Pregled bibliografske jedinice broj: 847740
Analysis of flash flood occurred at Slani potok chachement, Croatia
Analysis of flash flood occurred at Slani potok chachement, Croatia // Landslide and flood hazard assesment /Proceedings / Arbanas MIhalić, Snježana ; Arbanas, Željko (ur.).
Zagreb: Faculty of Mining, Geology and Petrleum Rngineering, University of Zagreb and Faculty of Civil Engineering, University of Rijeka, 2014. str. 107-110 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 847740 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Analysis of flash flood occurred at Slani potok chachement, Croatia
Autori
Sušanj, Ivana ; Ožanić, Nevenka ; Yamashiki, Yosuke
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Landslide and flood hazard assesment /Proceedings
/ Arbanas MIhalić, Snježana ; Arbanas, Željko - Zagreb : Faculty of Mining, Geology and Petrleum Rngineering, University of Zagreb and Faculty of Civil Engineering, University of Rijeka, 2014, 107-110
ISBN
978-953-6953-43-1
Skup
1st Regional Symposium on Landslides in the Adriatic-Balkan Region, 3rd Workshop of the Japanese-Croatian Project "Risk Identification and Land-Use Planning for Disaster Mitigation of Landslides and Floods in Croatia"
Mjesto i datum
Zagreb, Hrvatska, 06.04.2013. - 09.04.2013
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Flash flood ; Slani potok ; water level
Sažetak
Estimation of potential hazard caused by flash flood is important for the design and construction of the structural mitigation elements. Due to this matter, river discharge after short time rain event and its environmental impact are two main parameters that have to be studied in detail. Measurement of water velocity is difficult when short time flash flood occurred and at the same time is crucial for calculation of water discharge. This paper describes the calculation procedure of river discharge after high rain intensity when water level and velocity data are not available. Calculation is based on flash flood water table traces (left after flash flood) and riverbed geometry.
Izvorni jezik
Engleski
Znanstvena područja
Građevinarstvo
POVEZANOST RADA
Ustanove:
Građevinski fakultet, Rijeka