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Permafrost and periglacial research in Antarctica: new results and perspectives

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Resumo:In the last two years the research within the Antarctic Permafrost, Periglacial Environments and Soils (ANTPAS) Expert Group of the Scientific Committee on Antarctic Research (SCAR) andWorking Group of the International Permafrost Association (IPA) provided newresults on the dynamics of periglacial environments both inMaritime and Continental Antarctica. In continental Antarctica despite the absence of air warming, in the last 15 years an active layer thickening and acceleration of permafrost degradation erosional phenomena were reported, these beingmainly related to the increase of solar radiation. On the other hand, inMaritime Antarctica,with a dramatic airwarming, permafrost degradation has been observed, but the role of snowcover on the ground energy balance and consequently on permafrost and active layer has been underlined. Moreover, many contributions on the knowledge on the characteristics of the Antarctic soils were carried out in several areas along a wide latitudinal range.
Autores principais:Guglielmin, Mauro
Outros Autores:Vieira, Goncalo
Assunto:Antarctica permafrost active layer soils
Ano:2014
País:Portugal
Tipo de documento:artigo
Tipo de acesso:acesso restrito
Instituição associada:Universidade de Lisboa
Idioma:inglês
Origem:Repositório da Universidade de Lisboa
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author Guglielmin, Mauro
author2 Vieira, Goncalo
author2_role author
author_facet Guglielmin, Mauro
Vieira, Goncalo
author_role author
contributor_name_str_mv Repositório Científico de Acesso Aberto da ULisboa
country_str PT
creators_json_txt [{\"Person.name\":\"Guglielmin, Mauro\"},{\"Person.name\":\"Vieira, Goncalo\",\"Person.identifier.orcid\":\"0000-0001-7611-3464\"}]
datacite.contributors.contributor.contributorName.fl_str_mv Repositório Científico de Acesso Aberto da ULisboa
datacite.creators.creator.creatorName.fl_str_mv Guglielmin, Mauro
Vieira, Goncalo
datacite.date.Accepted.fl_str_mv 2014-01-01T00:00:00Z
datacite.date.available.fl_str_mv 2017-03-17T13:24:01Z
datacite.date.embargoed.fl_str_mv 2017-03-17T13:24:01Z
datacite.rights.fl_str_mv http://purl.org/coar/access_right/c_16ec
datacite.subjects.subject.fl_str_mv Antarctica
permafrost
active layer
soils
datacite.titles.title.fl_str_mv Permafrost and periglacial research in Antarctica: new results and perspectives
dc.contributor.none.fl_str_mv Repositório Científico de Acesso Aberto da ULisboa
dc.creator.none.fl_str_mv Guglielmin, Mauro
Vieira, Goncalo
dc.date.Accepted.fl_str_mv 2014-01-01T00:00:00Z
dc.date.available.fl_str_mv 2017-03-17T13:24:01Z
dc.date.embargoed.fl_str_mv 2017-03-17T13:24:01Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv http://hdl.handle.net/10451/27208
dc.language.none.fl_str_mv eng
dc.publisher.none.fl_str_mv Elsevier
dc.rights.none.fl_str_mv http://purl.org/coar/access_right/c_16ec
dc.subject.none.fl_str_mv Antarctica
permafrost
active layer
soils
dc.title.fl_str_mv Permafrost and periglacial research in Antarctica: new results and perspectives
dc.type.none.fl_str_mv http://purl.org/coar/resource_type/c_6501
description In the last two years the research within the Antarctic Permafrost, Periglacial Environments and Soils (ANTPAS) Expert Group of the Scientific Committee on Antarctic Research (SCAR) andWorking Group of the International Permafrost Association (IPA) provided newresults on the dynamics of periglacial environments both inMaritime and Continental Antarctica. In continental Antarctica despite the absence of air warming, in the last 15 years an active layer thickening and acceleration of permafrost degradation erosional phenomena were reported, these beingmainly related to the increase of solar radiation. On the other hand, inMaritime Antarctica,with a dramatic airwarming, permafrost degradation has been observed, but the role of snowcover on the ground energy balance and consequently on permafrost and active layer has been underlined. Moreover, many contributions on the knowledge on the characteristics of the Antarctic soils were carried out in several areas along a wide latitudinal range.
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eu_rights_str_mv restrictedAccess
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id ul_fedca9a8d013e01980931ebfac8efa4a
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language eng
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oai_identifier_str oai:repositorio.ulisboa.pt:10451/27208
organization_str_mv urn:organizationAcronym:ul
person_str_mv Guglielmin, Mauro
Vieira, Goncalo
Vieira, Goncalo
https://www.ciencia-id.pt/2519-6583-CAEA
2519-6583-CAEA
http://orcid.org/0000-0001-7611-3464
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publishDate 2014
publisher.none.fl_str_mv Elsevier
reponame_str Repositório da Universidade de Lisboa
repository_id_str urn:repositoryAcronym:ul
service_str_mv urn:repositoryAcronym:ul
spelling engElsevierpt_PTIn the last two years the research within the Antarctic Permafrost, Periglacial Environments and Soils (ANTPAS) Expert Group of the Scientific Committee on Antarctic Research (SCAR) andWorking Group of the International Permafrost Association (IPA) provided newresults on the dynamics of periglacial environments both inMaritime and Continental Antarctica. In continental Antarctica despite the absence of air warming, in the last 15 years an active layer thickening and acceleration of permafrost degradation erosional phenomena were reported, these beingmainly related to the increase of solar radiation. On the other hand, inMaritime Antarctica,with a dramatic airwarming, permafrost degradation has been observed, but the role of snowcover on the ground energy balance and consequently on permafrost and active layer has been underlined. Moreover, many contributions on the knowledge on the characteristics of the Antarctic soils were carried out in several areas along a wide latitudinal range.application/pdfpt_PTPermafrost and periglacial research in Antarctica: new results and perspectivesGuglielmin, MauroPersonalVieira, GoncaloDSpacehttp://dspace.org/items/7039fbb2-e1f8-4c3e-80f1-603b12d33c1cDSpacehttp://dspace.org/items/7039fbb2-e1f8-4c3e-80f1-603b12d33c1cBrito Guapo Teles VieiraGonçaloCiência IDhttps://www.ciencia-id.pt2519-6583-CAEAORCIDhttp://orcid.org0000-0001-7611-3464Scopus Author IDhttps://www.scopus.com7005863976HostingInstitutionOrganizationalRepositório Científico de Acesso Aberto da ULisboae-mailmailto:repositorio@reitoria.ulisboa.ptrepositorio@reitoria.ulisboa.ptISSNIsPartOf0169-555XDOIIsPartOf10.1016/j.geomorph.2014.04.0052017-03-17T13:24:01Z20142014-01-01T00:00:00ZHandlehttp://hdl.handle.net/10451/27208http://purl.org/coar/access_right/c_16ecrestricted accessAntarcticapermafrostactive layersoils201296 bytesliteraturehttp://purl.org/coar/resource_type/c_6501journal articlehttp://purl.org/coar/access_right/c_16ecapplication/pdffulltexthttps://repositorio.ulisboa.pt/bitstreams/33512ee8-6e40-4de8-89a4-e53c35e1ab68/downloadGeomorphology22513Amsterdam
spellingShingle Permafrost and periglacial research in Antarctica: new results and perspectives
Guglielmin, Mauro
Antarctica
permafrost
active layer
soils
status SINGLETON
subject.fl_str_mv Antarctica
permafrost
active layer
soils
title Permafrost and periglacial research in Antarctica: new results and perspectives
title_full Permafrost and periglacial research in Antarctica: new results and perspectives
title_fullStr Permafrost and periglacial research in Antarctica: new results and perspectives
title_full_unstemmed Permafrost and periglacial research in Antarctica: new results and perspectives
title_short Permafrost and periglacial research in Antarctica: new results and perspectives
title_sort Permafrost and periglacial research in Antarctica: new results and perspectives
topic Antarctica
permafrost
active layer
soils
topic_facet Antarctica
permafrost
active layer
soils
url http://hdl.handle.net/10451/27208
visible 1