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dc.contributor.authorCorreia, Tamíres Partélli-
dc.date.accessioned2025-05-20T16:01:51Z-
dc.date.available2025-05-20T16:01:51Z-
dc.date.issued2020-
dc.identifier.citationCORREIA, Tamires Partélli. Tendência temporal e regime hidrotérmico da camada ativa do permafrost na Antártica, e sua relação com os eventos climáticos de grande escala. 2020. 164 f. Tese (Doutorado em Ciências Ambientais e Florestais) - Instituto de Florestas, Universidade Federal Rural do Rio de Janeiro, Seropédica, 2020.pt_BR
dc.identifier.urihttps://rima.ufrrj.br/jspui/handle/20.500.14407/21834-
dc.description.abstractO permafrost, juntamente com a camada ativa, são um dos componentes mais importantes da criosfera. Neste contexto, o objetivo geral deste estudo, foi analisar a tendência temporal de seis sítios de monitoramento hidrotermal localizados na Antártica Marítima e Peninsular. Além de avaliar minuciosamente, o regime hidrotérmico dos solos desses sítios e de verificar as correlações, entre eventos climáticos de grande escala e as temperaturas do solo. Para tendência temporal, utilizou-se o método de Mann-Kendall, mas com abordagens diferentes em cada capítulo. A espessura da camada ativa (ALT), foi estimada de acordo com a temperatura máxima mensal ao atingir 0 °C. O ENSO (El Niño - Oscilação Sul) e AAO (Índice de Oscilação Antártica), foram escolhidos para gerar as correlações (Spearman), entre os eventos climáticos de grande escala e o regime térmico do solo. No capítulo 1, foi possível utilizar dados de neve e precipitação pluvial, para subsidiar hipóteses sobre o regime hídrico do solo. A dinâmica da camada ativa e o regime térmico, foram influenciados pelos efeitos locais de cada sítio, como em Deception, com bastante influência das atividades geotérmicas. Destaca- se o estado isotérmico, como processo marcante, com sentido crescente em profundidade nos sítios de Fildes, Low Head, Deception e Hope Bay, no verão, outono e inverno. De forma geral, os seis sítios apresentaram tendências nas diferentes escalas analisadas. A espessura média da camada ativa, foi de 92,6 cm (Fildes), 115,6 cm (Low Head), 88,3 cm (Deception), 142,7 cm (Hope Bay), e 94,2 (Seymour). A umidade e a textura do solo, também exerceram controle sobre os períodos de congelamento e descongelamento, na intensificação do efeito de cortina zero e na transmissão de energia no perfil do solo. As séries temporais, foram bem correlacionadas com o ENSO e AAO. Com maior intensidade, pelo forte El Niño (2015/2016), e La Niña de classe moderada em 2011, com ocorrência de invernos rigorosos e verões muito quentes, com efeito também no ponto de mudança brusca da reta de tendência.pt_BR
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESpt_BR
dc.languageporpt_BR
dc.publisherUniversidade Federal Rural do Rio de Janeiropt_BR
dc.subjecttemperatura do solopt_BR
dc.subjecttemperatura do arpt_BR
dc.subjecttendência temporalpt_BR
dc.subjectumidade do solopt_BR
dc.subjectpermafrostpt_BR
dc.subjectcamada ativapt_BR
dc.subjectmodos climáticospt_BR
dc.subjectsoil temperaturept_BR
dc.subjectair temperaturept_BR
dc.subjecttemporal trendpt_BR
dc.subjectsoil moisturept_BR
dc.subjectpermafrostpt_BR
dc.subjectactive layerpt_BR
dc.subjectclimatic modespt_BR
dc.titleTendência temporal e regime hidrotérmico da camada ativa do permafrost na Antártica, e sua relação com os eventos climáticos de grande escalapt_BR
dc.title.alternativeTemporal trend and hydrothermal regime of the active layer of permafrost in Antarctica, and its relationship with large scale climatic eventsen
dc.typeTesept_BR
dc.description.abstractOtherPermafrost, together with the active layer, are one of the most important components of the cryosphere. In this context, the general objective of this study was to analyze the temporal trend of six hydrothermal monitoring sites located in the Antarctic Maritime and Peninsular. In addition to thoroughly assessing the hydrothermal regime of the soils in these sites and verifying the correlations between large scale climatic events and soil temperatures. For temporal trends, the Mann-Kendall method was used, but with different approaches in each chapter. The Active Layer Thickness (ALT) was estimated according to the maximum monthly temperature when reaching 0 ° C. ENSO (El Niño - South Oscillation) and AAO (Antarctic Oscillation Index) were chosen to generate the correlations (Spearman), between large scale climatic events and the thermal regime of the soil. In chapter 1, it was possible to use snow and rainfall data to support hypotheses about the soil water regime. The dynamics of the active layer and the thermal regime were influenced by the local effects of each site, as in Deception, with a lot of influence from geothermal activities. The isothermal state stands out as a remarkable process, with a growing sense of depth at the sites of Fildes, Low Head, Deception and Hope Bay, in summer, autumn and winter. In general, the six sites showed trends at the different scales analyzed. The average thickness of the active layer was 92.6 cm (Fildes), 115.6 cm (Low Head), 88.3 cm (Deception), 142.7 cm (Hope Bay), and 94.2 (Seymour). The moisture and texture of the soil also exercised control over the periods of freezing and thawing, in intensifying the effect zero curtain and in the transmission of energy in the soil profile. The time series, were well correlated with ENSO and AAO. With greater intensity, by the strong El Niño (2015/2016), and La Niña of moderate class in 2011, with the occurrence of harsh winters and very hot summers, with effect also at the point of abrupt change of the trend line.en
dc.contributor.advisor1Francelino, Marcio Rocha-
dc.contributor.advisor1IDhttps://orcid.org/0000-0001-8837-1372pt_BR
dc.contributor.advisor1Latteshttp://lattes.cnpq.br/1335748426615308pt_BR
dc.contributor.advisor-co1Veloso, Gustavo Vieira-
dc.contributor.advisor-co1IDhttps://orcid.org/0000-0002-9451-2714pt_BR
dc.contributor.advisor-co1Latteshttp://lattes.cnpq.br/5446388671333942pt_BR
dc.contributor.advisor-co2Michel, Roberto Ferreira Machado-
dc.contributor.advisor-co2IDhttps://orcid.org/0000-0001-5951-4610pt_BR
dc.contributor.advisor-co2Latteshttp://lattes.cnpq.br/9952967245812027pt_BR
dc.contributor.referee1Francelino, Marcio Rocha-
dc.contributor.referee1IDhttps://orcid.org/0000-0001-8837-1372pt_BR
dc.contributor.referee1Latteshttp://lattes.cnpq.br/1335748426615308pt_BR
dc.contributor.referee2Schaefer, Carlos Ernesto Gonçalves Reynaud-
dc.contributor.referee2Latteshttp://lattes.cnpq.br/0904177542323793pt_BR
dc.contributor.referee3Fernandes Filho, Elpidio Inacio-
dc.contributor.referee3IDhttps://orcid.org/0000-0002-9484-1411pt_BR
dc.contributor.referee3Latteshttp://lattes.cnpq.br/9848935150180973pt_BR
dc.contributor.referee4Justino, Flávio Barbosa-
dc.contributor.referee4IDhttps://orcid.org/0000-0003-0929-1388pt_BR
dc.contributor.referee4Latteshttp://lattes.cnpq.br/3675336131283739pt_BR
dc.contributor.referee5Lyra, Gustavo Bastos-
dc.contributor.referee5IDhttps://orcid.org/0000-0002-9882-7000pt_BR
dc.contributor.referee5Latteshttp://lattes.cnpq.br/2677800541601144pt_BR
dc.creator.IDhttps://orcid.org/0000-0002-1303-8273pt_BR
dc.creator.Latteshttp://lattes.cnpq.br/7902863199631787pt_BR
dc.publisher.countryBrasilpt_BR
dc.publisher.departmentInstituto de Florestaspt_BR
dc.publisher.initialsUFRRJpt_BR
dc.publisher.programPrograma de Pós-Graduação em Ciências Ambientais e Florestaispt_BR
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