systems Produced By Wintertime Buoyancy Forcing Of The Adriatic // The Oceanography Society's 2005 International Ocean Research Conference, Program and Abstracts / ? (ur.). Pariz, 2005. str. 124-124-x

Podaci o odgovornosti

Orlić, Mirko ; Dadić, Vlado ; Grbec, Branka ; Leder, Nenad ; Matić, Frano ; Mihanović, Hrvoje ; Beg Paklar, Gordana ; Pasarić, Miroslava ; Pasarić, Zoran ; Vilibić, Ivica

engleski

Two Different Circulation Systems Produced By Wintertime Buoyancy Forcing Of The Adriatic

Measurements performed in winter and spring 2003 showed that - contrary to the expectations - the East Adriatic Current (EAC) peaked in January/February and again in May. The first maximum corresponded with the considerable cross-shore variability of hydrographic properties, the second one coincided with the massive intrusion of warm, saline water. Meteorological and hydrological forcing was anomalous over the measurement interval: during winter 2003 the cooling and river outflows were strong, during spring 2003 the pronounced warming was combined with exceptional dryness. In order to interpret the two EAC maxima a simple numerical model of the Adriatic-Mediterranean system has been 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 surface cooling of the Adriatic while warmer conditions prevailed above the Mediterranean. Thus, two circulation systems developed, one inside the Adriatic, the other between the Adriatic and the Mediterranean, and they differed not only in spatial but also in temporal scales, therefore supporting the occurrence of two EAC maxima.

buoyancy forcing; circulation systems; Adriatic

NEPOTPUN BIBLIOGRAFSKI ZAPIS!!

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o prilogu

124-124-x.

2005.

objavljeno

Podaci o matičnoj publikaciji

The Oceanography Society's 2005 International Ocean Research Conference, Program and Abstracts

?

Pariz:

Podaci o skupu

The Oceanography Society's 2005 International Ocean Research Conference

poster

06.06.2005-10.06.2005

Pariz, Francuska

Povezanost rada

Geologija