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Pregled bibliografske jedinice broj: 301427

"Zadar calm" during severe Bora


Ivančan-Picek, Branka; Grubišić, Vanda; Stiperski, Ivana; Xiao, Ming; Bajić, Alica
"Zadar calm" during severe Bora // 29th International Conference on Alpine Meteorology, Extended abstracts, 4– 8 June 2007, Chambery, France, Vol. 1 / Meteo-France (ur.).
Toulouse, 2007. str. 11-14 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


Naslov
"Zadar calm" during severe Bora

Autori
Ivančan-Picek, Branka ; Grubišić, Vanda ; Stiperski, Ivana ; Xiao, Ming ; Bajić, Alica

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
29th International Conference on Alpine Meteorology, Extended abstracts, 4– 8 June 2007, Chambery, France, Vol. 1 / Meteo-France - Toulouse, 2007, 11-14

Skup
29th International Conference on Alpine Meteorology

Mjesto i datum
Chambery, Francuska, 4-8.06.2007

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Bora flow; sodar; flow separation; mesoscale variability

Sažetak
In this study, we investigate small-scale characteristics and spatial variability of severe Bora flow in the wider Zadar area with the objective of identifying reasons for the “ Zadar calm” . A detailed analysis of several severe Bora events that occurred in the winter-spring 2004/5 season is undertaken, during which a new sodar system was deployed at the Zadar-Zemunik airport, which provided continuous vertical soundings from 40 to 700 m MSL at the temporal resolution of 10 minutes. The Zadar sodar data reveals a significant variability in the wind speed and direction during the severe Bora events. The maximum Bora speeds were observed in the layer between 300 and 500 m MSL, while the low-level flow was characterized by weak winds. This observational analysis also includes surface data from Zadar and several automatic weather stations located inside the target area, as well as the Zadar - Zemunik radio-sounding data. Initial simulation results indicate that the Bora flow never fully penetrated to the surface near the coast in the Zadar area. The simulation results also suggest that the primary mountain wave could be responsible for low-level flow separation over the steep terrain, leading to weak surface winds over Zadar, downstream of Velebit.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekt / tema
004-1193086-3036 - Oluje i prirodne katastrofe u Hrvatskoj (Branka Ivančan-Picek, )
083-0821466-1465 - POUZDANOST KONSTRUKCIJA I PROCJENA RIZIKA USLIJED EKSTREMNIH DJELOVANJA (Bernardin Peroš, )

Ustanove
Državni hidrometeorološki zavod