Pregled bibliografske jedinice broj: 570486
Mechanisms producing heavy precipitation event in the southern Adriatic area
Mechanisms producing heavy precipitation event in the southern Adriatic area // Proceedings - 6th European Conference on Severe Storms (ECSS 2011), Palma de Mallorca, Spain, 03-07 October 2011
Palma de Mallorca, Španjolska, 2011. (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 570486 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Mechanisms producing heavy precipitation event in the southern Adriatic area
Autori
Ivančan-Picek, Branka ; Horvath, Kristian ; Strelec Mahović, Nataša
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Proceedings - 6th European Conference on Severe Storms (ECSS 2011), Palma de Mallorca, Spain, 03-07 October 2011
/ - , 2011
Skup
6th European Conference on Severe Storms (ECSS 2011), Palma de Mallorca, Spain, 03-07 October 2011
Mjesto i datum
Palma de Mallorca, Španjolska, 03.10.2011. - 07.10.2011
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
heavy precipitation; WRF model; satellite data; orography
Sažetak
Extreme precipitation event occurred in the morning hours on 22 November 2010 over Dubrovnik, Croatia and the surrounding area of the southern Dinaric Alps mountain range. The rain gauge measurements in Dubrovnik exceeded 160 mm / 24 h, with a peak intensity of 71.5 mm/h. The event caused severe flash floods, landslides, interruption of traffic and electricity as well as other infrastructural damage. The synoptic environment was characterized by a deep cyclone moving from northern Europe over the Alps and farther east. The associated frontal system covered most of the central Europe and the mid-Mediterranean. The mechanisms responsible for the formation of convection have been analyzed though synoptic measurements, satellite data and numerical experiments performed with the WRF model, which was set up at the convection-resolving resolution in the innermost domain. The numerical simulations highlighted the essential role of southerly low-level jet stream (LLJS) in the transport of warm and moist air towards the affected area. In addition, numerical sensitivity experiments shaded light on the role of the complex orography of the southern Dinaric Alps on the initialization and development of convection over the target area.
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