First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images

We apply cross-correlation to Pléiades satellite images to generate accurate, highresolution monthly surface velocity maps of Monte Tronador glaciers between March and June 2012. Measured surface displacements cover periods as short as 19 days, with a precision of 0.58 m (11 m a–1). These glaciers f...

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Published in:Journal of Glaciology
Main Authors: Ruiz, Lucas Ernesto, Berthier, E., Masiokas, Mariano Hugo, Pitte, Pedro Miguel, Villalba, Ricardo
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society
Subjects:
Online Access:http://hdl.handle.net/11336/38221
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record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/38221 2023-10-09T21:53:01+02:00 First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images Ruiz, Lucas Ernesto Berthier, E. Masiokas, Mariano Hugo Pitte, Pedro Miguel Villalba, Ricardo application/pdf http://hdl.handle.net/11336/38221 eng eng International Glaciological Society info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.3189/2015JoG14J134 info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/journal-of-glaciology/article/first-surface-velocity-maps-for-glaciers-of-monte-tronador-north-patagonian-andes-derived-from-sequential-pleiades-satellite-images/863108563B74396906ED7557CB275EA5 http://hdl.handle.net/11336/38221 Ruiz, Lucas Ernesto; Berthier, E.; Masiokas, Mariano Hugo; Pitte, Pedro Miguel; Villalba, Ricardo; First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images; International Glaciological Society; Journal Of Glaciology; 61; 229; 11-2015; 908-922 0022-1430 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ Glacier Flow Ice Dynamics Ice Velocity Remote Sensing Subglacial Processes https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.3189/2015JoG14J134 2023-09-24T18:57:10Z We apply cross-correlation to Pléiades satellite images to generate accurate, highresolution monthly surface velocity maps of Monte Tronador glaciers between March and June 2012. Measured surface displacements cover periods as short as 19 days, with a precision of 0.58 m (11 m a–1). These glaciers follow a radial flow pattern, with maximum surface speeds of 390 m a–1 associated with steep icefalls. The lower reaches of the debris-covered tongues of Verde and Casa Pangue glaciers are almost stagnant, whereas Ventisquero Negro, another debris-covered glacier, shows acceleration at the front due to calving into a proglacial lake. Low-elevation debris-covered glacier tongues show increasing velocities at the beginning of the accumulation season, whereas higherelevation, clean-ice tongues reduce their speed during this period. This contrasting behavior is probably in response to an increase in water input to the subglacial system from winter rainfall events at low elevations and a decrease in meltwater production at higher elevations. These sequential velocity maps can help to identify the controls on glacier surface velocity, aid in the delimitation of ice divides and could also contribute to more realistic calibration of ice-flux–mass-balance models in this glacierized area. Fil: Ruiz, Lucas Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Berthier, E. Universite de Toulouse; Francia Fil: Masiokas, Mariano Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias ... Article in Journal/Newspaper Journal of Glaciology CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentino Argentina Tronador ENVELOPE(-62.917,-62.917,-64.317,-64.317) Ventisquero ENVELOPE(-45.383,-45.383,-60.717,-60.717) Journal of Glaciology 61 229 908 922
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic Glacier Flow
Ice Dynamics
Ice Velocity
Remote Sensing
Subglacial Processes
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle Glacier Flow
Ice Dynamics
Ice Velocity
Remote Sensing
Subglacial Processes
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Ruiz, Lucas Ernesto
Berthier, E.
Masiokas, Mariano Hugo
Pitte, Pedro Miguel
Villalba, Ricardo
First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
topic_facet Glacier Flow
Ice Dynamics
Ice Velocity
Remote Sensing
Subglacial Processes
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description We apply cross-correlation to Pléiades satellite images to generate accurate, highresolution monthly surface velocity maps of Monte Tronador glaciers between March and June 2012. Measured surface displacements cover periods as short as 19 days, with a precision of 0.58 m (11 m a–1). These glaciers follow a radial flow pattern, with maximum surface speeds of 390 m a–1 associated with steep icefalls. The lower reaches of the debris-covered tongues of Verde and Casa Pangue glaciers are almost stagnant, whereas Ventisquero Negro, another debris-covered glacier, shows acceleration at the front due to calving into a proglacial lake. Low-elevation debris-covered glacier tongues show increasing velocities at the beginning of the accumulation season, whereas higherelevation, clean-ice tongues reduce their speed during this period. This contrasting behavior is probably in response to an increase in water input to the subglacial system from winter rainfall events at low elevations and a decrease in meltwater production at higher elevations. These sequential velocity maps can help to identify the controls on glacier surface velocity, aid in the delimitation of ice divides and could also contribute to more realistic calibration of ice-flux–mass-balance models in this glacierized area. Fil: Ruiz, Lucas Ernesto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Berthier, E. Universite de Toulouse; Francia Fil: Masiokas, Mariano Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias ...
format Article in Journal/Newspaper
author Ruiz, Lucas Ernesto
Berthier, E.
Masiokas, Mariano Hugo
Pitte, Pedro Miguel
Villalba, Ricardo
author_facet Ruiz, Lucas Ernesto
Berthier, E.
Masiokas, Mariano Hugo
Pitte, Pedro Miguel
Villalba, Ricardo
author_sort Ruiz, Lucas Ernesto
title First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
title_short First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
title_full First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
title_fullStr First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
title_full_unstemmed First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images
title_sort first surface velocity maps for glaciers of monte tronador, north patagonian andes, derived from sequential pléiades satellite images
publisher International Glaciological Society
url http://hdl.handle.net/11336/38221
long_lat ENVELOPE(-62.917,-62.917,-64.317,-64.317)
ENVELOPE(-45.383,-45.383,-60.717,-60.717)
geographic Argentino
Argentina
Tronador
Ventisquero
geographic_facet Argentino
Argentina
Tronador
Ventisquero
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.3189/2015JoG14J134
info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/journal-of-glaciology/article/first-surface-velocity-maps-for-glaciers-of-monte-tronador-north-patagonian-andes-derived-from-sequential-pleiades-satellite-images/863108563B74396906ED7557CB275EA5
http://hdl.handle.net/11336/38221
Ruiz, Lucas Ernesto; Berthier, E.; Masiokas, Mariano Hugo; Pitte, Pedro Miguel; Villalba, Ricardo; First surface velocity maps for glaciers of Monte Tronador, North Patagonian Andes, derived from sequential Pléiades satellite images; International Glaciological Society; Journal Of Glaciology; 61; 229; 11-2015; 908-922
0022-1430
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
op_doi https://doi.org/10.3189/2015JoG14J134
container_title Journal of Glaciology
container_volume 61
container_issue 229
container_start_page 908
op_container_end_page 922
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