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Carbajal, Fabricio Joaquin  
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García, Sebastián E.  
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Vigide, Nicolás Carlos  
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Badi, Gabriela  
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Agusto, Mariano Roberto  
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Lamberti, María Clara Isabel  
dc.date.available
2025-05-20T08:31:15Z  
dc.date.issued
2023  
dc.identifier.citation
Variations of Copahue Volcano Crater Lake and its Relation with Gas and Ash Emission During 2019-2021; IAVCEI Scientific Assembly 2023 ; Rotoura; Nueva Zelanda; 2023; 1-1  
dc.identifier.uri
http://hdl.handle.net/11336/262027  
dc.description.abstract
Copahue volcano is located on the international border between Argentina and Chile. It is monitored by the “OAVV” (SEGEMAR, Argentina) and “OVDAS” (SERNAGEOMIN, Chile). Copahue´s lastest and ongoing eruptive cycle initiated in 2012. During 2019-2021, periodic vapor-gases and ash emissions were emitted through the crater, and the hot, acidic crater-lake (CL) presented a significant area variation, in some cases being completely dried. In this work, a correlation between SO2 emissions and changes in the active crater dynamics for the last 3 years is presented. CL area analysis were carried out between 2018-2021, using 3.7 m of resolution satellite images (http://www.planet.com). Additionally, SO2 emissions were studied through the GEE (Google Earth Engine) web platform and contrasted with average flux data from DOAS equipment. Both satellite and ground-based measurements were correlated for the maximum SO2 emission during 2019-2021. Satellite images and meteorological data were integrated, observing a gradual variation in the CL area for the period, reaching maximum values up to 60000 m2, also observing a seasonal component. During 2020 and 2021 winters, maximum SO2 values (up 14000 t/d or day with DOAS and 0,7 Dobson units with GEE) and ash-clouds heights (1700m acl) were identified together with the disappearance of the CL. In addition, an increase in seismic tremor activity was registered for the same time span.This correlation of events allows us to hypothesize: i) during the colder months, the ambient temperature prevents the defrosting that feeds the shallower hydrothermal system, favoring evaporation and decrease of the CL, and consequently, ii) the CL brine generates a shallow chemical seal, from which gases and ash are emitted when the system reaches critical pressure, consistent with the increase in tremor activity. In summary, the activity of the Copahue CL during the 2019-2021 period suggests a seasonal control for gas and ash emissions.  
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application/pdf  
dc.language.iso
eng  
dc.publisher
International Association of Volcanology and Chemistry of the Earth's Interior  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
COPAHUE  
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VOLCANO  
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CRATER LAKE  
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ASH EMISSION  
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Vulcanología  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Variations of Copahue Volcano Crater Lake and its Relation with Gas and Ash Emission During 2019-2021  
dc.type
info:eu-repo/semantics/publishedVersion  
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info:eu-repo/semantics/conferenceObject  
dc.type
info:ar-repo/semantics/documento de conferencia  
dc.date.updated
2025-03-31T15:58:01Z  
dc.journal.pagination
1-1  
dc.journal.pais
Alemania  
dc.journal.ciudad
Springer  
dc.description.fil
Fil: Carbajal, Fabricio Joaquin. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina  
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Fil: García, Sebastián E.. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina  
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Fil: Vigide, Nicolás Carlos. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
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Fil: Badi, Gabriela. Secretaría de Industria y Minería. Servicio Geológico Minero Argentino; Argentina  
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Fil: Agusto, Mariano Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas. Grupo de Estudio y Seguimiento de Volcanes Activos; Argentina  
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Fil: Lamberti, María Clara Isabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas. Grupo de Estudio y Seguimiento de Volcanes Activos; Argentina  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.iavceivolcano.org/content/uploads/2021/03/iavcei-2023-book-of-abstracts.pdf  
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Autor  
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Internacional  
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Congreso  
dc.description.nombreEvento
IAVCEI Scientific Assembly 2023  
dc.date.evento
2023-01-30  
dc.description.ciudadEvento
Rotoura  
dc.description.paisEvento
Nueva Zelanda  
dc.type.publicacion
Book  
dc.description.institucionOrganizadora
International Association of Volcanology and Chemistry of the Earth's Interior  
dc.source.libro
Book of abstracts: IAVCEI Scientific Assembly 2023  
dc.date.eventoHasta
2023-02-03  
dc.type
Congreso