Frequency, predisposition, and triggers of floods in flysch Carpathians: regional study using dendrogeomorphic methods

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F15%3AA1501DM5" target="_blank" >RIV/61988987:17310/15:A1501DM5 - 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

Frequency, predisposition, and triggers of floods in flysch Carpathians: regional study using dendrogeomorphic methods

Popis výsledku v původním jazyce

Dangerous overland flood events in the foothills of the flysch Carpathians often result from a cumulative effect of floods in high-gradient channels. Detailed understanding of the origin of floods in these catchments is only possible if the occurrence ofthese floods in the past has thoroughly been studied. Yet, no gauging stations can be found in the local catchments. The reconstruction of floods in ungauged catchments has so far been performed using dendrogeomorphicmethods. Stems or branches floatingin the floodwater can affect stemsor roots of living trees and injure them. Trees are able to record these signals in their tree-ring series. Within the flysch Carpathians, the floods have been reconstructed based on the analysis of 446 cross sections from scarred tree roots and 192 increment cores fromthe stems of affected trees in the studied area of 10 catchments surrounding the highest peak of theMoravskoslezské Beskydy Mts, the Lysá hora Mt.

Název v anglickém jazyce

Frequency, predisposition, and triggers of floods in flysch Carpathians: regional study using dendrogeomorphic methods

Popis výsledku anglicky

Dangerous overland flood events in the foothills of the flysch Carpathians often result from a cumulative effect of floods in high-gradient channels. Detailed understanding of the origin of floods in these catchments is only possible if the occurrence ofthese floods in the past has thoroughly been studied. Yet, no gauging stations can be found in the local catchments. The reconstruction of floods in ungauged catchments has so far been performed using dendrogeomorphicmethods. Stems or branches floatingin the floodwater can affect stemsor roots of living trees and injure them. Trees are able to record these signals in their tree-ring series. Within the flysch Carpathians, the floods have been reconstructed based on the analysis of 446 cross sections from scarred tree roots and 192 increment cores fromthe stems of affected trees in the studied area of 10 catchments surrounding the highest peak of theMoravskoslezské Beskydy Mts, the Lysá hora Mt.

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

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

GEOMORPHOLOGY

ISSN

0169-555X

e-ISSN

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Svazek periodika

234

Číslo periodika v rámci svazku

jaro

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

11

Strana od-do

243-253

Kód UT WoS článku

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EID výsledku v databázi Scopus

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