Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data
- Autores
- Masiokas, Mariano Hugo; Christie, D. A.; Le Quesne, C.; Pitte, Pedro Miguel; Ruiz, Lucas Ernesto; Villalba, Ricardo; Luckman, B. H.; Berthier, E.; Nussbaumer, S. U.; González Reyes, A.; McPhee, J.; Barcaza, G.
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Despite the great number and variety of glaciers in southern South America, in situ glacier mass balance records are extremely scarce and glacier climate relationships are still poorly understood in this region. Here we use the longest (> 35 years) and most complete in situ mass balance record, available for glaciar Echaurren Norte in the Andes at ~34° S, to develop a minimal glacier surface mass balance model that relies on nearby monthly precipitation and air temperature data as forcing. This basic model is able to explain 78 % of the variance in the annual glacier mass balance record over the 1978?2013 calibration period. An attribution assessment indicates that precipitation variability constitutes the most important forcing modulating annual glacier mass balances at this site. A regionally-averaged series of mean annual streamflow records from both sides of the Andes is then used to estimate, through simple linear regression, this glacier´s annual mass balance variations since 1909. The reconstruction model captures 68 % of the observed glacier mass balance variability and shows three periods of sustained positive mass balances embedded in an overall negative trend totaling almost −42 m w.eq. over the past 105 years. The three periods of sustained positive mass balances (centered in the 1920s?1930s, in the 1980s and in the first decade of the 21st century) coincide with several documented glacier advances in this region. Similar trends observed in other shorter glacier mass balance series suggest the glaciar Echaurren Norte reconstruction is representative of larger-scale conditions and could be useful for more detailed glaciological, hydrological and climatological assessments in this portion of the Andes.
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 Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Christie, D. A.. Universidad Austral de Chile; Chile. Center for Climate and Resilience Research; Chile
Fil: Le Quesne, C.. Universidad Austral de Chile; Chile
Fil: Pitte, Pedro Miguel. 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: 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: Villalba, Ricardo. 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: Luckman, B. H.. University of Western Ontario; Canadá
Fil: Berthier, E.. Centre National de la Recherche Scientifique; Francia
Fil: Nussbaumer, S. U.. University of Fribourg; Suiza
Fil: González Reyes, A.. Universidad de Chile; Chile
Fil: McPhee, J.. Universidad de Chile; Chile
Fil: Barcaza, G.. Dirección General de Aguas; Chile - Materia
-
GLACIER MASS BALANCE
CENTRAL ANDES
RECONSTRUCTION
MINIMAL MODEL - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/69743
Ver los metadatos del registro completo
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Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic dataMasiokas, Mariano HugoChristie, D. A.Le Quesne, C.Pitte, Pedro MiguelRuiz, Lucas ErnestoVillalba, RicardoLuckman, B. H.Berthier, E.Nussbaumer, S. U.González Reyes, A.McPhee, J.Barcaza, G.GLACIER MASS BALANCECENTRAL ANDESRECONSTRUCTIONMINIMAL MODELhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Despite the great number and variety of glaciers in southern South America, in situ glacier mass balance records are extremely scarce and glacier climate relationships are still poorly understood in this region. Here we use the longest (> 35 years) and most complete in situ mass balance record, available for glaciar Echaurren Norte in the Andes at ~34° S, to develop a minimal glacier surface mass balance model that relies on nearby monthly precipitation and air temperature data as forcing. This basic model is able to explain 78 % of the variance in the annual glacier mass balance record over the 1978?2013 calibration period. An attribution assessment indicates that precipitation variability constitutes the most important forcing modulating annual glacier mass balances at this site. A regionally-averaged series of mean annual streamflow records from both sides of the Andes is then used to estimate, through simple linear regression, this glacier´s annual mass balance variations since 1909. The reconstruction model captures 68 % of the observed glacier mass balance variability and shows three periods of sustained positive mass balances embedded in an overall negative trend totaling almost −42 m w.eq. over the past 105 years. The three periods of sustained positive mass balances (centered in the 1920s?1930s, in the 1980s and in the first decade of the 21st century) coincide with several documented glacier advances in this region. Similar trends observed in other shorter glacier mass balance series suggest the glaciar Echaurren Norte reconstruction is representative of larger-scale conditions and could be useful for more detailed glaciological, hydrological and climatological assessments in this portion of the Andes.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 Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Christie, D. A.. Universidad Austral de Chile; Chile. Center for Climate and Resilience Research; ChileFil: Le Quesne, C.. Universidad Austral de Chile; ChileFil: Pitte, Pedro Miguel. 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; ArgentinaFil: 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; ArgentinaFil: Villalba, Ricardo. 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; ArgentinaFil: Luckman, B. H.. University of Western Ontario; CanadáFil: Berthier, E.. Centre National de la Recherche Scientifique; FranciaFil: Nussbaumer, S. U.. University of Fribourg; SuizaFil: González Reyes, A.. Universidad de Chile; ChileFil: McPhee, J.. Universidad de Chile; ChileFil: Barcaza, G.. Dirección General de Aguas; ChileCopernicus Publications2015-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/69743Masiokas, Mariano Hugo; Christie, D. A.; Le Quesne, C.; Pitte, Pedro Miguel; Ruiz, Lucas Ernesto; et al.; Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data; Copernicus Publications; The Cryosphere Discussions; 9; 5; 9-2015; 4949-49801994-04161994-0440CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.5194/tcd-9-4949-2015info:eu-repo/semantics/altIdentifier/url/https://www.the-cryosphere.net/10/927/2016/tc-10-927-2016-discussion.htmlinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-02-26T10:35:49Zoai:ri.conicet.gov.ar:11336/69743instacron: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:34982026-02-26 10:35:49.465CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| title |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| spellingShingle |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data Masiokas, Mariano Hugo GLACIER MASS BALANCE CENTRAL ANDES RECONSTRUCTION MINIMAL MODEL |
| title_short |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| title_full |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| title_fullStr |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| title_full_unstemmed |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| title_sort |
Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data |
| dc.creator.none.fl_str_mv |
Masiokas, Mariano Hugo Christie, D. A. Le Quesne, C. Pitte, Pedro Miguel Ruiz, Lucas Ernesto Villalba, Ricardo Luckman, B. H. Berthier, E. Nussbaumer, S. U. González Reyes, A. McPhee, J. Barcaza, G. |
| author |
Masiokas, Mariano Hugo |
| author_facet |
Masiokas, Mariano Hugo Christie, D. A. Le Quesne, C. Pitte, Pedro Miguel Ruiz, Lucas Ernesto Villalba, Ricardo Luckman, B. H. Berthier, E. Nussbaumer, S. U. González Reyes, A. McPhee, J. Barcaza, G. |
| author_role |
author |
| author2 |
Christie, D. A. Le Quesne, C. Pitte, Pedro Miguel Ruiz, Lucas Ernesto Villalba, Ricardo Luckman, B. H. Berthier, E. Nussbaumer, S. U. González Reyes, A. McPhee, J. Barcaza, G. |
| author2_role |
author author author author author author author author author author author |
| dc.subject.none.fl_str_mv |
GLACIER MASS BALANCE CENTRAL ANDES RECONSTRUCTION MINIMAL MODEL |
| topic |
GLACIER MASS BALANCE CENTRAL ANDES RECONSTRUCTION MINIMAL MODEL |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Despite the great number and variety of glaciers in southern South America, in situ glacier mass balance records are extremely scarce and glacier climate relationships are still poorly understood in this region. Here we use the longest (> 35 years) and most complete in situ mass balance record, available for glaciar Echaurren Norte in the Andes at ~34° S, to develop a minimal glacier surface mass balance model that relies on nearby monthly precipitation and air temperature data as forcing. This basic model is able to explain 78 % of the variance in the annual glacier mass balance record over the 1978?2013 calibration period. An attribution assessment indicates that precipitation variability constitutes the most important forcing modulating annual glacier mass balances at this site. A regionally-averaged series of mean annual streamflow records from both sides of the Andes is then used to estimate, through simple linear regression, this glacier´s annual mass balance variations since 1909. The reconstruction model captures 68 % of the observed glacier mass balance variability and shows three periods of sustained positive mass balances embedded in an overall negative trend totaling almost −42 m w.eq. over the past 105 years. The three periods of sustained positive mass balances (centered in the 1920s?1930s, in the 1980s and in the first decade of the 21st century) coincide with several documented glacier advances in this region. Similar trends observed in other shorter glacier mass balance series suggest the glaciar Echaurren Norte reconstruction is representative of larger-scale conditions and could be useful for more detailed glaciological, hydrological and climatological assessments in this portion of the Andes. 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 Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Christie, D. A.. Universidad Austral de Chile; Chile. Center for Climate and Resilience Research; Chile Fil: Le Quesne, C.. Universidad Austral de Chile; Chile Fil: Pitte, Pedro Miguel. 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: 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: Villalba, Ricardo. 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: Luckman, B. H.. University of Western Ontario; Canadá Fil: Berthier, E.. Centre National de la Recherche Scientifique; Francia Fil: Nussbaumer, S. U.. University of Fribourg; Suiza Fil: González Reyes, A.. Universidad de Chile; Chile Fil: McPhee, J.. Universidad de Chile; Chile Fil: Barcaza, G.. Dirección General de Aguas; Chile |
| description |
Despite the great number and variety of glaciers in southern South America, in situ glacier mass balance records are extremely scarce and glacier climate relationships are still poorly understood in this region. Here we use the longest (> 35 years) and most complete in situ mass balance record, available for glaciar Echaurren Norte in the Andes at ~34° S, to develop a minimal glacier surface mass balance model that relies on nearby monthly precipitation and air temperature data as forcing. This basic model is able to explain 78 % of the variance in the annual glacier mass balance record over the 1978?2013 calibration period. An attribution assessment indicates that precipitation variability constitutes the most important forcing modulating annual glacier mass balances at this site. A regionally-averaged series of mean annual streamflow records from both sides of the Andes is then used to estimate, through simple linear regression, this glacier´s annual mass balance variations since 1909. The reconstruction model captures 68 % of the observed glacier mass balance variability and shows three periods of sustained positive mass balances embedded in an overall negative trend totaling almost −42 m w.eq. over the past 105 years. The three periods of sustained positive mass balances (centered in the 1920s?1930s, in the 1980s and in the first decade of the 21st century) coincide with several documented glacier advances in this region. Similar trends observed in other shorter glacier mass balance series suggest the glaciar Echaurren Norte reconstruction is representative of larger-scale conditions and could be useful for more detailed glaciological, hydrological and climatological assessments in this portion of the Andes. |
| publishDate |
2015 |
| dc.date.none.fl_str_mv |
2015-09 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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http://hdl.handle.net/11336/69743 Masiokas, Mariano Hugo; Christie, D. A.; Le Quesne, C.; Pitte, Pedro Miguel; Ruiz, Lucas Ernesto; et al.; Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data; Copernicus Publications; The Cryosphere Discussions; 9; 5; 9-2015; 4949-4980 1994-0416 1994-0440 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/69743 |
| identifier_str_mv |
Masiokas, Mariano Hugo; Christie, D. A.; Le Quesne, C.; Pitte, Pedro Miguel; Ruiz, Lucas Ernesto; et al.; Reconstructing glacier mass balances in the Central Andes of Chile and Argentina using local and regional hydro-climatic data; Copernicus Publications; The Cryosphere Discussions; 9; 5; 9-2015; 4949-4980 1994-0416 1994-0440 CONICET Digital CONICET |
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eng |
| language |
eng |
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info:eu-repo/semantics/altIdentifier/doi/10.5194/tcd-9-4949-2015 info:eu-repo/semantics/altIdentifier/url/https://www.the-cryosphere.net/10/927/2016/tc-10-927-2016-discussion.html |
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