Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021

Glacier change in Kenai Fjords National Park in southcentral Alaska affects local terrestrial, fresh water and marine ecosystems and will likely impact ecotourism. We used Landsat 4–8 imagery from 1984 through 2021 to manually map lower glacier ice margins for 19 maritime glaciers in Kenai Fjords Na...

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Published in:Journal of Glaciology
Main Authors: Taryn Black, Deborah Kurtz
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.55
https://doaj.org/article/88c3ae8b97164adabba77be379a16bfe
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spelling ftdoajarticles:oai:doaj.org/article:88c3ae8b97164adabba77be379a16bfe 2023-05-15T16:20:19+02:00 Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021 Taryn Black Deborah Kurtz 2023-04-01T00:00:00Z https://doi.org/10.1017/jog.2022.55 https://doaj.org/article/88c3ae8b97164adabba77be379a16bfe EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000557/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.55 0022-1430 1727-5652 https://doaj.org/article/88c3ae8b97164adabba77be379a16bfe Journal of Glaciology, Vol 69, Pp 251-265 (2023) Glacier mapping glacier monitoring mountain glaciers remote sensing Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.55 2023-03-19T01:31:51Z Glacier change in Kenai Fjords National Park in southcentral Alaska affects local terrestrial, fresh water and marine ecosystems and will likely impact ecotourism. We used Landsat 4–8 imagery from 1984 through 2021 to manually map lower glacier ice margins for 19 maritime glaciers in Kenai Fjords National Park. Of these glaciers, six are tidewater, three are lake-terminating, six are land-terminating and four terminated in more than one environment throughout the study period. We used the mapped ice margins to quantify seasonal terminus position and areal change, including distinguishing between ice loss at glacier termini and along glacier margins. Overall, 13 glaciers substantially retreated (more than 2σ), 14 lost substantial area and only two underwent both net advance and area gain. The glaciers that had insubstantial length and area changes were predominantly tidewater. Cumulatively, the lower reaches of these 19 glaciers lost 42 km2 of ice, which was nearly evenly distributed between the terminus and the lateral margins. The rapid rate of glacier change and subsequent land cover changes are highly visible to visitors and locals at Kenai Fjords National Park, and this study quantifies those changes in terms of glacier length and area. Article in Journal/Newspaper glacier glaciers Journal of Glaciology Tidewater Alaska Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 69 274 251 265
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier mapping
glacier monitoring
mountain glaciers
remote sensing
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier mapping
glacier monitoring
mountain glaciers
remote sensing
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Taryn Black
Deborah Kurtz
Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
topic_facet Glacier mapping
glacier monitoring
mountain glaciers
remote sensing
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Glacier change in Kenai Fjords National Park in southcentral Alaska affects local terrestrial, fresh water and marine ecosystems and will likely impact ecotourism. We used Landsat 4–8 imagery from 1984 through 2021 to manually map lower glacier ice margins for 19 maritime glaciers in Kenai Fjords National Park. Of these glaciers, six are tidewater, three are lake-terminating, six are land-terminating and four terminated in more than one environment throughout the study period. We used the mapped ice margins to quantify seasonal terminus position and areal change, including distinguishing between ice loss at glacier termini and along glacier margins. Overall, 13 glaciers substantially retreated (more than 2σ), 14 lost substantial area and only two underwent both net advance and area gain. The glaciers that had insubstantial length and area changes were predominantly tidewater. Cumulatively, the lower reaches of these 19 glaciers lost 42 km2 of ice, which was nearly evenly distributed between the terminus and the lateral margins. The rapid rate of glacier change and subsequent land cover changes are highly visible to visitors and locals at Kenai Fjords National Park, and this study quantifies those changes in terms of glacier length and area.
format Article in Journal/Newspaper
author Taryn Black
Deborah Kurtz
author_facet Taryn Black
Deborah Kurtz
author_sort Taryn Black
title Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
title_short Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
title_full Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
title_fullStr Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
title_full_unstemmed Maritime glacier retreat and terminus area change in Kenai Fjords National Park, Alaska, between 1984 and 2021
title_sort maritime glacier retreat and terminus area change in kenai fjords national park, alaska, between 1984 and 2021
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2022.55
https://doaj.org/article/88c3ae8b97164adabba77be379a16bfe
genre glacier
glaciers
Journal of Glaciology
Tidewater
Alaska
genre_facet glacier
glaciers
Journal of Glaciology
Tidewater
Alaska
op_source Journal of Glaciology, Vol 69, Pp 251-265 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000557/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.55
0022-1430
1727-5652
https://doaj.org/article/88c3ae8b97164adabba77be379a16bfe
op_doi https://doi.org/10.1017/jog.2022.55
container_title Journal of Glaciology
container_volume 69
container_issue 274
container_start_page 251
op_container_end_page 265
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