Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021

Abstract The paper describes the transformation of the coastal landscape near former Davislaguna Lake, SE Spitsbergen. It is a comparative study which outlines the changing state of the area based on old maps, other archival materials, remote sensing data from the years 1900 to 2021, and our own fie...

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Published in:Land Degradation & Development
Main Authors: Ziaja, Wieslaw, Ostafin, Krzysztof, Maciejowski, Wojciech, Kruse, Frigga
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Ice
Online Access:http://dx.doi.org/10.1002/ldr.4765
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.4765
id crwiley:10.1002/ldr.4765
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spelling crwiley:10.1002/ldr.4765 2024-06-23T07:53:05+00:00 Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021 Ziaja, Wieslaw Ostafin, Krzysztof Maciejowski, Wojciech Kruse, Frigga 2023 http://dx.doi.org/10.1002/ldr.4765 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.4765 en eng Wiley http://creativecommons.org/licenses/by-nc-nd/4.0/ Land Degradation & Development volume 34, issue 16, page 4823-4832 ISSN 1085-3278 1099-145X journal-article 2023 crwiley https://doi.org/10.1002/ldr.4765 2024-06-06T04:21:53Z Abstract The paper describes the transformation of the coastal landscape near former Davislaguna Lake, SE Spitsbergen. It is a comparative study which outlines the changing state of the area based on old maps, other archival materials, remote sensing data from the years 1900 to 2021, and our own fieldwork performed since 2005. The indirect cause of this transformation is identified herein as climate warming which has produced a progressive degradation of the cryosphere and triggered three key forces behind the said transformation: glacial recession in the 20th century, shortening of the sea‐ice season, permafrost thawing in the 21st century. From the year 1900 to the 1920s the coastal landscape of the study area consisted of a bay with beaches between a mountain range in the west and a tidewater glacier tongue protruding into the sea in the northeast. The tongue subsequently melted and the bay became transformed into a coastal plain, with the resulting lake becoming separated from the sea by a gravel‐sand bar by 1936. Afterwards, both the plain and lake dwindled in size due to the decline of the bar found to the west. This process continued until the lake became divided into two parts in the 1980s; one of these then disappeared between 2006 and 2010, and the second one by 2021. Hence, the land in question, with the coastal plain partly glaciated and surrounding the bay, then unglaciated and surrounding the lake, became over time replaced by the sea. Today, the process of abrasion acting near the sea is destroying the remaining beaches and cutting down the steep slopes of area mountains and ice‐cored moraines. Article in Journal/Newspaper glacier Ice permafrost Sea ice Svalbard Tidewater Spitsbergen Wiley Online Library Davislaguna ENVELOPE(17.282,17.282,76.974,76.974) Svalbard Land Degradation & Development 34 16 4823 4832
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The paper describes the transformation of the coastal landscape near former Davislaguna Lake, SE Spitsbergen. It is a comparative study which outlines the changing state of the area based on old maps, other archival materials, remote sensing data from the years 1900 to 2021, and our own fieldwork performed since 2005. The indirect cause of this transformation is identified herein as climate warming which has produced a progressive degradation of the cryosphere and triggered three key forces behind the said transformation: glacial recession in the 20th century, shortening of the sea‐ice season, permafrost thawing in the 21st century. From the year 1900 to the 1920s the coastal landscape of the study area consisted of a bay with beaches between a mountain range in the west and a tidewater glacier tongue protruding into the sea in the northeast. The tongue subsequently melted and the bay became transformed into a coastal plain, with the resulting lake becoming separated from the sea by a gravel‐sand bar by 1936. Afterwards, both the plain and lake dwindled in size due to the decline of the bar found to the west. This process continued until the lake became divided into two parts in the 1980s; one of these then disappeared between 2006 and 2010, and the second one by 2021. Hence, the land in question, with the coastal plain partly glaciated and surrounding the bay, then unglaciated and surrounding the lake, became over time replaced by the sea. Today, the process of abrasion acting near the sea is destroying the remaining beaches and cutting down the steep slopes of area mountains and ice‐cored moraines.
format Article in Journal/Newspaper
author Ziaja, Wieslaw
Ostafin, Krzysztof
Maciejowski, Wojciech
Kruse, Frigga
spellingShingle Ziaja, Wieslaw
Ostafin, Krzysztof
Maciejowski, Wojciech
Kruse, Frigga
Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
author_facet Ziaja, Wieslaw
Ostafin, Krzysztof
Maciejowski, Wojciech
Kruse, Frigga
author_sort Ziaja, Wieslaw
title Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
title_short Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
title_full Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
title_fullStr Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
title_full_unstemmed Coastal landscape degradation and disappearance of Davislaguna Lake, Sørkappland, Svalbard, 1900–2021
title_sort coastal landscape degradation and disappearance of davislaguna lake, sørkappland, svalbard, 1900–2021
publisher Wiley
publishDate 2023
url http://dx.doi.org/10.1002/ldr.4765
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.4765
long_lat ENVELOPE(17.282,17.282,76.974,76.974)
geographic Davislaguna
Svalbard
geographic_facet Davislaguna
Svalbard
genre glacier
Ice
permafrost
Sea ice
Svalbard
Tidewater
Spitsbergen
genre_facet glacier
Ice
permafrost
Sea ice
Svalbard
Tidewater
Spitsbergen
op_source Land Degradation & Development
volume 34, issue 16, page 4823-4832
ISSN 1085-3278 1099-145X
op_rights http://creativecommons.org/licenses/by-nc-nd/4.0/
op_doi https://doi.org/10.1002/ldr.4765
container_title Land Degradation & Development
container_volume 34
container_issue 16
container_start_page 4823
op_container_end_page 4832
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