The Rapid and Steady Mass Loss of the Patagonian Icefields throughout the GRACE Era: 2002–2017
- Autores
- Richter, Andreas; Groh, Andreas; Horwath, Martin; Ivins, Erik; Marderwald, Eric Rodolfo; Hormaechea, José Luis; Perdomo, Raúl Aníbal; 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.
Laboratorio de Meteorología espacial, Atmósfera terrestre, Geodesia, Geodinámica, diseño de Instrumental y Astrometría - Materia
-
Ciencias Astronómicas
Ice mass
Satellite gravimetry
Patagonia
GRACE - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/125385
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, AndreasGroh, AndreasHorwath, MartinIvins, ErikMarderwald, Eric RodolfoHormaechea, José LuisPerdomo, Raúl AníbalDietrich, ReinhardCiencias AstronómicasIce massSatellite gravimetryPatagoniaGRACEWe 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.Laboratorio de Meteorología espacial, Atmósfera terrestre, Geodesia, Geodinámica, diseño de Instrumental y Astrometría2019info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/125385enginfo:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2072-4292/11/8/909info:eu-repo/semantics/altIdentifier/issn/2072-4292info:eu-repo/semantics/altIdentifier/doi/10.3390/rs11080909info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-15T11:21:56Zoai:sedici.unlp.edu.ar:10915/125385Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-15 11:21:56.482SEDICI (UNLP) - Universidad Nacional de La Platafalse |
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 Ciencias Astronómicas 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 Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Aníbal Dietrich, Reinhard |
author |
Richter, Andreas |
author_facet |
Richter, Andreas Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Aníbal Dietrich, Reinhard |
author_role |
author |
author2 |
Groh, Andreas Horwath, Martin Ivins, Erik Marderwald, Eric Rodolfo Hormaechea, José Luis Perdomo, Raúl Aníbal Dietrich, Reinhard |
author2_role |
author author author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Astronómicas Ice mass Satellite gravimetry Patagonia GRACE |
topic |
Ciencias Astronómicas Ice mass Satellite gravimetry Patagonia GRACE |
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. Laboratorio de Meteorología espacial, Atmósfera terrestre, Geodesia, Geodinámica, diseño de Instrumental y Astrometría |
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 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo 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://sedici.unlp.edu.ar/handle/10915/125385 |
url |
http://sedici.unlp.edu.ar/handle/10915/125385 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://www.mdpi.com/2072-4292/11/8/909 info:eu-repo/semantics/altIdentifier/issn/2072-4292 info:eu-repo/semantics/altIdentifier/doi/10.3390/rs11080909 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
eu_rights_str_mv |
openAccess |
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http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International (CC BY 4.0) |
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application/pdf |
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