Napredna pretraga

Pregled bibliografske jedinice broj: 692426

Landslides Triggered in the Continental Part of Croatia by Extreme Precipitation in 2013


Bernat, Sanja; Mihalić Arbanas, Snježana; Krkač, Martin
Landslides Triggered in the Continental Part of Croatia by Extreme Precipitation in 2013 // Proceedings of the XII IAEG Congress 'Engineering Geology for Society and Territory', Vol. 2 'Landslide Processes' / Lollino, Giorgio ; Giordan, Daniele ; Battista Crosta, Giovanni ; Corominas, Jordi ; Azzam, Rafig ; Wasowski, Janusz ; Sciarra, Nicola (ur.).
Heidelberg: Springer, 2015. str. 1599-1603 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


Naslov
Landslides Triggered in the Continental Part of Croatia by Extreme Precipitation in 2013

Autori
Bernat, Sanja ; Mihalić Arbanas, Snježana ; Krkač, Martin

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

Izvornik
Proceedings of the XII IAEG Congress 'Engineering Geology for Society and Territory', Vol. 2 'Landslide Processes' / Lollino, Giorgio ; Giordan, Daniele ; Battista Crosta, Giovanni ; Corominas, Jordi ; Azzam, Rafig ; Wasowski, Janusz ; Sciarra, Nicola - Heidelberg : Springer, 2015, 1599-1603

ISBN
978-3-319-09056-6

Skup
XII IAEG Congress 'Engineering Geology for Society and Territory'

Mjesto i datum
Torino, Italy, 15-19.09.2014

Vrsta sudjelovanja
Poster

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Soil slides ; Extreme precipitation ; Empirical thresholds ; Croatia

Sažetak
The subject of this paper are landslides triggered by the extreme precipitation during winter and spring of 2013. More than 900 landslides were (re)activated in the continental part of Croatia during the analyzed period. This paper presents preliminary analysis results of the relationship between 55 slide-type occurrences and precipitation conditions. The preliminary analysis is based on the sliding data from the hilly area of Medvednica Mt. in the City of Zagreb. The exact landslide location, the slope failure time, information on the precipitation duration D and the mean intensity I, which have resulted in landslide activation, are known for each analyzed landslide event. A comparison of precipitation series and landslides occurrence dates with global rainfall intensity-duration (ID) thresholds showed that precipitation conditions exceeded threshold values and were likely to trigger a landslide. The results will be used for further study of the empirical threshold of landslides in the area of NW Croatia.

Izvorni jezik
Engleski

Znanstvena područja
Rudarstvo, nafta i geološko inženjerstvo



POVEZANOST RADA


Ustanove
Rudarsko-geološko-naftni fakultet, Zagreb

Časopis indeksira:


  • Web of Science Core Collection (WoSCC)
    • Conference Proceedings Citation Index - Science (CPCI-S)
  • Scopus