Pregled bibliografske jedinice broj: 392952
The complex bora flow in the lee of Southern Velebit
The complex bora flow in the lee of Southern Velebit // 30th International Conference on Alpine Meteorology - Programme & Extended Abstracts. Deutscher Wetterdienst: Annalen der Meteorologie, 44 / Volkert, Hans (ur.).
Offenbach: Deutscher Wetterdienst, 2009. str. 216-217 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 392952 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The complex bora flow in the lee of Southern Velebit
Autori
Stiperski, Ivana ; Ivančan-Picek, Branka ; Grubišić, Vanda
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
30th International Conference on Alpine Meteorology - Programme & Extended Abstracts. Deutscher Wetterdienst: Annalen der Meteorologie, 44
/ Volkert, Hans - Offenbach : Deutscher Wetterdienst, 2009, 216-217
ISBN
978-3-88148-440-4
Skup
30th International Conference on Alpine Meteorology
Mjesto i datum
Rastatt, Njemačka, 11.05.2009. - 15.05.2009
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
bora; critical level; orography; rotors; upstream conditions; wake
Sažetak
The complex flow structure in the lee of the Southern Velebit is investigated by means of very high-resolution numerical simulations carried out with the NRL COAMPS model. The focus is placed on a wintertime severe bora episode. The spatially complex and temporally highly variable 3D flow structure is characterized by a hydraulic jump over the lee slope and a pronounced wake over the Zadar area. The wake structure appears very sensitive to the upstream flow evolution and is highly non-stationary. The reversed flow along the wake centerline as well as flow separation and rotor formation are observed during different stages of the bora evolution. Sensitivity experiments show the height of Velebit exerting a strong influence on the flow structure, including the onset and strength of the bora flow and the structure of the wake. The terrain of the Zadar peninsula, although significantly lower than that of Velebit, is shown to influence the characteristics of the fully developed bora flow.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
004-1193086-3036 - Oluje i prirodne katastrofe u Hrvatskoj (Ivančan-Picek, Branka, MZOS ) ( CroRIS)
Ustanove:
Državni hidrometeorološki zavod