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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/271702
Ver los metadatos del registro completo
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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 |
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info:eu-repo/semantics/altIdentifier/url/https://epic.awi.de/id/eprint/39543/1/2014_EUCOP4_Book_of_Abstracts.pdf |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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Universidade de Lisboa |
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Universidade de Lisboa |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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