Pregled bibliografske jedinice broj: 227976
Regional short-term heavy rainfalls and their causes
Regional short-term heavy rainfalls and their causes // Geophysical Research Abstracts, Vol. 7, EGU General Assembly 2005
Beč: European Geosciences Union (EGU), 2005. (poster, nije recenziran, sažetak, ostalo)
CROSBI ID: 227976 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Regional short-term heavy rainfalls and their causes
Autori
Gajić-Čapka, Marjana ; Horvat, Melita
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, ostalo
Izvornik
Geophysical Research Abstracts, Vol. 7, EGU General Assembly 2005
/ - Beč : European Geosciences Union (EGU), 2005
Skup
European Geophysical Union, General Assembly 2005
Mjesto i datum
Beč, Austrija, 24.04.2005. - 29.04.2005
Vrsta sudjelovanja
Poster
Vrsta recenzije
Nije recenziran
Ključne riječi
heavy reanfall; extreme value analysis; weather types; Croatia
Sažetak
This paper deals with the investigation of magnitude (design parameter) and causes (forecasting input) of rainfall extremes over this region (coastal and inland sites). Extreme value analysis (GEV) according to Jenkinson (Jenkinson, 1969, Faragó and Katz, 1990, Gajic-Capka, 1991) has been applied to rainfall maxima for intervals t up to two hours that are relevant for surface drainage. Jenkinson distribution for almost all intervals has positive values of curvature parameter k, except for very short intervals (10-40 min) in inland, but close to zero. Estimated short-term rainfall maxima are a little bit higher in inland than at coastal site (10-15%).During the period 1985-2002 weather type characterized by front side of the cyclone caused heavy precipitation in 26% of the episodes at the coast and in 31% in inland. These were the weak cyclones with the pressure of 1000 hPa in its centre and their front side over the Istra peninsula and Northern Adriatic. It was followed by low air pressure weather types, front side of trough, with 12% of episodes in inland and back side of trough, with 14% of episodes at the coast. Unexpectedly 11% of rainfall episodes were caused by low gradient anticyclone surface field. In the most cases they were accompanied by upper level cyclones or low pressure troughs.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA