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	Provedor de dados ArchiMer (2) Autor Barton, Benjamin I. (1) Hamon, Mathieu (1) Lenn, Yueng‐djern (1) Lique, Camille (1) Palavra-chave Freshwater content (2) Heat content (2) Arctic Ocean (1) Biais XBT (1) Contenu d’eau douce (1) Contenu thermique (1) Field reconstruction (1) Global warming (1) In situ measurement (1) Observations in situ (1) Reconstruction de champs (1) Réchauffement climatique (1) Satellite (1) Steric height (1) XBT bias (1) Mais... Tipo do documento Text (2) Ano 2020 (1) 2012 (1) País France (2) Idioma Francês (1) Inglês (1)		Ordenar por:  Relevância Autor Título Ano Registros recuperados: 2 Primeira ... 1 ... Última Caractérisation des effets du réchauffement climatique sur l'océan superficiel au cours des 50 dernières années ArchiMer Hamon, Mathieu. To identify and characterize the effects of global warming is one of the major scientific challenges of this new century. The rise of sea level, the hydrological changes are some consequences of this phenomenon which will influence all forms of life on Earth. Due to its high thermal capacity, it is estimated that 84% of the energy developed by global warming is stored in the first layers of the ocean. However, it is rather difficult to assess its overall impact over the last 50 years because the ocean is not warming uniformly and the inhomogeneous sampling (spatial and temporal) of oceanographic observations, instrumental errors (XBT) and biases related to the estimation process of global indicators can affect our assessment of the evolution of ocean... Tipo: Text Palavras-chave: Réchauffement climatique; Observations in situ; Biais XBT; Reconstruction de champs; Contenu thermique; Contenu d’eau douce; Global warming; In situ measurement; XBT bias; Field reconstruction; Heat content; Freshwater content. Ano: 2012 URL: https://archimer.ifremer.fr/doc/00498/60957/64360.pdf Water mass properties derived from satellite observations in the Barents Sea ArchiMer Barton, Benjamin I.; Lique, Camille; Lenn, Yueng‐djern. The Barents Sea is a region of deep water formation where Atlantic Water is converted into cooler, fresher Barents Sea Water. Barents Sea Water properties exhibit variability at seasonal, interannual and decadal timescales. This variability is transferred to Arctic Intermediate Water, which eventually contributes to the deeper branch of the Atlantic Meridional Overturning Circulation. Variations in Barents Sea Water properties are reflected in steric height (contribution of density to sea level variations) that depends on heat and freshwater content, and is a quantity usually derived from in situ observations of water temperature, salinity and pressure that remain sparse during winter in the Barents Sea. This analysis explores the utility of satellite... Tipo: Text Palavras-chave: Satellite; Steric height; Freshwater content; Heat content; Arctic Ocean. Ano: 2020 URL: https://archimer.ifremer.fr/doc/00634/74651/74556.pdf Registros recuperados: 2 Primeira ... 1 ... Última

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