Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery

The Antarctic Peninsula and the adjacent South Shetland Islands show a significant atmospheric warming trend. Increase in air temperature is commonly associated with glacier melting. However, there is a dearth of documentation about the glaciers of Greenwich Island. This study fills a knowledge gap...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16016
http://id.nii.ac.jp/1291/00015904/
id ftnipr:oai:nipr.repo.nii.ac.jp:00016016
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00016016 2023-05-15T13:49:00+02:00 Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery 2020-06 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16016 http://id.nii.ac.jp/1291/00015904/ en eng https://doi.org/10.1016/j.polar.2020.100526 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16016 http://id.nii.ac.jp/1291/00015904/ Polar Science, 24, 100526(2020-06) 18739652 Glacier Antarctica Remote sensing Greenwich island Journal Article 2020 ftnipr https://doi.org/10.1016/j.polar.2020.100526 2022-12-03T19:43:16Z The Antarctic Peninsula and the adjacent South Shetland Islands show a significant atmospheric warming trend. Increase in air temperature is commonly associated with glacier melting. However, there is a dearth of documentation about the glaciers of Greenwich Island. This study fills a knowledge gap about glacier melting on Greenwich Island by focusing on four glaciers located on the northern part of it. We also update the temperature trends and analyze the relationship between glaciers melting and temperature changes. We used airborne, optical and SAR satellite sensors along with in-situ measurements over the 1956–2019 period to map glaciers extent changes. The total ice cover of these glaciers decreased from 10.01 km2 in 1956 to 7.97 km2 in 2019, i.e. 20.4%. The results suggest a glacier loss rate of 32359 m2/year (−0.32%/year). This rate of loss is coherent with other measurements made in the South Shetland Islands. We also update the air temperature rising trend in this area to +0.23 °C/decade between 1966 and 2018 at Chile's Arturo Prat base. We do however find two significant trends over the last sixty years: +0.36 °C per decade between 1966 and 1998 and a sharp decrease between 1998 and 2015 of −0.6 °C per decade. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Greenwich Island Polar Science Polar Science South Shetland Islands National Institute of Polar Research Repository, Japan Antarctic The Antarctic Antarctic Peninsula South Shetland Islands Greenwich Prat ENVELOPE(-59.467,-59.467,-62.467,-62.467) Greenwich Island ENVELOPE(-59.783,-59.783,-62.517,-62.517) Polar Science 24 100526
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Glacier
Antarctica
Remote sensing
Greenwich island
spellingShingle Glacier
Antarctica
Remote sensing
Greenwich island
Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
topic_facet Glacier
Antarctica
Remote sensing
Greenwich island
description The Antarctic Peninsula and the adjacent South Shetland Islands show a significant atmospheric warming trend. Increase in air temperature is commonly associated with glacier melting. However, there is a dearth of documentation about the glaciers of Greenwich Island. This study fills a knowledge gap about glacier melting on Greenwich Island by focusing on four glaciers located on the northern part of it. We also update the temperature trends and analyze the relationship between glaciers melting and temperature changes. We used airborne, optical and SAR satellite sensors along with in-situ measurements over the 1956–2019 period to map glaciers extent changes. The total ice cover of these glaciers decreased from 10.01 km2 in 1956 to 7.97 km2 in 2019, i.e. 20.4%. The results suggest a glacier loss rate of 32359 m2/year (−0.32%/year). This rate of loss is coherent with other measurements made in the South Shetland Islands. We also update the air temperature rising trend in this area to +0.23 °C/decade between 1966 and 2018 at Chile's Arturo Prat base. We do however find two significant trends over the last sixty years: +0.36 °C per decade between 1966 and 1998 and a sharp decrease between 1998 and 2015 of −0.6 °C per decade.
format Article in Journal/Newspaper
title Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
title_short Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
title_full Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
title_fullStr Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
title_full_unstemmed Estimating ice retreat on Greenwich island – Antarctica between 1956 and 2019 using optical and SAR imagery
title_sort estimating ice retreat on greenwich island – antarctica between 1956 and 2019 using optical and sar imagery
publishDate 2020
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16016
http://id.nii.ac.jp/1291/00015904/
long_lat ENVELOPE(-59.467,-59.467,-62.467,-62.467)
ENVELOPE(-59.783,-59.783,-62.517,-62.517)
geographic Antarctic
The Antarctic
Antarctic Peninsula
South Shetland Islands
Greenwich
Prat
Greenwich Island
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
South Shetland Islands
Greenwich
Prat
Greenwich Island
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Greenwich Island
Polar Science
Polar Science
South Shetland Islands
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Greenwich Island
Polar Science
Polar Science
South Shetland Islands
op_relation https://doi.org/10.1016/j.polar.2020.100526
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16016
http://id.nii.ac.jp/1291/00015904/
Polar Science, 24, 100526(2020-06)
18739652
op_doi https://doi.org/10.1016/j.polar.2020.100526
container_title Polar Science
container_volume 24
container_start_page 100526
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