Naslov
The mechanism of severe bora wind

Autori
Grisogono, Branko

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, neobjavljeni rad, znanstveni

Izvornik
Tellus A / - , 2010

Skup
Ponedeljkov fizikalni kolokvij

Mjesto i datum
Ljubljana, Slovenija, 10.05.2010

Vrsta sudjelovanja
Pozvano predavanje

Vrsta recenzije
Nije recenziran

Ključne riječi
downslope windstorm; orographic-wave breaking; pulsations; rotors; turbulence

Sažetak
A gusty downslope windstorm which blows at the eastern Adriatic coast is called bora. There has been substantial progress in bora observations and measurements, understanding, modeling and its more detailed prediction during the last 25 years. It was generally thought before that bora was a falling, mostly thermodynamically driven wind ; however, (severe) bora is primarily governed by mountain wave breaking. Understandings of bora interactions and influences on other processes have taken place as well, most notably in the air-sea interaction, but are not completed yet. The focus here is on stronger bora flows at the NE Adriatic coast.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

Napomena
Pozvano predavanje održano je u sklopu nastavka suradnje s koleg(ic)ama u Ljubljani, napose s doc. dr. Nedjeljkom Žagar, suradnicom na projektu BORA. Suradnja se odvija i kroz međunarodni projekt EMEP4HR. Rezultati iznijeti u predavanju objavljeni su 2009. godine u znanstvenom radu u časopisu Tellus A kojega citira CC baza u koautorstvu s Danijelom Belušićem (CROSBI 365902).

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