Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia

The study of glaciers in remote regions improves our understanding of global glacier change. With an area of 149.31 ± 1.84 km2, the Santa Inés Icefield constitutes one of the largest and least studied and explored glaciated areas of Southern Patagonia. We study the extent and glacier variations of t...

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Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Isaac Gurdiel, Camilo Rada, Philipp Malz, Matthias Braun, Gino Casassa
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2022
Subjects:
geo
Online Access:https://doi.org/10.1080/15230430.2022.2071793
https://doaj.org/article/d34a7916bf814ccca81a98b03e127b47
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:d34a7916bf814ccca81a98b03e127b47 2023-05-15T14:14:25+02:00 Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia Isaac Gurdiel Camilo Rada Philipp Malz Matthias Braun Gino Casassa 2022-12-01 https://doi.org/10.1080/15230430.2022.2071793 https://doaj.org/article/d34a7916bf814ccca81a98b03e127b47 en eng Taylor & Francis Group doi:10.1080/15230430.2022.2071793 1938-4246 1523-0430 https://doaj.org/article/d34a7916bf814ccca81a98b03e127b47 undefined Arctic, Antarctic, and Alpine Research, Vol 54, Iss 1, Pp 202-220 (2022) Glacier inventory recent variations Patagonia geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.1080/15230430.2022.2071793 2023-01-22T17:53:16Z The study of glaciers in remote regions improves our understanding of global glacier change. With an area of 149.31 ± 1.84 km2, the Santa Inés Icefield constitutes one of the largest and least studied and explored glaciated areas of Southern Patagonia. We study the extent and glacier variations of the Santa Inés Icefield over the last 75 years, and we generate the most detailed glacier inventory to date of its 24 constituting glaciers. We estimate surface elevation changes between 2000 and 2014 using Shuttle Radar Topography Mission (SRTM) and TanDEM-X digital elevation models. Our results show a generalized trend of retreat, with a glacier area loss of −9.78 ± 1.52 km2 between 1998 and 2020, with annual rate increase from −0.15 ± 0.01 km2 a−1 (1998–2005) to −0.58 ± 0.10 km2 a−1 (2005–2020), and an average thinning of 0.60 ± 0.26 m a−1 (2σ) between 2000 and 2014. No clear correlation was found between retreat or thinning rates and Accumulation Area Ratio (AAR), terminus slope, aspect, or glacier type. While ERA5 reanalysis data shows no significant climatic trends in temperature or precipitation, a small warming trend below our detection record is the most likely cause of the observed retreat and thinning of the Santa Inés Icefield. Article in Journal/Newspaper Antarctic and Alpine Research Arctic Unknown Patagonia Arctic, Antarctic, and Alpine Research 54 1 202 220
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic Glacier inventory
recent variations
Patagonia
geo
envir
spellingShingle Glacier inventory
recent variations
Patagonia
geo
envir
Isaac Gurdiel
Camilo Rada
Philipp Malz
Matthias Braun
Gino Casassa
Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
topic_facet Glacier inventory
recent variations
Patagonia
geo
envir
description The study of glaciers in remote regions improves our understanding of global glacier change. With an area of 149.31 ± 1.84 km2, the Santa Inés Icefield constitutes one of the largest and least studied and explored glaciated areas of Southern Patagonia. We study the extent and glacier variations of the Santa Inés Icefield over the last 75 years, and we generate the most detailed glacier inventory to date of its 24 constituting glaciers. We estimate surface elevation changes between 2000 and 2014 using Shuttle Radar Topography Mission (SRTM) and TanDEM-X digital elevation models. Our results show a generalized trend of retreat, with a glacier area loss of −9.78 ± 1.52 km2 between 1998 and 2020, with annual rate increase from −0.15 ± 0.01 km2 a−1 (1998–2005) to −0.58 ± 0.10 km2 a−1 (2005–2020), and an average thinning of 0.60 ± 0.26 m a−1 (2σ) between 2000 and 2014. No clear correlation was found between retreat or thinning rates and Accumulation Area Ratio (AAR), terminus slope, aspect, or glacier type. While ERA5 reanalysis data shows no significant climatic trends in temperature or precipitation, a small warming trend below our detection record is the most likely cause of the observed retreat and thinning of the Santa Inés Icefield.
format Article in Journal/Newspaper
author Isaac Gurdiel
Camilo Rada
Philipp Malz
Matthias Braun
Gino Casassa
author_facet Isaac Gurdiel
Camilo Rada
Philipp Malz
Matthias Braun
Gino Casassa
author_sort Isaac Gurdiel
title Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
title_short Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
title_full Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
title_fullStr Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
title_full_unstemmed Glacier inventory and recent variations of Santa Inés Icefield, Southern Patagonia
title_sort glacier inventory and recent variations of santa inés icefield, southern patagonia
publisher Taylor & Francis Group
publishDate 2022
url https://doi.org/10.1080/15230430.2022.2071793
https://doaj.org/article/d34a7916bf814ccca81a98b03e127b47
geographic Patagonia
geographic_facet Patagonia
genre Antarctic and Alpine Research
Arctic
genre_facet Antarctic and Alpine Research
Arctic
op_source Arctic, Antarctic, and Alpine Research, Vol 54, Iss 1, Pp 202-220 (2022)
op_relation doi:10.1080/15230430.2022.2071793
1938-4246
1523-0430
https://doaj.org/article/d34a7916bf814ccca81a98b03e127b47
op_rights undefined
op_doi https://doi.org/10.1080/15230430.2022.2071793
container_title Arctic, Antarctic, and Alpine Research
container_volume 54
container_issue 1
container_start_page 202
op_container_end_page 220
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