Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)

Autores
Vieira, Gonçalo; Baltakova, Ahinora; Batista, Vanesa; Bockheim, James; Caselli, Alberto Tomás; Catalão, João; Correia, Antonio; David, Ana; Ferreira, Alice; Hodson, Andrew; Goyanes, Gabriel Alejandro; Kenderova, Rositza; Mora, Carla; Neves, Mário; Nieuwendam, Alexandre; Nowak, Agnieszka; Oliva, Marc; de Pablo, Miguel Angel; Pimpirev, Christo; Prates, Gonçalo; Ramos, Miguel; Santos, Fernando; Schaefer, Carlos; Simas, Felipe
Año de publicación
2014
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
There are currently ci 75 GTN-P boreholes and 18 CALM sites in Antarctica, most of them installed during the IPY and still with a short data series. In the Antarctic Peninsula, only 6 boreholes are deeper than 10 m and 4 of them are maintained by the PERMANTAR team. Several new boreholes and CALM sites have been installed in a collaborative effort between Argentina, Brazil, Bulgaria, Portugal, Russia, Spain, Switzerland and the United States. Such an integrated approach, besides contributing to the installation of infrastructure, allowed for new advances on the permafrost thermal state (Vieira et al 2010, Bockheim et al 2013). It is now becoming clear that the Antarctic Peninsula, one of Earth´s regions where air temperature has increased the most in the last 60 years shows a very high sensitivity of permafrost to warming. In the South Shetlands, permafrost temperatures are just below freezing and permafrost degradation is prone to occur. Consequences in the terrestrial ecosystems are still unknown, but changes in hydrology, carbon storage and geomorphological dynamics are expected. The region is a key natural laboratory for understanding permafrost´s reaction to climate change and quite different to the Arctic, with the unique influence on physical and life processes of the Southern Ocean. P3 is taking place from May 2013 to April 2015 and focuses on maintaining and upgrading several GTN-P and CALM sites in the Antarctic Peninsula region, but also on contributing to new questions that developed from on-going work. In this sense, P3 is more than a monitoring project, but an integrated approach aiming at science deliverables dealing with Antarctic permafrost reaction to a changing climate. PERMANTAR´s scope is now enlarged to a latitudinal gradient from 61º to 65ºS in the western Antarctic Peninsula, where we aim at more than traditional focus on permafrost temperature monitoring. Variables linked to permafrost dynamics and modelling are approached in a more integrated way and using state-of-the-art techniques: snow cover dynamics from the local to the regional scale, active layer moisture content, ice-content at the transient layer and changing rates of geomorphic processes. P3 focusses on a set of target questions along the latitudinal gradient: 1) Where is the boundary between continuous and discontinuous permafrost 2) How does the climatic sensitivity of permafrost changes 3) What is the role of late lying snow patches at the continuous permafrost boundary 4) How does soil moisture varies seasonally in the active layer 5) How does ground-ice content occur in the transient layer 6) Can accurate terrain deformation rates be derived by means of DInSAR 7) Can key geomorphic units used as geo-indicators of climate change in the AP.This presentation synthesises the main contributions of the PERMANTAR team with new advances deriving from the Antarctic campaign of 2013-14.
Fil: Vieira, Gonçalo. Universidade Nova de Lisboa; Portugal
Fil: Baltakova, Ahinora. Bulgarian Antarctic Institute; Bulgaria
Fil: Batista, Vanesa. Universidade Nova de Lisboa; Portugal
Fil: Bockheim, James. University of Wisconsin; Estados Unidos
Fil: Caselli, Alberto Tomás. Universidade Nova de Lisboa; Portugal. Universidad Nacional de Rio Negro. Sede Alto Valle y Valle Medio.; Argentina
Fil: Catalão, João. Universidade Nova de Lisboa; Portugal
Fil: Correia, Antonio. Universidade Nova de Lisboa; Portugal
Fil: David, Ana. Universidade Nova de Lisboa; Portugal
Fil: Ferreira, Alice. Universidade Nova de Lisboa; Portugal
Fil: Hodson, Andrew. University of Sheffield;
Fil: Goyanes, Gabriel Alejandro. Ministerio de Relaciones Exteriores, Comercio Internacional y Culto. Direccion Nacional del Antártico; Argentina. 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
Fil: Kenderova, Rositza. Universidade Nova de Lisboa; Portugal
Fil: Mora, Carla. Universidade Nova de Lisboa; Portugal
Fil: Neves, Mário. Universidade Nova de Lisboa; Portugal
Fil: Nieuwendam, Alexandre. Universidade Nova de Lisboa; Portugal
Fil: Nowak, Agnieszka. University of Sheffield;
Fil: Oliva, Marc. Universidade Nova de Lisboa; Portugal
Fil: de Pablo, Miguel Angel. Universidad de Alcalá; España
Fil: Pimpirev, Christo. Bulgarian Antarctic Institute; Bulgaria
Fil: Prates, Gonçalo. Universidade Nova de Lisboa; Portugal
Fil: Ramos, Miguel. Universidad de Alcalá; España
Fil: Santos, Fernando. Universidade Nova de Lisboa; Portugal
Fil: Schaefer, Carlos. Universidade Federal de Viçosa; Brasil
Fil: Simas, Felipe. Universidade Federal de Viçosa; Brasil
4th European Conference on Permafrost
Évora
Portugal
Universidade de Lisboa
Universidade de Évora
Materia
PERMANTAR-3
PERMAFROST
CLIMATE CHANGE
ANTARCTIC PENINSULA
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/271702

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oai_identifier_str oai:ri.conicet.gov.ar:11336/271702
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)Vieira, GonçaloBaltakova, AhinoraBatista, VanesaBockheim, JamesCaselli, Alberto TomásCatalão, JoãoCorreia, AntonioDavid, AnaFerreira, AliceHodson, AndrewGoyanes, Gabriel AlejandroKenderova, RositzaMora, CarlaNeves, MárioNieuwendam, AlexandreNowak, AgnieszkaOliva, Marcde Pablo, Miguel AngelPimpirev, ChristoPrates, GonçaloRamos, MiguelSantos, FernandoSchaefer, CarlosSimas, FelipePERMANTAR-3PERMAFROSTCLIMATE CHANGEANTARCTIC PENINSULAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1There are currently ci 75 GTN-P boreholes and 18 CALM sites in Antarctica, most of them installed during the IPY and still with a short data series. In the Antarctic Peninsula, only 6 boreholes are deeper than 10 m and 4 of them are maintained by the PERMANTAR team. Several new boreholes and CALM sites have been installed in a collaborative effort between Argentina, Brazil, Bulgaria, Portugal, Russia, Spain, Switzerland and the United States. Such an integrated approach, besides contributing to the installation of infrastructure, allowed for new advances on the permafrost thermal state (Vieira et al 2010, Bockheim et al 2013). It is now becoming clear that the Antarctic Peninsula, one of Earth´s regions where air temperature has increased the most in the last 60 years shows a very high sensitivity of permafrost to warming. In the South Shetlands, permafrost temperatures are just below freezing and permafrost degradation is prone to occur. Consequences in the terrestrial ecosystems are still unknown, but changes in hydrology, carbon storage and geomorphological dynamics are expected. The region is a key natural laboratory for understanding permafrost´s reaction to climate change and quite different to the Arctic, with the unique influence on physical and life processes of the Southern Ocean. P3 is taking place from May 2013 to April 2015 and focuses on maintaining and upgrading several GTN-P and CALM sites in the Antarctic Peninsula region, but also on contributing to new questions that developed from on-going work. In this sense, P3 is more than a monitoring project, but an integrated approach aiming at science deliverables dealing with Antarctic permafrost reaction to a changing climate. PERMANTAR´s scope is now enlarged to a latitudinal gradient from 61º to 65ºS in the western Antarctic Peninsula, where we aim at more than traditional focus on permafrost temperature monitoring. Variables linked to permafrost dynamics and modelling are approached in a more integrated way and using state-of-the-art techniques: snow cover dynamics from the local to the regional scale, active layer moisture content, ice-content at the transient layer and changing rates of geomorphic processes. P3 focusses on a set of target questions along the latitudinal gradient: 1) Where is the boundary between continuous and discontinuous permafrost 2) How does the climatic sensitivity of permafrost changes 3) What is the role of late lying snow patches at the continuous permafrost boundary 4) How does soil moisture varies seasonally in the active layer 5) How does ground-ice content occur in the transient layer 6) Can accurate terrain deformation rates be derived by means of DInSAR 7) Can key geomorphic units used as geo-indicators of climate change in the AP.This presentation synthesises the main contributions of the PERMANTAR team with new advances deriving from the Antarctic campaign of 2013-14.Fil: Vieira, Gonçalo. Universidade Nova de Lisboa; PortugalFil: Baltakova, Ahinora. Bulgarian Antarctic Institute; BulgariaFil: Batista, Vanesa. Universidade Nova de Lisboa; PortugalFil: Bockheim, James. University of Wisconsin; Estados UnidosFil: Caselli, Alberto Tomás. Universidade Nova de Lisboa; Portugal. Universidad Nacional de Rio Negro. Sede Alto Valle y Valle Medio.; ArgentinaFil: Catalão, João. Universidade Nova de Lisboa; PortugalFil: Correia, Antonio. Universidade Nova de Lisboa; PortugalFil: David, Ana. Universidade Nova de Lisboa; PortugalFil: Ferreira, Alice. Universidade Nova de Lisboa; PortugalFil: Hodson, Andrew. University of Sheffield;Fil: Goyanes, Gabriel Alejandro. Ministerio de Relaciones Exteriores, Comercio Internacional y Culto. Direccion Nacional del Antártico; Argentina. 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"; ArgentinaFil: Kenderova, Rositza. Universidade Nova de Lisboa; PortugalFil: Mora, Carla. Universidade Nova de Lisboa; PortugalFil: Neves, Mário. Universidade Nova de Lisboa; PortugalFil: Nieuwendam, Alexandre. Universidade Nova de Lisboa; PortugalFil: Nowak, Agnieszka. University of Sheffield;Fil: Oliva, Marc. Universidade Nova de Lisboa; PortugalFil: de Pablo, Miguel Angel. Universidad de Alcalá; EspañaFil: Pimpirev, Christo. Bulgarian Antarctic Institute; BulgariaFil: Prates, Gonçalo. Universidade Nova de Lisboa; PortugalFil: Ramos, Miguel. Universidad de Alcalá; EspañaFil: Santos, Fernando. Universidade Nova de Lisboa; PortugalFil: Schaefer, Carlos. Universidade Federal de Viçosa; BrasilFil: Simas, Felipe. Universidade Federal de Viçosa; Brasil4th European Conference on PermafrostÉvoraPortugalUniversidade de LisboaUniversidade de ÉvoraUniversidade de Lisboa2014info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectConferenciaBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/271702Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3); 4th European Conference on Permafrost; Évora; Portugal; 2014; 478-479CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://epic.awi.de/id/eprint/39543/1/2014_EUCOP4_Book_of_Abstracts.pdfInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:33:35Zoai:ri.conicet.gov.ar:11336/271702instacron: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 09:33:35.418CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
title Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
spellingShingle Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
Vieira, Gonçalo
PERMANTAR-3
PERMAFROST
CLIMATE CHANGE
ANTARCTIC PENINSULA
title_short Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
title_full Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
title_fullStr Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
title_full_unstemmed Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
title_sort Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3)
dc.creator.none.fl_str_mv Vieira, Gonçalo
Baltakova, Ahinora
Batista, Vanesa
Bockheim, James
Caselli, Alberto Tomás
Catalão, João
Correia, Antonio
David, Ana
Ferreira, Alice
Hodson, Andrew
Goyanes, Gabriel Alejandro
Kenderova, Rositza
Mora, Carla
Neves, Mário
Nieuwendam, Alexandre
Nowak, Agnieszka
Oliva, Marc
de Pablo, Miguel Angel
Pimpirev, Christo
Prates, Gonçalo
Ramos, Miguel
Santos, Fernando
Schaefer, Carlos
Simas, Felipe
author Vieira, Gonçalo
author_facet Vieira, Gonçalo
Baltakova, Ahinora
Batista, Vanesa
Bockheim, James
Caselli, Alberto Tomás
Catalão, João
Correia, Antonio
David, Ana
Ferreira, Alice
Hodson, Andrew
Goyanes, Gabriel Alejandro
Kenderova, Rositza
Mora, Carla
Neves, Mário
Nieuwendam, Alexandre
Nowak, Agnieszka
Oliva, Marc
de Pablo, Miguel Angel
Pimpirev, Christo
Prates, Gonçalo
Ramos, Miguel
Santos, Fernando
Schaefer, Carlos
Simas, Felipe
author_role author
author2 Baltakova, Ahinora
Batista, Vanesa
Bockheim, James
Caselli, Alberto Tomás
Catalão, João
Correia, Antonio
David, Ana
Ferreira, Alice
Hodson, Andrew
Goyanes, Gabriel Alejandro
Kenderova, Rositza
Mora, Carla
Neves, Mário
Nieuwendam, Alexandre
Nowak, Agnieszka
Oliva, Marc
de Pablo, Miguel Angel
Pimpirev, Christo
Prates, Gonçalo
Ramos, Miguel
Santos, Fernando
Schaefer, Carlos
Simas, Felipe
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv PERMANTAR-3
PERMAFROST
CLIMATE CHANGE
ANTARCTIC PENINSULA
topic PERMANTAR-3
PERMAFROST
CLIMATE CHANGE
ANTARCTIC PENINSULA
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv There are currently ci 75 GTN-P boreholes and 18 CALM sites in Antarctica, most of them installed during the IPY and still with a short data series. In the Antarctic Peninsula, only 6 boreholes are deeper than 10 m and 4 of them are maintained by the PERMANTAR team. Several new boreholes and CALM sites have been installed in a collaborative effort between Argentina, Brazil, Bulgaria, Portugal, Russia, Spain, Switzerland and the United States. Such an integrated approach, besides contributing to the installation of infrastructure, allowed for new advances on the permafrost thermal state (Vieira et al 2010, Bockheim et al 2013). It is now becoming clear that the Antarctic Peninsula, one of Earth´s regions where air temperature has increased the most in the last 60 years shows a very high sensitivity of permafrost to warming. In the South Shetlands, permafrost temperatures are just below freezing and permafrost degradation is prone to occur. Consequences in the terrestrial ecosystems are still unknown, but changes in hydrology, carbon storage and geomorphological dynamics are expected. The region is a key natural laboratory for understanding permafrost´s reaction to climate change and quite different to the Arctic, with the unique influence on physical and life processes of the Southern Ocean. P3 is taking place from May 2013 to April 2015 and focuses on maintaining and upgrading several GTN-P and CALM sites in the Antarctic Peninsula region, but also on contributing to new questions that developed from on-going work. In this sense, P3 is more than a monitoring project, but an integrated approach aiming at science deliverables dealing with Antarctic permafrost reaction to a changing climate. PERMANTAR´s scope is now enlarged to a latitudinal gradient from 61º to 65ºS in the western Antarctic Peninsula, where we aim at more than traditional focus on permafrost temperature monitoring. Variables linked to permafrost dynamics and modelling are approached in a more integrated way and using state-of-the-art techniques: snow cover dynamics from the local to the regional scale, active layer moisture content, ice-content at the transient layer and changing rates of geomorphic processes. P3 focusses on a set of target questions along the latitudinal gradient: 1) Where is the boundary between continuous and discontinuous permafrost 2) How does the climatic sensitivity of permafrost changes 3) What is the role of late lying snow patches at the continuous permafrost boundary 4) How does soil moisture varies seasonally in the active layer 5) How does ground-ice content occur in the transient layer 6) Can accurate terrain deformation rates be derived by means of DInSAR 7) Can key geomorphic units used as geo-indicators of climate change in the AP.This presentation synthesises the main contributions of the PERMANTAR team with new advances deriving from the Antarctic campaign of 2013-14.
Fil: Vieira, Gonçalo. Universidade Nova de Lisboa; Portugal
Fil: Baltakova, Ahinora. Bulgarian Antarctic Institute; Bulgaria
Fil: Batista, Vanesa. Universidade Nova de Lisboa; Portugal
Fil: Bockheim, James. University of Wisconsin; Estados Unidos
Fil: Caselli, Alberto Tomás. Universidade Nova de Lisboa; Portugal. Universidad Nacional de Rio Negro. Sede Alto Valle y Valle Medio.; Argentina
Fil: Catalão, João. Universidade Nova de Lisboa; Portugal
Fil: Correia, Antonio. Universidade Nova de Lisboa; Portugal
Fil: David, Ana. Universidade Nova de Lisboa; Portugal
Fil: Ferreira, Alice. Universidade Nova de Lisboa; Portugal
Fil: Hodson, Andrew. University of Sheffield;
Fil: Goyanes, Gabriel Alejandro. Ministerio de Relaciones Exteriores, Comercio Internacional y Culto. Direccion Nacional del Antártico; Argentina. 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
Fil: Kenderova, Rositza. Universidade Nova de Lisboa; Portugal
Fil: Mora, Carla. Universidade Nova de Lisboa; Portugal
Fil: Neves, Mário. Universidade Nova de Lisboa; Portugal
Fil: Nieuwendam, Alexandre. Universidade Nova de Lisboa; Portugal
Fil: Nowak, Agnieszka. University of Sheffield;
Fil: Oliva, Marc. Universidade Nova de Lisboa; Portugal
Fil: de Pablo, Miguel Angel. Universidad de Alcalá; España
Fil: Pimpirev, Christo. Bulgarian Antarctic Institute; Bulgaria
Fil: Prates, Gonçalo. Universidade Nova de Lisboa; Portugal
Fil: Ramos, Miguel. Universidad de Alcalá; España
Fil: Santos, Fernando. Universidade Nova de Lisboa; Portugal
Fil: Schaefer, Carlos. Universidade Federal de Viçosa; Brasil
Fil: Simas, Felipe. Universidade Federal de Viçosa; Brasil
4th European Conference on Permafrost
Évora
Portugal
Universidade de Lisboa
Universidade de Évora
description There are currently ci 75 GTN-P boreholes and 18 CALM sites in Antarctica, most of them installed during the IPY and still with a short data series. In the Antarctic Peninsula, only 6 boreholes are deeper than 10 m and 4 of them are maintained by the PERMANTAR team. Several new boreholes and CALM sites have been installed in a collaborative effort between Argentina, Brazil, Bulgaria, Portugal, Russia, Spain, Switzerland and the United States. Such an integrated approach, besides contributing to the installation of infrastructure, allowed for new advances on the permafrost thermal state (Vieira et al 2010, Bockheim et al 2013). It is now becoming clear that the Antarctic Peninsula, one of Earth´s regions where air temperature has increased the most in the last 60 years shows a very high sensitivity of permafrost to warming. In the South Shetlands, permafrost temperatures are just below freezing and permafrost degradation is prone to occur. Consequences in the terrestrial ecosystems are still unknown, but changes in hydrology, carbon storage and geomorphological dynamics are expected. The region is a key natural laboratory for understanding permafrost´s reaction to climate change and quite different to the Arctic, with the unique influence on physical and life processes of the Southern Ocean. P3 is taking place from May 2013 to April 2015 and focuses on maintaining and upgrading several GTN-P and CALM sites in the Antarctic Peninsula region, but also on contributing to new questions that developed from on-going work. In this sense, P3 is more than a monitoring project, but an integrated approach aiming at science deliverables dealing with Antarctic permafrost reaction to a changing climate. PERMANTAR´s scope is now enlarged to a latitudinal gradient from 61º to 65ºS in the western Antarctic Peninsula, where we aim at more than traditional focus on permafrost temperature monitoring. Variables linked to permafrost dynamics and modelling are approached in a more integrated way and using state-of-the-art techniques: snow cover dynamics from the local to the regional scale, active layer moisture content, ice-content at the transient layer and changing rates of geomorphic processes. P3 focusses on a set of target questions along the latitudinal gradient: 1) Where is the boundary between continuous and discontinuous permafrost 2) How does the climatic sensitivity of permafrost changes 3) What is the role of late lying snow patches at the continuous permafrost boundary 4) How does soil moisture varies seasonally in the active layer 5) How does ground-ice content occur in the transient layer 6) Can accurate terrain deformation rates be derived by means of DInSAR 7) Can key geomorphic units used as geo-indicators of climate change in the AP.This presentation synthesises the main contributions of the PERMANTAR team with new advances deriving from the Antarctic campaign of 2013-14.
publishDate 2014
dc.date.none.fl_str_mv 2014
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Conferencia
Book
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/271702
Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3); 4th European Conference on Permafrost; Évora; Portugal; 2014; 478-479
CONICET Digital
CONICET
url http://hdl.handle.net/11336/271702
identifier_str_mv Permafrost and climate change in the Antarctic Peninsula region (PERMANTAR-3); 4th European Conference on Permafrost; Évora; Portugal; 2014; 478-479
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://epic.awi.de/id/eprint/39543/1/2014_EUCOP4_Book_of_Abstracts.pdf
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
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dc.publisher.none.fl_str_mv Universidade de Lisboa
publisher.none.fl_str_mv Universidade de Lisboa
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
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reponame_str CONICET Digital (CONICET)
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instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
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