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pro vyhledávání: '"Edier Aristizábal (d)"'
Autor:
Roberto J. Marin(a, María Fernanda Velásquez (a, Edwin F. García (b), Massimiliano Alvioli (c), Edier Aristizábal (d)
Publikováno v:
Catena (Cremling.) 206 (2021): 105563. doi:10.1016/j.catena.2021.105563
info:cnr-pdr/source/autori:Roberto J. Marin(a,b), María Fernanda Velásquez (a,b), Edwin F. García (b), Massimiliano Alvioli (c), Edier Aristizábal (d)/titolo:Assessing two methods to define rainfall intensity and duration thresholds for shallow landslides in data-scarce catchments of the Colombian Andean Mountains/doi:10.1016%2Fj.catena.2021.105563/rivista:Catena (Cremling.)/anno:2021/pagina_da:105563/pagina_a:/intervallo_pagine:105563/volume:206
info:cnr-pdr/source/autori:Roberto J. Marin(a,b), María Fernanda Velásquez (a,b), Edwin F. García (b), Massimiliano Alvioli (c), Edier Aristizábal (d)/titolo:Assessing two methods to define rainfall intensity and duration thresholds for shallow landslides in data-scarce catchments of the Colombian Andean Mountains/doi:10.1016%2Fj.catena.2021.105563/rivista:Catena (Cremling.)/anno:2021/pagina_da:105563/pagina_a:/intervallo_pagine:105563/volume:206
Rainfall thresholds are intensity-duration relations that are supposedly able to distinguish precipitation events that may or may not trigger landslides. The most common method for defining rainfall thresholds relies on observed landslides and the co