Landslides and Quaternary climate changes—The state of the art

Kód výsledku v 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>

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

Landslides and Quaternary climate changes—The state of the art

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

Landslides and Quaternary climate changes—The state of the art

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

<a href="/cs/project/GA17-17712S" target="_blank" >GA17-17712S: Sackung v nezaledněných pohořích: prostorové a chronologické chování hlubokých svahových deformací ve Vnějších Západních Karpatech</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2019

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Earth-Science Reviews

ISSN

0012-8252

e-ISSN

—

Svazek periodika

196

Číslo periodika v rámci svazku

September

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

22

Strana od-do

1-22

Kód UT WoS článku

000482246200006

EID výsledku v databázi Scopus

2-s2.0-85067193356