Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden

Abstract The occurrence of turf‐banked solifluction landforms in the Abisko region was analysed using a grid‐based approach and statistical modelling through logistic regression. Significant parameters in the model were the vegetation index NDVI, annual incoming potential radiation, wetness index, s...

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Published in:Permafrost and Periglacial Processes
Main Authors: Ridefelt, Hanna, Etzelmüller, Bernd, Boelhouwers, Jan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2010
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.681
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spelling crwiley:10.1002/ppp.681 2024-10-06T13:41:33+00:00 Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden Ridefelt, Hanna Etzelmüller, Bernd Boelhouwers, Jan 2010 http://dx.doi.org/10.1002/ppp.681 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.681 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.681 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 21, issue 3, page 241-255 ISSN 1045-6740 1099-1530 journal-article 2010 crwiley https://doi.org/10.1002/ppp.681 2024-09-11T04:15:17Z Abstract The occurrence of turf‐banked solifluction landforms in the Abisko region was analysed using a grid‐based approach and statistical modelling through logistic regression. Significant parameters in the model were the vegetation index NDVI, annual incoming potential radiation, wetness index, slope gradient and elevation. The model had an acceptable discrimination capacity and rather low model‐fit values, but clearly showed the importance of vegetation patterns for the occurrence of solifluction at a regional scale. Solifluction movement rates measured at eight sites were combined with model parameters and the annual duration of sun hours to regionalise solifluction movement rates through an unsupervised terrain classification. For comparison, the linear relationship between the probability of solifluction occurrence and variations in movement rates was also used to regionalise movement rates. Potential geomorphic work was calculated for six different areas within the region, with the greatest being for Kärkevagge, the area with the highest precipitation. The combination of a logistic regression model of mapped landforms and field measurements of solifluction rates represents a promising methodology to assess the occurrence and activity of the process at a regional scale. Copyright © 2010 John Wiley & Sons, Ltd. Article in Journal/Newspaper Abisko Northern Sweden Permafrost and Periglacial Processes Wiley Online Library Abisko ENVELOPE(18.829,18.829,68.349,68.349) Kärkevagge ENVELOPE(18.310,18.310,68.402,68.402) Permafrost and Periglacial Processes 21 3 241 255
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The occurrence of turf‐banked solifluction landforms in the Abisko region was analysed using a grid‐based approach and statistical modelling through logistic regression. Significant parameters in the model were the vegetation index NDVI, annual incoming potential radiation, wetness index, slope gradient and elevation. The model had an acceptable discrimination capacity and rather low model‐fit values, but clearly showed the importance of vegetation patterns for the occurrence of solifluction at a regional scale. Solifluction movement rates measured at eight sites were combined with model parameters and the annual duration of sun hours to regionalise solifluction movement rates through an unsupervised terrain classification. For comparison, the linear relationship between the probability of solifluction occurrence and variations in movement rates was also used to regionalise movement rates. Potential geomorphic work was calculated for six different areas within the region, with the greatest being for Kärkevagge, the area with the highest precipitation. The combination of a logistic regression model of mapped landforms and field measurements of solifluction rates represents a promising methodology to assess the occurrence and activity of the process at a regional scale. Copyright © 2010 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Ridefelt, Hanna
Etzelmüller, Bernd
Boelhouwers, Jan
spellingShingle Ridefelt, Hanna
Etzelmüller, Bernd
Boelhouwers, Jan
Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
author_facet Ridefelt, Hanna
Etzelmüller, Bernd
Boelhouwers, Jan
author_sort Ridefelt, Hanna
title Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
title_short Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
title_full Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
title_fullStr Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
title_full_unstemmed Spatial analysis of solifluction landforms and process rates in the Abisko Mountains, northern Sweden
title_sort spatial analysis of solifluction landforms and process rates in the abisko mountains, northern sweden
publisher Wiley
publishDate 2010
url http://dx.doi.org/10.1002/ppp.681
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.681
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.681
long_lat ENVELOPE(18.829,18.829,68.349,68.349)
ENVELOPE(18.310,18.310,68.402,68.402)
geographic Abisko
Kärkevagge
geographic_facet Abisko
Kärkevagge
genre Abisko
Northern Sweden
Permafrost and Periglacial Processes
genre_facet Abisko
Northern Sweden
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 21, issue 3, page 241-255
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.681
container_title Permafrost and Periglacial Processes
container_volume 21
container_issue 3
container_start_page 241
op_container_end_page 255
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