Detailed Information on Publication Record
2023
The longest tree-ring based chronology of mass movements in Central Europe and their meteorological triggers
ŠILHÁN, Karel, Rudolf BRÁZDIL, Pavel ZAHRADNÍČEK and Tomáš PÁNEKBasic information
Original name
The longest tree-ring based chronology of mass movements in Central Europe and their meteorological triggers
Authors
ŠILHÁN, Karel (guarantor), Rudolf BRÁZDIL (203 Czech Republic, belonging to the institution), Pavel ZAHRADNÍČEK and Tomáš PÁNEK
Edition
Catena, Elsevier, 2023, 0341-8162
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 6.200 in 2022
RIV identification code
RIV/00216224:14310/23:00130603
Organization unit
Faculty of Science
UT WoS
000976659100001
Keywords in English
Dendrogeomorphology; Landslide; Long chronology; Meteorological triggers
Tags
Tags
International impact, Reviewed
Změněno: 2/6/2023 13:41, Mgr. Marie Šípková, DiS.
Abstract
V originále
Knowledge of meteorological triggers of mass movements is crucial for determining the degree of hazards, but also for predicting their occurrence. Dendrogeomorphic methods (tree-ring based) have repeatedly provided data on historical landslide activity as a basis for detailed trigger analysis. However, the construction of long dendrogeomorphic chronologies encounters limits in the sensitivity of growth disturbances in trees as well as their age dependence. Moreover, accurate meteorological instrumental data usually do not cover the entire length of long tree-ring based chronologies of landslide movements. To resolve these uncertainties, this study has compiled the longest tree-ring-based chronology of mass movements in Central Europe for Mt. Kněhyně in Outer Western Carpathians, spanning more than a quarter of a millennium and based on 228 tree-ring series of disturbed individuals of Norway spruce (Picea abies (L.) Karst.). The resulting chronology is a combination of two sub-chronologies that we constructed from different tree growth disturbances (reaction wood and tree-ring eccentricity), combining the advantages of both approaches. To identify potential meteorological triggers, we combined instrumental data from the nearest meteorological station together with reconstructed data from the wider landslide study area and documentary records. This gave us a uniquely long overlap of the two datasets across the full length of the mass movement chronology, allowing for more robust results compared to significantly shorter overlays. The studied mass movements followed up to three years of above-mean precipitation and were immediately triggered by short (several days) precipitation extremes. Snowmelt lasting several days to weeks in selected cases further modified this pattern.