Naslov
Orographic effects on meteorological fields over the Adriatic from different models

Autori
Pasarić, Zoran ; Belušić, Danijel ; Chiggiato, J.

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Recent Advances in Adriatic Oceanography and Marine Meteorology / Orlić, Mirko ; Pasarić, Miroslava - Zagreb : Geofizički odsjek Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu, 2008, 46-46

ISBN
978-953-6076-18-5

Skup
Recent Advances in Adriatic Oceanography and Marine Meteorology

Mjesto i datum
Dubrovnik, Hrvatska, 05.11.2008. - 07.11.2008

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Nije recenziran

Ključne riječi
Adriatic; orografic effects; models
(Adriatic; orografic effects; numerical models)

Sažetak
The effects that orography may exert on meteorological fields over the Adriatic region are investigated by analyzing the output fields from the mesoscale meteorological model LAMI and the global ECMWF model. The analysis is performed over four weather regimes typical for the Adriatic Sea, namely those characterized by bora, sirocco, bora-sirocco and etesian winds. The investigated period stretches between October 2005 and September 2006. Analyzed are mean fields and mean differences between the two models. Results indicate that all investigated flow regimes are significantly affected by the Apennines and the Dinaric Alps, but also by smaller scale orography that is at least along the Italian coast adequately represented by LAMI and not by the ECMWF model. A kind of symmetry is found between sirocco and etesian regimes on the Adriatic scale, as well as on smaller scales, e.g. around the Gargano peninsula which acts as a typical 3D obstacle. Well known jets-and-wakes bora pattern along the eastern coast is clearly seen in the mean fields. The enhanced cloudiness and precipitation regions are shown to appear in convergence zones of bora, bora-sirocco and sirocco regimes, related to the mountain ridges perpendicular to the respective flow. Additionally, within the bora-sirocco regime a relatively narrow convergence zone at the boundary between the bora and sirocco flow is noticed. We believe that the methods used can be useful when applied to other coastal regions and models. By considering the differences between output fields from two models of different resolution the areas affected by smaller scale phenomena could be clearly seen. On the other side, the mean modeled fields show persistent meso to synoptic scale structures thus enabling better understanding of dynamical and climatological characteristics, both of the considered region and the models used.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA