Diversification of landslide areas as a means for reducing noise in dendrogeomorphic dating

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F22%3AN2302FM4" target="_blank" >RIV/61988987:17310/22:N2302FM4 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61988987:17310/22:A2302FM4

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S1871101422001108" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1871101422001108</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quageo.2022.101362" target="_blank" >10.1016/j.quageo.2022.101362</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Diversification of landslide areas as a means for reducing noise in dendrogeomorphic dating

Popis výsledku v původním jazyce

The result of tree-ring-based reconstruction of past landslide events is often the development of a single total chronology. This approach can be very effective for small homogeneous landslides. However, compiling chronological data from heterogeneous (often independent) zones of large complex landslide areas into one chronology can induce over- or underestimation of some events, resulting in lowered reliability of the reconstruction. The solution for elimination of this effect can lie in the diversification of complex landslide areas into homogeneous zones with separate analyses. The aim of this study was to quantify the effect of this separation on detected slope movement events and to define parameters whose investigation could distinguish events (sliding) from noise (creeping).

Název v anglickém jazyce

Diversification of landslide areas as a means for reducing noise in dendrogeomorphic dating

Popis výsledku anglicky

The result of tree-ring-based reconstruction of past landslide events is often the development of a single total chronology. This approach can be very effective for small homogeneous landslides. However, compiling chronological data from heterogeneous (often independent) zones of large complex landslide areas into one chronology can induce over- or underestimation of some events, resulting in lowered reliability of the reconstruction. The solution for elimination of this effect can lie in the diversification of complex landslide areas into homogeneous zones with separate analyses. The aim of this study was to quantify the effect of this separation on detected slope movement events and to define parameters whose investigation could distinguish events (sliding) from noise (creeping).

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

<a href="/cs/project/GA19-01866S" target="_blank" >GA19-01866S: Staré sesuvy: skutečně neaktivní?</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2022

Kód důvěrnosti údajů

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

Název periodika

QUAT GEOCHRONOL

ISSN

1871-1014

e-ISSN

—

Svazek periodika

—

Číslo periodika v rámci svazku

srpen

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

10

Strana od-do

—

Kód UT WoS článku

000818003100003

EID výsledku v databázi Scopus

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