Evaluation of meteorological controls of reconstructed rockfall activity in the Czech Flysch Carpathians
Article first published online: 19 AUG 2011
Copyright © 2011 John Wiley & Sons, Ltd.
Earth Surface Processes and Landforms
Volume 36, Issue 14, pages 1898–1909, November 2011
How to Cite
Šilhán, K., Brázdil, R., Pánek, T., Dobrovolný, P., Kašičková, L., Tolasz, R., Turský, O. and Václavek, M. (2011), Evaluation of meteorological controls of reconstructed rockfall activity in the Czech Flysch Carpathians. Earth Surf. Process. Landforms, 36: 1898–1909. doi: 10.1002/esp.2211
- Issue published online: 21 OCT 2011
- Article first published online: 19 AUG 2011
- Accepted manuscript online: 15 JUL 2011 08:37AM EST
- Manuscript Accepted: 5 JUL 2011
- Manuscript Revised: 27 JUN 2011
- Manuscript Received: 27 OCT 2010
- Czech Science Foundation. Grant Number: P209/10/0309
- Czech Flysch Carpathians
Rockfall is an important process in the final sculpturing of escarpments and scree slopes that originate in bedrock landslides in the Flysch Carpathians. The spatio-temporal characteristics of rockfall activity were studied at four localities representative of old landslides in the highest part of the Czech Flysch Carpathians (Moravskoslezské Beskydy Mountains). Historical activity, chronology, and spatial context of rockfall activity were reconstructed using dendrogeomorphic techniques and rockfall rate index (RR). A total of 1132 increment cores from 283 trees growing in the rockfall transport and accumulation zones enabled the dating of 989 rockfall events. Reconstruction of a 78-year-long RR chronology suggests similar rockfall histories and trends at all study sites, indicating the existence of major common factors driving rockfall dynamics in the region. Temporal analysis and correlation of the RR series obtained with monthly mean temperatures, numbers of days with temperature transitions through 0 °C and monthly precipitation totals show that meteorological characteristics have evident but variable influence on rockfall activity. The most important factor is the effect of freeze–thaw cycles throughout the year, supplemented by low temperatures, especially during autumn. The influence of precipitation totals is of lesser importance. Copyright © 2011 John Wiley & Sons, Ltd.