Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images

The dynamics of seasonal snow ablation on six glaciers in central Spitsbergen (Dicksonland) were assessed by examining a set of Sentinel-2 satellite images covering the summer ablation season for the period 2016–19. All glaciers lost 80% or more of their surface snow cover during the studied ablatio...

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Published in:Journal of Glaciology
Main Authors: Jan Kavan, Vincent Haagmans
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
Subjects:
Online Access:https://doi.org/10.1017/jog.2021.36
https://doaj.org/article/27fc0a10ca1942d0922070204884cdd4
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spelling ftdoajarticles:oai:doaj.org/article:27fc0a10ca1942d0922070204884cdd4 2023-05-15T16:57:32+02:00 Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images Jan Kavan Vincent Haagmans 2021-10-01T00:00:00Z https://doi.org/10.1017/jog.2021.36 https://doaj.org/article/27fc0a10ca1942d0922070204884cdd4 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021000368/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.36 0022-1430 1727-5652 https://doaj.org/article/27fc0a10ca1942d0922070204884cdd4 Journal of Glaciology, Vol 67, Pp 961-966 (2021) Glacier ablation phenomena glacier mass balance snow wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2021.36 2023-03-12T01:30:57Z The dynamics of seasonal snow ablation on six glaciers in central Spitsbergen (Dicksonland) were assessed by examining a set of Sentinel-2 satellite images covering the summer ablation season for the period 2016–19. All glaciers lost 80% or more of their surface snow cover during the studied ablation seasons. This bolsters the recently observed trend of local glacier thinning, even at higher altitudes. Snow ablation dynamics are highly dependent on the glaciers altitudes, their position relative to the prevailing wind direction and the exposure to insolation. The accumulation areas of the studied glaciers were delimited based on the overlap of the minimum extent of snow-covered areas in the four consecutive studied summer seasons. The high temporal and spatial resolutions of available images enabled a detailed description of the seasonal snow ablation dynamics. Moreover, an estimate of the average number of days with below threshold glacier snow cover was made. This study contributes to our understanding of recent processes and might further support the modelling of glacier melt and subsequent runoff. Article in Journal/Newspaper Journal of Glaciology Spitsbergen Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 67 265 961 966
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier ablation phenomena
glacier mass balance
snow
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier ablation phenomena
glacier mass balance
snow
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Jan Kavan
Vincent Haagmans
Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
topic_facet Glacier ablation phenomena
glacier mass balance
snow
wind-blown snow
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description The dynamics of seasonal snow ablation on six glaciers in central Spitsbergen (Dicksonland) were assessed by examining a set of Sentinel-2 satellite images covering the summer ablation season for the period 2016–19. All glaciers lost 80% or more of their surface snow cover during the studied ablation seasons. This bolsters the recently observed trend of local glacier thinning, even at higher altitudes. Snow ablation dynamics are highly dependent on the glaciers altitudes, their position relative to the prevailing wind direction and the exposure to insolation. The accumulation areas of the studied glaciers were delimited based on the overlap of the minimum extent of snow-covered areas in the four consecutive studied summer seasons. The high temporal and spatial resolutions of available images enabled a detailed description of the seasonal snow ablation dynamics. Moreover, an estimate of the average number of days with below threshold glacier snow cover was made. This study contributes to our understanding of recent processes and might further support the modelling of glacier melt and subsequent runoff.
format Article in Journal/Newspaper
author Jan Kavan
Vincent Haagmans
author_facet Jan Kavan
Vincent Haagmans
author_sort Jan Kavan
title Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
title_short Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
title_full Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
title_fullStr Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
title_full_unstemmed Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
title_sort seasonal dynamics of snow ablation on selected glaciers in central spitsbergen derived from sentinel-2 satellite images
publisher Cambridge University Press
publishDate 2021
url https://doi.org/10.1017/jog.2021.36
https://doaj.org/article/27fc0a10ca1942d0922070204884cdd4
genre Journal of Glaciology
Spitsbergen
genre_facet Journal of Glaciology
Spitsbergen
op_source Journal of Glaciology, Vol 67, Pp 961-966 (2021)
op_relation https://www.cambridge.org/core/product/identifier/S0022143021000368/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2021.36
0022-1430
1727-5652
https://doaj.org/article/27fc0a10ca1942d0922070204884cdd4
op_doi https://doi.org/10.1017/jog.2021.36
container_title Journal of Glaciology
container_volume 67
container_issue 265
container_start_page 961
op_container_end_page 966
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