Münchow, J.; Brenning, A. & Richter, M. (2012): <b>Geomorphic process rates of landslides along a humidity gradient in the tropical Andes</b>. <i>Geomorphology</i> <b>139-140</b>, 271-284.
Resource Description
Title:
Geomorphic process rates of landslides along a humidity gradient in the tropical Andes
Short Name:
landslide gradient
FOR816dw ID:
1074
Publication Date:
2012-02-01
License and Usage Rights:
Resource Owner(s):
Individual:
Jannes Münchow
Contact:
email:
malnamalja <at> gmx.de
91054 Erlangen
Deutschland
Individual:
Allexander Brenning
Contact:
email:
webmaster <at> tropicalmountainforest.com
Individual:
Michael Richter
Contact:
email:
sairecabur <at> web.de
University Erlangen
Institute for Geography FAU
Kochstr. 4/4
91054 Erlangen
Germany
Abstract:
Areas with high landslide activity and diversity were encountered in the tropical Andes of Southern Ecuador under contrasting, semi-arid to perhumid climatic conditions. The objective of this study was to determine and compare geomorphic process rates of shallow landslides along this remarkable humidity gradient and subject to different types of human-made and natural environmental changes. Geomorphic work, geomorphic power and landslide mobilization rate (LMR) were therefore calculated for shallow landslides in two study areas with two separate geological or land use-related subareas each. While landslide ages were known in the perhumid Reserva Biológica San Francisco (RBSF) area, only an approximation of the frequency of critical landslide-triggering rainfall events was available for the semi-arid Masamanaca area. Landslide volumes were estimated by volume–area scaling. Generalized additive models (GAMs) were used as landslide susceptibility models in order to analyze the relative importance of topography, and to downscale LMR values to a fine spatial resolution. LMR in the perhumid RBSF area ranged from ˜2 mm yr-1 in the natural part of this area with tropical mountain rainforests to ˜5 mmyr-1 in the human-influenced part. The semi-arid Masamanaca area, though subject to greater estimation uncertainties, displayed LMR on the order of ˜0.4 to 4 mm yr-1 for shallow landslides. The results provide a basis for the spatially differentiated assessment of landscape evolution and degradation in an area with a close relation between landslide activity, natural vegetation succession and human land use.
Keywords:
| mass movements | denudation rate | geomorphic work | generalized additive model |
