Detection of crevassed areas with minimum geometric information: Vernagtferner case study

Crevasses pose severe risks for mountaineers and field glaciologists. Smaller cracks between 0.5 and 2 m are still dangerous, but often not visible in medium resolution satellite imagery. If they are snow covered, they are completely undetectable by optical sensors. We set out to develop an approach...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Theresa Dobler, Wilfried Hagg, Christoph Mayer
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2023.12
https://doaj.org/article/a6520999c9274cfcbb26563177d969b6
id ftdoajarticles:oai:doaj.org/article:a6520999c9274cfcbb26563177d969b6
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:a6520999c9274cfcbb26563177d969b6 2023-11-12T04:19:55+01:00 Detection of crevassed areas with minimum geometric information: Vernagtferner case study Theresa Dobler Wilfried Hagg Christoph Mayer 2023-10-01T00:00:00Z https://doi.org/10.1017/jog.2023.12 https://doaj.org/article/a6520999c9274cfcbb26563177d969b6 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143023000126/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2023.12 0022-1430 1727-5652 https://doaj.org/article/a6520999c9274cfcbb26563177d969b6 Journal of Glaciology, Vol 69, Pp 1214-1224 (2023) Applied glaciology crevasses glacier hazards Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2023.12 2023-10-29T00:40:50Z Crevasses pose severe risks for mountaineers and field glaciologists. Smaller cracks between 0.5 and 2 m are still dangerous, but often not visible in medium resolution satellite imagery. If they are snow covered, they are completely undetectable by optical sensors. We set out to develop an approach to detect potentially crevassed areas by a minimum of geometric data, and to make the method generally applicable to glacier regions. On Vernagtferner, we compared a reference dataset of crevasses observed in high-resolution optical imagery with the curvature of the ice surface and the spatial gradients in driving stress. Both parameters can be derived from a digital surface model and a bedrock model, derived from ice thickness measurements. The correlation patterns show that crevasses preferably form in convex areas and in areas where the driving stress rapidly increases. This corresponds with the theory of crevasse formation. Although the method still misclassifies larger parts, the approach has the potential to define probable non-crevassed areas as well as to aid the planning of safe routes. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 11
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Applied glaciology
crevasses
glacier hazards
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Applied glaciology
crevasses
glacier hazards
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Theresa Dobler
Wilfried Hagg
Christoph Mayer
Detection of crevassed areas with minimum geometric information: Vernagtferner case study
topic_facet Applied glaciology
crevasses
glacier hazards
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Crevasses pose severe risks for mountaineers and field glaciologists. Smaller cracks between 0.5 and 2 m are still dangerous, but often not visible in medium resolution satellite imagery. If they are snow covered, they are completely undetectable by optical sensors. We set out to develop an approach to detect potentially crevassed areas by a minimum of geometric data, and to make the method generally applicable to glacier regions. On Vernagtferner, we compared a reference dataset of crevasses observed in high-resolution optical imagery with the curvature of the ice surface and the spatial gradients in driving stress. Both parameters can be derived from a digital surface model and a bedrock model, derived from ice thickness measurements. The correlation patterns show that crevasses preferably form in convex areas and in areas where the driving stress rapidly increases. This corresponds with the theory of crevasse formation. Although the method still misclassifies larger parts, the approach has the potential to define probable non-crevassed areas as well as to aid the planning of safe routes.
format Article in Journal/Newspaper
author Theresa Dobler
Wilfried Hagg
Christoph Mayer
author_facet Theresa Dobler
Wilfried Hagg
Christoph Mayer
author_sort Theresa Dobler
title Detection of crevassed areas with minimum geometric information: Vernagtferner case study
title_short Detection of crevassed areas with minimum geometric information: Vernagtferner case study
title_full Detection of crevassed areas with minimum geometric information: Vernagtferner case study
title_fullStr Detection of crevassed areas with minimum geometric information: Vernagtferner case study
title_full_unstemmed Detection of crevassed areas with minimum geometric information: Vernagtferner case study
title_sort detection of crevassed areas with minimum geometric information: vernagtferner case study
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2023.12
https://doaj.org/article/a6520999c9274cfcbb26563177d969b6
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 1214-1224 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143023000126/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2023.12
0022-1430
1727-5652
https://doaj.org/article/a6520999c9274cfcbb26563177d969b6
op_doi https://doi.org/10.1017/jog.2023.12
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 11
_version_ 1782336145758093312