Distribution and morphometric characteristics of icing fields in Svalbard

Icing fields are common in Svalbard and very diverse with respect to shape. The occurrence and spatial structure of icing fields in front of glaciers were analysed using aerial photographs (at a scale of 1:50000) taken from 19 July to 25 August 1990–a unique set of images covering the whole archipel...

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Published in:Polar Research
Main Authors: Bukowska-Jania, Elzbieta, Szafraniec, Joanna
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2005
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2059
https://doi.org/10.3402/polar.v24i1.6252
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spelling ftjpolarres:oai:journals.openacademia.net:article/2059 2024-09-15T18:31:21+00:00 Distribution and morphometric characteristics of icing fields in Svalbard Bukowska-Jania, Elzbieta Szafraniec, Joanna 2005-07-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2059 https://doi.org/10.3402/polar.v24i1.6252 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2059/5310 https://polarresearch.net/index.php/polar/article/view/2059 doi:10.3402/polar.v24i1.6252 Polar Research; Vol 24, No 1-2 (2005); 41-53 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2005 ftjpolarres https://doi.org/10.3402/polar.v24i1.6252 2024-06-28T03:10:15Z Icing fields are common in Svalbard and very diverse with respect to shape. The occurrence and spatial structure of icing fields in front of glaciers were analysed using aerial photographs (at a scale of 1:50000) taken from 19 July to 25 August 1990–a unique set of images covering the whole archipelago in one summer season. Icing fields were observed in front of 217 glaciers. A total area of 12.3 km2 appeared to be covered by the icings. This value, from late in the ablation season, is likely to be near the seasonal minimum. Of the 217 glaciers, 192 were selected for further analysis, carried out by stereoscopic observation of the aerial photographs. Striking difference in brightness of the icing fields in comparison to the surrounded terrain combined with field experience of the geomorphic setting of its occurrence made possible the complete inventory of the icing phenomena for the whole of Svalbard. Morphometric features were measured directly on photographs and on scanned portions of them. Results from field studies of melting and the decrease of the area of icing fields at the front of two glaciers are also presented. The shape and distribution of icings depend on a set of glaciological factors and on the glacial and geomorphologic setting. The duration of frigid temperatures in the winter when the icing fields were formed is also important. Results show that oval and circular shapes are characteristic for icing fields after surviving the ablation season. These fields have an important geomorphological influence on the outwash plains that currently develop in Svalbard. Article in Journal/Newspaper Polar Research Svalbard Polar Research Polar Research 24 1-2 41 53
institution Open Polar
collection Polar Research
op_collection_id ftjpolarres
language English
description Icing fields are common in Svalbard and very diverse with respect to shape. The occurrence and spatial structure of icing fields in front of glaciers were analysed using aerial photographs (at a scale of 1:50000) taken from 19 July to 25 August 1990–a unique set of images covering the whole archipelago in one summer season. Icing fields were observed in front of 217 glaciers. A total area of 12.3 km2 appeared to be covered by the icings. This value, from late in the ablation season, is likely to be near the seasonal minimum. Of the 217 glaciers, 192 were selected for further analysis, carried out by stereoscopic observation of the aerial photographs. Striking difference in brightness of the icing fields in comparison to the surrounded terrain combined with field experience of the geomorphic setting of its occurrence made possible the complete inventory of the icing phenomena for the whole of Svalbard. Morphometric features were measured directly on photographs and on scanned portions of them. Results from field studies of melting and the decrease of the area of icing fields at the front of two glaciers are also presented. The shape and distribution of icings depend on a set of glaciological factors and on the glacial and geomorphologic setting. The duration of frigid temperatures in the winter when the icing fields were formed is also important. Results show that oval and circular shapes are characteristic for icing fields after surviving the ablation season. These fields have an important geomorphological influence on the outwash plains that currently develop in Svalbard.
format Article in Journal/Newspaper
author Bukowska-Jania, Elzbieta
Szafraniec, Joanna
spellingShingle Bukowska-Jania, Elzbieta
Szafraniec, Joanna
Distribution and morphometric characteristics of icing fields in Svalbard
author_facet Bukowska-Jania, Elzbieta
Szafraniec, Joanna
author_sort Bukowska-Jania, Elzbieta
title Distribution and morphometric characteristics of icing fields in Svalbard
title_short Distribution and morphometric characteristics of icing fields in Svalbard
title_full Distribution and morphometric characteristics of icing fields in Svalbard
title_fullStr Distribution and morphometric characteristics of icing fields in Svalbard
title_full_unstemmed Distribution and morphometric characteristics of icing fields in Svalbard
title_sort distribution and morphometric characteristics of icing fields in svalbard
publisher Norwegian Polar Institute
publishDate 2005
url https://polarresearch.net/index.php/polar/article/view/2059
https://doi.org/10.3402/polar.v24i1.6252
genre Polar Research
Svalbard
genre_facet Polar Research
Svalbard
op_source Polar Research; Vol 24, No 1-2 (2005); 41-53
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2059/5310
https://polarresearch.net/index.php/polar/article/view/2059
doi:10.3402/polar.v24i1.6252
op_doi https://doi.org/10.3402/polar.v24i1.6252
container_title Polar Research
container_volume 24
container_issue 1-2
container_start_page 41
op_container_end_page 53
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