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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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 |
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908 |
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1779316234824712192 |