50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes
Artículo de publicación ISI Despite their importance as freshwater reservoirs for downstream river systems, few glaciers in central Chile have been comprehensively surveyed. This study presents ground-penetrating radar (GPR) and field-based observations for characterizing the englacial and basal con...
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ftunivchile:oai:repositorio.uchile.cl:2250/135590 2023-05-15T13:29:08+02:00 50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes Gacitúa, Guisella Uribe, José A. Wilson, Ryan Loriaux, Thomas Hernández, Jorge Rivera Ibáñez, Sergio 2015 application/pdf https://doi.org/10.3189/2015AoG70A953 https://repositorio.uchile.cl/handle/2250/135590 en eng Int Glaciol Soc Annals of Glaciology 56(70) 2015 doi:10.3189/2015AoG70A953 https://repositorio.uchile.cl/handle/2250/135590 Atribución-NoComercial-SinDerivadas 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ CC-BY-NC-ND Aerogeophysical measurements Applied glaciology Basal ice Glacial geomorphology Artículo de revista 2015 ftunivchile https://doi.org/10.3189/2015AoG70A953 2023-01-22T01:03:58Z Artículo de publicación ISI Despite their importance as freshwater reservoirs for downstream river systems, few glaciers in central Chile have been comprehensively surveyed. This study presents ground-penetrating radar (GPR) and field-based observations for characterizing the englacial and basal conditions of Glaciar Olivares Alfa (33°110 S, 70°130 W), central Chilean Andes. Using a 50MHz radar mounted onto a helicopter platform, data were collected covering large portions of the glacier accumulation and ablation zones. The radar data revealed boundaries of a temperate-ice layer at the base of the eastern body of Glaciar Olivares Alfa which appears to be covered by colder ice that extends throughout large parts of the glacier. The thickness of the temperate ice layer is highly variable across the glacier, being on average 40% of the total ice thickness. Radar data analyses reveal regions of cold ice at the bottom/ base of the glacier and also patterns of highly saturated sediments beneath the glacier. Using GPR data, this study represents the most exhaustive analysis of glacier ice structure performed in the central Chilean Andes. The results will enable improved estimations of the glacier’s mass balance and ice dynamics, helping us to understand its further development and its impact on water availability. Basal Financing Program of the Scientific and Technological National Commission of Chile (CONICYT) CODELCO Andina Division mining company Anglo American Chile mining company Article in Journal/Newspaper Annals of Glaciology Universidad de Chile: Repositorio académico Isi ENVELOPE(-38.550,-38.550,65.617,65.617) Olivares ENVELOPE(-56.983,-56.983,-63.400,-63.400) Annals of Glaciology 56 70 193 201 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Aerogeophysical measurements Applied glaciology Basal ice Glacial geomorphology |
spellingShingle |
Aerogeophysical measurements Applied glaciology Basal ice Glacial geomorphology Gacitúa, Guisella Uribe, José A. Wilson, Ryan Loriaux, Thomas Hernández, Jorge Rivera Ibáñez, Sergio 50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
topic_facet |
Aerogeophysical measurements Applied glaciology Basal ice Glacial geomorphology |
description |
Artículo de publicación ISI Despite their importance as freshwater reservoirs for downstream river systems, few glaciers in central Chile have been comprehensively surveyed. This study presents ground-penetrating radar (GPR) and field-based observations for characterizing the englacial and basal conditions of Glaciar Olivares Alfa (33°110 S, 70°130 W), central Chilean Andes. Using a 50MHz radar mounted onto a helicopter platform, data were collected covering large portions of the glacier accumulation and ablation zones. The radar data revealed boundaries of a temperate-ice layer at the base of the eastern body of Glaciar Olivares Alfa which appears to be covered by colder ice that extends throughout large parts of the glacier. The thickness of the temperate ice layer is highly variable across the glacier, being on average 40% of the total ice thickness. Radar data analyses reveal regions of cold ice at the bottom/ base of the glacier and also patterns of highly saturated sediments beneath the glacier. Using GPR data, this study represents the most exhaustive analysis of glacier ice structure performed in the central Chilean Andes. The results will enable improved estimations of the glacier’s mass balance and ice dynamics, helping us to understand its further development and its impact on water availability. Basal Financing Program of the Scientific and Technological National Commission of Chile (CONICYT) CODELCO Andina Division mining company Anglo American Chile mining company |
format |
Article in Journal/Newspaper |
author |
Gacitúa, Guisella Uribe, José A. Wilson, Ryan Loriaux, Thomas Hernández, Jorge Rivera Ibáñez, Sergio |
author_facet |
Gacitúa, Guisella Uribe, José A. Wilson, Ryan Loriaux, Thomas Hernández, Jorge Rivera Ibáñez, Sergio |
author_sort |
Gacitúa, Guisella |
title |
50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
title_short |
50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
title_full |
50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
title_fullStr |
50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
title_full_unstemmed |
50 MHz helicopter-borne radar data for determination of glacier thermal regime in the central Chilean Andes |
title_sort |
50 mhz helicopter-borne radar data for determination of glacier thermal regime in the central chilean andes |
publisher |
Int Glaciol Soc |
publishDate |
2015 |
url |
https://doi.org/10.3189/2015AoG70A953 https://repositorio.uchile.cl/handle/2250/135590 |
long_lat |
ENVELOPE(-38.550,-38.550,65.617,65.617) ENVELOPE(-56.983,-56.983,-63.400,-63.400) |
geographic |
Isi Olivares |
geographic_facet |
Isi Olivares |
genre |
Annals of Glaciology |
genre_facet |
Annals of Glaciology |
op_relation |
Annals of Glaciology 56(70) 2015 doi:10.3189/2015AoG70A953 https://repositorio.uchile.cl/handle/2250/135590 |
op_rights |
Atribución-NoComercial-SinDerivadas 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.3189/2015AoG70A953 |
container_title |
Annals of Glaciology |
container_volume |
56 |
container_issue |
70 |
container_start_page |
193 |
op_container_end_page |
201 |
_version_ |
1765998663911342080 |