The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017
- Autores
- Richter, Andreas Jorg; Groh, Andreas; Horwath, Martin; Ivins, Erik; Marderwald, Eric Rodolfo; Hormaechea, José Luis; Perdomo, Raúl; Dietrich, Reinhard
- Año de publicación
- 2019
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for by a regional model that is constrained by global navigation satellite systems (GNSS) uplift observations. Further corrections are applied concerning the effect of mass variations in the ocean, in the continental water storage, and of the Antarctic ice sheet. The 161 monthly GRACE gravity field solutions are inverted in the spatial domain through the adjustment of scaling factors applied to a-priori ice mass change patterns based on published remote sensing results for the Southern and Northern Patagonian Icefields, respectively. We infer an ice mass change rate of -24.4 ± 4.7 Gt/a for the Patagonian Icefields between April 2002 and June 2017, which corresponds to a contribution to the eustatic sea level rise of 0.067 ± 0.013 mm/a. Our time series of monthly ice mass changes reveals no indication for an acceleration in ice mass loss. We find indications that the Northern Patagonian Icefield contributes more to the integral ice loss than previously assumed.
Fil: Richter, Andreas Jorg. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Technische Universität Dresden; Alemania
Fil: Groh, Andreas. Technische Universität Dresden; Alemania
Fil: Horwath, Martin. Technische Universität Dresden; Alemania
Fil: Ivins, Erik. California Institute of Technology; Estados Unidos
Fil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Hormaechea, José Luis. Estacion Astronomica Rio Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Perdomo, Raúl. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Dietrich, Reinhard. Technische Universität Dresden; Alemania - Materia
-
ICE MASS
SATELLITE GRAVIMETRY
PATAGONIA
GRACE - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/119256
Ver los metadatos del registro completo
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The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017Richter, Andreas JorgGroh, AndreasHorwath, MartinIvins, ErikMarderwald, Eric RodolfoHormaechea, José LuisPerdomo, RaúlDietrich, ReinhardICE MASSSATELLITE GRAVIMETRYPATAGONIAGRACEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for by a regional model that is constrained by global navigation satellite systems (GNSS) uplift observations. Further corrections are applied concerning the effect of mass variations in the ocean, in the continental water storage, and of the Antarctic ice sheet. The 161 monthly GRACE gravity field solutions are inverted in the spatial domain through the adjustment of scaling factors applied to a-priori ice mass change patterns based on published remote sensing results for the Southern and Northern Patagonian Icefields, respectively. We infer an ice mass change rate of -24.4 ± 4.7 Gt/a for the Patagonian Icefields between April 2002 and June 2017, which corresponds to a contribution to the eustatic sea level rise of 0.067 ± 0.013 mm/a. Our time series of monthly ice mass changes reveals no indication for an acceleration in ice mass loss. We find indications that the Northern Patagonian Icefield contributes more to the integral ice loss than previously assumed.Fil: Richter, Andreas Jorg. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Technische Universität Dresden; AlemaniaFil: Groh, Andreas. Technische Universität Dresden; AlemaniaFil: Horwath, Martin. Technische Universität Dresden; AlemaniaFil: Ivins, Erik. California Institute of Technology; Estados UnidosFil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Hormaechea, José Luis. Estacion Astronomica Rio Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Perdomo, Raúl. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Dietrich, Reinhard. Technische Universität Dresden; AlemaniaMDPI2019-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/119256Richter, Andreas Jorg; Groh, Andreas; Horwath, Martin; Ivins, Erik; Marderwald, Eric Rodolfo; et al.; The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017; MDPI; Remote Sensing; 11; 8; 4-2019; 1-202072-4292CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.3390/rs11080909info:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2072-4292/11/8/909info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:54:15Zoai:ri.conicet.gov.ar:11336/119256instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:54:15.419CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
title |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
spellingShingle |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 Richter, Andreas Jorg ICE MASS SATELLITE GRAVIMETRY PATAGONIA GRACE |
title_short |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
title_full |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
title_fullStr |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
title_full_unstemmed |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
title_sort |
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017 |
dc.creator.none.fl_str_mv |
Richter, Andreas Jorg Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Dietrich, Reinhard |
author |
Richter, Andreas Jorg |
author_facet |
Richter, Andreas Jorg Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Dietrich, Reinhard |
author_role |
author |
author2 |
Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Dietrich, Reinhard |
author2_role |
author author author author author author author |
dc.subject.none.fl_str_mv |
ICE MASS SATELLITE GRAVIMETRY PATAGONIA GRACE |
topic |
ICE MASS SATELLITE GRAVIMETRY PATAGONIA GRACE |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for by a regional model that is constrained by global navigation satellite systems (GNSS) uplift observations. Further corrections are applied concerning the effect of mass variations in the ocean, in the continental water storage, and of the Antarctic ice sheet. The 161 monthly GRACE gravity field solutions are inverted in the spatial domain through the adjustment of scaling factors applied to a-priori ice mass change patterns based on published remote sensing results for the Southern and Northern Patagonian Icefields, respectively. We infer an ice mass change rate of -24.4 ± 4.7 Gt/a for the Patagonian Icefields between April 2002 and June 2017, which corresponds to a contribution to the eustatic sea level rise of 0.067 ± 0.013 mm/a. Our time series of monthly ice mass changes reveals no indication for an acceleration in ice mass loss. We find indications that the Northern Patagonian Icefield contributes more to the integral ice loss than previously assumed. Fil: Richter, Andreas Jorg. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Technische Universität Dresden; Alemania Fil: Groh, Andreas. Technische Universität Dresden; Alemania Fil: Horwath, Martin. Technische Universität Dresden; Alemania Fil: Ivins, Erik. California Institute of Technology; Estados Unidos Fil: Marderwald, Eric Rodolfo. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina Fil: Hormaechea, José Luis. Estacion Astronomica Rio Grande; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Perdomo, Raúl. Universidad Nacional de la Plata. Facultad de Cs.astronomicas y Geofisicas. Laboratorio Maggia.; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina Fil: Dietrich, Reinhard. Technische Universität Dresden; Alemania |
description |
We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for by a regional model that is constrained by global navigation satellite systems (GNSS) uplift observations. Further corrections are applied concerning the effect of mass variations in the ocean, in the continental water storage, and of the Antarctic ice sheet. The 161 monthly GRACE gravity field solutions are inverted in the spatial domain through the adjustment of scaling factors applied to a-priori ice mass change patterns based on published remote sensing results for the Southern and Northern Patagonian Icefields, respectively. We infer an ice mass change rate of -24.4 ± 4.7 Gt/a for the Patagonian Icefields between April 2002 and June 2017, which corresponds to a contribution to the eustatic sea level rise of 0.067 ± 0.013 mm/a. Our time series of monthly ice mass changes reveals no indication for an acceleration in ice mass loss. We find indications that the Northern Patagonian Icefield contributes more to the integral ice loss than previously assumed. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-04 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/119256 Richter, Andreas Jorg; Groh, Andreas; Horwath, Martin; Ivins, Erik; Marderwald, Eric Rodolfo; et al.; The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017; MDPI; Remote Sensing; 11; 8; 4-2019; 1-20 2072-4292 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/119256 |
identifier_str_mv |
Richter, Andreas Jorg; Groh, Andreas; Horwath, Martin; Ivins, Erik; Marderwald, Eric Rodolfo; et al.; The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017; MDPI; Remote Sensing; 11; 8; 4-2019; 1-20 2072-4292 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.3390/rs11080909 info:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2072-4292/11/8/909 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
MDPI |
publisher.none.fl_str_mv |
MDPI |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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13.070432 |