Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada

Abstract Using historical and recent aerial photography and structure from motion (SfM) multiview stereo (MVS) techniques, we reconstruct the 1959 and 2018 ice surface topography and determine the geodetic mass balance of Bowman Glacier, a small mountain glacier on northern Ellesmere Island. This is...

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Published in:Journal of Glaciology
Main Authors: Medrzycka, Dorota, Copland, Luke, Noël, Brice
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.119
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001198
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spelling crcambridgeupr:10.1017/jog.2022.119 2024-03-03T08:41:42+00:00 Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada Medrzycka, Dorota Copland, Luke Noël, Brice 2023 http://dx.doi.org/10.1017/jog.2022.119 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001198 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 276, page 997-1010 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2022.119 2024-02-08T08:44:16Z Abstract Using historical and recent aerial photography and structure from motion (SfM) multiview stereo (MVS) techniques, we reconstruct the 1959 and 2018 ice surface topography and determine the geodetic mass balance of Bowman Glacier, a small mountain glacier on northern Ellesmere Island. This is combined with optical satellite imagery to reconstruct the evolution in extent of the glacier over six decades, and ground-penetrating radar measurements of ice thickness to estimate the remaining ice volume. Between 1959 and 2020, Bowman Glacier lost 78% of its extent (reducing from 2.75 to 0.61 km 2 ), while average annual area loss rates have nearly tripled in the past two decades. Over the 1959–2018 period, glacier-wide ice-thickness change averaged −22.7 ± 4.7 m, corresponding to a mean specific annual mass balance of −347.0 ± 71.4 mm w.e. a −1 . Projecting rates of area and volume change into the future indicates that the glacier will likely entirely disappear between 2030 and 2060. This study demonstrates the potential of SfM-MVS processing to generate elevation products from 1950/60s historical aerial photographs, and to extend observations of ice elevation and glacier volume change for the Canadian Arctic, prior to the satellite record. Article in Journal/Newspaper Arctic Ellesmere Island glacier* Journal of Glaciology Cambridge University Press Arctic Ellesmere Island Canada Bowman Glacier ENVELOPE(-162.000,-162.000,-85.567,-85.567) Journal of Glaciology 1 14
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Medrzycka, Dorota
Copland, Luke
Noël, Brice
Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
topic_facet Earth-Surface Processes
description Abstract Using historical and recent aerial photography and structure from motion (SfM) multiview stereo (MVS) techniques, we reconstruct the 1959 and 2018 ice surface topography and determine the geodetic mass balance of Bowman Glacier, a small mountain glacier on northern Ellesmere Island. This is combined with optical satellite imagery to reconstruct the evolution in extent of the glacier over six decades, and ground-penetrating radar measurements of ice thickness to estimate the remaining ice volume. Between 1959 and 2020, Bowman Glacier lost 78% of its extent (reducing from 2.75 to 0.61 km 2 ), while average annual area loss rates have nearly tripled in the past two decades. Over the 1959–2018 period, glacier-wide ice-thickness change averaged −22.7 ± 4.7 m, corresponding to a mean specific annual mass balance of −347.0 ± 71.4 mm w.e. a −1 . Projecting rates of area and volume change into the future indicates that the glacier will likely entirely disappear between 2030 and 2060. This study demonstrates the potential of SfM-MVS processing to generate elevation products from 1950/60s historical aerial photographs, and to extend observations of ice elevation and glacier volume change for the Canadian Arctic, prior to the satellite record.
format Article in Journal/Newspaper
author Medrzycka, Dorota
Copland, Luke
Noël, Brice
author_facet Medrzycka, Dorota
Copland, Luke
Noël, Brice
author_sort Medrzycka, Dorota
title Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
title_short Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
title_full Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
title_fullStr Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
title_full_unstemmed Rapid demise and committed loss of Bowman Glacier, northern Ellesmere Island, Arctic Canada
title_sort rapid demise and committed loss of bowman glacier, northern ellesmere island, arctic canada
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2022.119
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001198
long_lat ENVELOPE(-162.000,-162.000,-85.567,-85.567)
geographic Arctic
Ellesmere Island
Canada
Bowman Glacier
geographic_facet Arctic
Ellesmere Island
Canada
Bowman Glacier
genre Arctic
Ellesmere Island
glacier*
Journal of Glaciology
genre_facet Arctic
Ellesmere Island
glacier*
Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 276, page 997-1010
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.119
container_title Journal of Glaciology
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