Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica

Abstract This study investigates the transient snowline (TSL) altitude for summer 2020, as well as glacial area loss in King George Island Icefields since 1988 using Sentinel-1 and 2 and Landsat Thematic Mapper (TM) imagery. Trends and anomalies in atmospheric temperature, U-wind, and V-wind were ex...

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Main Authors: JÚLIA L. LORENZ, KÁTIA K. DA ROSA, CARINA PETSCH, CLEIVA PERONDI, FILIPE D. IDALINO, JEFFREY DANIEL AUGER, ROSEMARY VIEIRA, JEFFERSON C. SIMÕES
Format: Article
Language:English
Published: Academia Brasileira de Ciências 2023-12-01
Series:Anais da Academia Brasileira de Ciências
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652023000601108&tlng=en
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author JÚLIA L. LORENZ
KÁTIA K. DA ROSA
CARINA PETSCH
CLEIVA PERONDI
FILIPE D. IDALINO
JEFFREY DANIEL AUGER
ROSEMARY VIEIRA
JEFFERSON C. SIMÕES
author_facet JÚLIA L. LORENZ
KÁTIA K. DA ROSA
CARINA PETSCH
CLEIVA PERONDI
FILIPE D. IDALINO
JEFFREY DANIEL AUGER
ROSEMARY VIEIRA
JEFFERSON C. SIMÕES
author_sort JÚLIA L. LORENZ
collection DOAJ
description Abstract This study investigates the transient snowline (TSL) altitude for summer 2020, as well as glacial area loss in King George Island Icefields since 1988 using Sentinel-1 and 2 and Landsat Thematic Mapper (TM) imagery. Trends and anomalies in atmospheric temperature, U-wind, and V-wind were examined using ERA5 solutions. Results show the wet-snow zone corresponds to values of ≤ -13dB, and 44.3% of the glacial area is located above the TSL (≥ 300 m). Glacial area for 2020 is 999.95 km², and losses in the period represent 104.9 km² (error <1%) – a retreat of 3.17 km² / year. Glaciers in Keller Peninsula and Bellingshausen Dome lost the most area (28% and 17%, respectively) and did not have a TSL in 2020; followed by Warszawa (15%), Kraków (13%), and Eastern (10%), where the TSL was verified. Percentage area loss values increased with decreases in dimensions, area above TSL, and maximum elevation. Calving glaciers with ice-flow toward deeper and steeper submarine sectors (Bransfield Strait) exhibited greater glacier variations. The trend in warming atmospheric temperature was greater in the Bransfield Strait than in the Drake Passage. TSL and retreat difference between glaciers were influenced by climatic and ocean input, as well as multiple environmental factors.
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spelling doaj.art-4bc82243cb014bdfb8fd3c10e4fabcfd2023-12-05T07:50:41ZengAcademia Brasileira de CiênciasAnais da Academia Brasileira de Ciências1678-26902023-12-0195suppl 310.1590/0001-3765202320211627Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, AntarcticaJÚLIA L. LORENZhttps://orcid.org/0000-0003-1695-1807KÁTIA K. DA ROSAhttps://orcid.org/0000-0003-0977-9658CARINA PETSCHhttps://orcid.org/0000-0002-1079-0080CLEIVA PERONDIhttps://orcid.org/0000-0003-2202-2721FILIPE D. IDALINOhttps://orcid.org/0000-0001-5587-5208JEFFREY DANIEL AUGERhttps://orcid.org/0000-0002-2304-2292ROSEMARY VIEIRAhttps://orcid.org/0000-0003-0312-2890JEFFERSON C. SIMÕEShttps://orcid.org/0000-0001-5555-3401Abstract This study investigates the transient snowline (TSL) altitude for summer 2020, as well as glacial area loss in King George Island Icefields since 1988 using Sentinel-1 and 2 and Landsat Thematic Mapper (TM) imagery. Trends and anomalies in atmospheric temperature, U-wind, and V-wind were examined using ERA5 solutions. Results show the wet-snow zone corresponds to values of ≤ -13dB, and 44.3% of the glacial area is located above the TSL (≥ 300 m). Glacial area for 2020 is 999.95 km², and losses in the period represent 104.9 km² (error <1%) – a retreat of 3.17 km² / year. Glaciers in Keller Peninsula and Bellingshausen Dome lost the most area (28% and 17%, respectively) and did not have a TSL in 2020; followed by Warszawa (15%), Kraków (13%), and Eastern (10%), where the TSL was verified. Percentage area loss values increased with decreases in dimensions, area above TSL, and maximum elevation. Calving glaciers with ice-flow toward deeper and steeper submarine sectors (Bransfield Strait) exhibited greater glacier variations. The trend in warming atmospheric temperature was greater in the Bransfield Strait than in the Drake Passage. TSL and retreat difference between glaciers were influenced by climatic and ocean input, as well as multiple environmental factors.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652023000601108&tlng=enclimate changeglacier fluctuationsNDSISentinelsnowline
spellingShingle JÚLIA L. LORENZ
KÁTIA K. DA ROSA
CARINA PETSCH
CLEIVA PERONDI
FILIPE D. IDALINO
JEFFREY DANIEL AUGER
ROSEMARY VIEIRA
JEFFERSON C. SIMÕES
Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
Anais da Academia Brasileira de Ciências
climate change
glacier fluctuations
NDSI
Sentinel
snowline
title Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
title_full Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
title_fullStr Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
title_full_unstemmed Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
title_short Short-term glacier area changes, glacier geometry dependence, and regional climatic variations forcing, King George Island, Antarctica
title_sort short term glacier area changes glacier geometry dependence and regional climatic variations forcing king george island antarctica
topic climate change
glacier fluctuations
NDSI
Sentinel
snowline
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652023000601108&tlng=en
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