Napredna pretraga

Pregled bibliografske jedinice broj: 116308

Orographic influence on Adriatic vortex generation


Ivančan-Picek, Branka; Jurčec, Vesna
Orographic influence on Adriatic vortex generation // International Conference on Alpine Meteorology and MAP meeting 2003, Extended Abstracts, Vol. A and B, Publication of MeteoSwiss, No.66 / Binder, Peter ; Richner, Hans (ur.).
Zurich: MeteoSwiss, 2003. str. 550-552 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


Naslov
Orographic influence on Adriatic vortex generation

Autori
Ivančan-Picek, Branka ; Jurčec, Vesna

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

Izvornik
International Conference on Alpine Meteorology and MAP meeting 2003, Extended Abstracts, Vol. A and B, Publication of MeteoSwiss, No.66 / Binder, Peter ; Richner, Hans - Zurich : MeteoSwiss, 2003, 550-552

Skup
International Conference on Alpine Meteorology and MAP meeting 2003

Mjesto i datum
Brig, Švicarska, 19. - 23. svibnja 2003

Vrsta sudjelovanja
Poster

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
cyclonic vortex; ageostrophic circulation; local winds; mesoscale wind analysis; orographic influence

Sažetak
The subject of this study is a cyclonic vortex genesis in the wind field over the Adriatic Sea. The vortex is an unbalanced - ageostrophic circulation system in which the center of vortex does not coincide with the center of low pressure. It is not formed by the lee-side effects as Alpine lee cyclogenesis, but the orographic influence appears through the special local winds - bora in the northern and jugo in the southern Adriatic. Both winds are relatively shallow and modified by the Dinaric Alps. Bora flow originates in the eastern side of Alps indicating an internal hydraulic mechanism across the mountain barrier. The jugo wind is associated with a cyclonic circulation in the Genoa bay entering the Adriatic area adds a southerly wind, but changing the direction to SE when approaching the coastal mountain barrier of Dinaric Alps. Mesoscale wind analysis emphasises a current through the valley in northern Italy (not the western side of Alps) toward the Genoa bay. An example of such a vortex generation is presented for the case of October 1999 during the MAP IOP 5.

Izvorni jezik
Engleski

Znanstvena područja
Geologija



POVEZANOST RADA


Projekt / tema
0004001

Ustanove
Državni hidrometeorološki zavod

Profili:

Avatar Url Vesna Jurčec (autor)

Avatar Url Branka Ivančan-Picek (autor)

Citiraj ovu publikaciju

Ivančan-Picek, Branka; Jurčec, Vesna
Orographic influence on Adriatic vortex generation // International Conference on Alpine Meteorology and MAP meeting 2003, Extended Abstracts, Vol. A and B, Publication of MeteoSwiss, No.66 / Binder, Peter ; Richner, Hans (ur.).
Zurich: MeteoSwiss, 2003. str. 550-552 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
Ivančan-Picek, B. & Jurčec, V. (2003) Orographic influence on Adriatic vortex generation. U: Binder, P. & Richner, H. (ur.)International Conference on Alpine Meteorology and MAP meeting 2003, Extended Abstracts, Vol. A and B, Publication of MeteoSwiss, No.66.
@article{article, year = {2003}, pages = {550-552}, keywords = {cyclonic vortex, ageostrophic circulation, local winds, mesoscale wind analysis, orographic influence}, title = {Orographic influence on Adriatic vortex generation}, keyword = {cyclonic vortex, ageostrophic circulation, local winds, mesoscale wind analysis, orographic influence}, publisher = {MeteoSwiss}, publisherplace = {Brig, \v{S}vicarska} }