Recent increase in debris flow activity in the Tatras Mountains: results of a regional dendrogeomorphic reconstruction

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F16%3AA1701GQJ" target="_blank" >RIV/61988987:17310/16:A1701GQJ - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Recent increase in debris flow activity in the Tatras Mountains: results of a regional dendrogeomorphic reconstruction

Popis výsledku v původním jazyce

Debris flows are very frequent geomorphic agents that form relief of the High Tatras Mountains, which are the highest mountain range in the Carpathian arc. The knowledge of their history is based on lichenometric dating, historical orthophotos and incomplete archival records. Nevertheless, complete chronologies of debris flows at an annual resolution for the High Tatras Mountains have not yet been reconstructed. In this paper, we present results of dendrogeomorphic research in the southern region of the mountains (the Great Cold Valley and Small Cold Valley). The research was undertaken to reconstruct regional year-to-year chronologies of debris flows, which would present unique perspectives on the debris flow activity. A total of 474 scars on the stems and branches of 414 P. mugo were dated with a seasonal precision (the best tool for distinguishing debris flow scars from snow avalanche scars) in 12 debris flow tracks.

Název v anglickém jazyce

Recent increase in debris flow activity in the Tatras Mountains: results of a regional dendrogeomorphic reconstruction

Popis výsledku anglicky

Debris flows are very frequent geomorphic agents that form relief of the High Tatras Mountains, which are the highest mountain range in the Carpathian arc. The knowledge of their history is based on lichenometric dating, historical orthophotos and incomplete archival records. Nevertheless, complete chronologies of debris flows at an annual resolution for the High Tatras Mountains have not yet been reconstructed. In this paper, we present results of dendrogeomorphic research in the southern region of the mountains (the Great Cold Valley and Small Cold Valley). The research was undertaken to reconstruct regional year-to-year chronologies of debris flows, which would present unique perspectives on the debris flow activity. A total of 474 scars on the stems and branches of 414 P. mugo were dated with a seasonal precision (the best tool for distinguishing debris flow scars from snow avalanche scars) in 12 debris flow tracks.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/GA13-15123S" target="_blank" >GA13-15123S: Časoprostorová variabilita hlubokých svahových deformací v Tatrách (Západní Karpaty)</a><br>

Návaznosti

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

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název periodika

CATENA

ISSN

0341-8162

e-ISSN

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Svazek periodika

143

Číslo periodika v rámci svazku

srpen

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

221-231

Kód UT WoS článku

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EID výsledku v databázi Scopus

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