Landslides and Quaternary climate changes—The state of the art

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F19%3AA20024HE" target="_blank" >RIV/61988987:17310/19:A20024HE - isvavai.cz</a>
Result on the web
<a href="https://reader.elsevier.com/reader/sd/pii/S0012825219300704?token=2448D936A1E71D7A1CFAC2A610A7D7F35369003FB310CA70D7195636429D0DA782FB3DC59C34CCFCA78F8CC9081A3048" target="_blank" >https://reader.elsevier.com/reader/sd/pii/S0012825219300704?token=2448D936A1E71D7A1CFAC2A610A7D7F35369003FB310CA70D7195636429D0DA782FB3DC59C34CCFCA78F8CC9081A3048</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.earscirev.2019.05.015" target="_blank" >10.1016/j.earscirev.2019.05.015</a>

Result language
angličtina
Original language name
Landslides and Quaternary climate changes—The state of the art
Original language description
Climatic factors are considered major causes and triggers of slope instability, but the palaeoclimatic implications of landslides have not yet been systematically reviewed. As inferred from landslides dated to the Late Glacial and Holocene, glacial-interglacial transitions are the major intervals of enhanced landsliding, but the length of this interval varies between distinct types of landscapes.Future progress in the understanding of the relationships between landslides and Quaternary climate changes should benefit from the i) extension of datasets of dated landslides, ii) geographical expansion of dating studies to regions with a lack of chronologically determined landslides (e.g., tropics), iii) improvement of landslide-dating strategies involving the incorporation of independent palaeoclimatic proxies and iv) wider incorporation of numerical modeling within landslide-dating studies.
Czech name
—
Czech description
—

Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10508 - Physical geography

Project
<a href="/en/project/GA17-17712S" target="_blank" >GA17-17712S: Sackung in non-glaciated landscapes: spatial and temporal behavior of deep-seated gravitational slope deformations in Outer Western Carpathians</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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