OS - Latest Articleshttp://www.ocean-sci.net/2010-03-08T07:20:32+01:00Copernicus Electronic Production Support Officehttp://www.ocean-sci.net/6/345/2010/Malvinas-slope water intrusions on the northern Patagonia continental shelfMalvinas-slope water intrusions on the northern Patagonia continental shelf, A. R. Piola, N. Martínez Avellaneda, R. A. Guerrero, F. P. Jardón, E. D. Palma, and S. I. Romero, Ocean Science, 6, 345-359, 2010Copernicus Electronic Production Support Office2010-03-08T00:00:00+01:002010-03-08T00:00:00+01:00http://www.ocean-sci.net/6/331/2010/Mediterranean intermediate circulation estimated from Argo data in 2003–2010Mediterranean intermediate circulation estimated from Argo data in 2003–2010, M. Menna and P. M. Poulain, Ocean Science, 6, 331-343, 2010Copernicus Electronic Production Support Office2010-03-03T00:00:00+01:002010-03-03T00:00:00+01:00http://www.ocean-sci.net/6/311/2010/Seasonal variability of the Caspian Sea three-dimensional circulation, sea level and air-sea interactionSeasonal variability of the Caspian Sea three-dimensional circulation, sea level and air-sea interaction, R. A. Ibrayev, E. Özsoy, C. Schrum, and H. İ. Sur, Ocean Science, 6, 311-329, 2010Copernicus Electronic Production Support Office2010-03-03T00:00:00+01:002010-03-03T00:00:00+01:00http://www.ocean-sci.net/6/301/2010/Entrainment in the Denmark Strait overflow plume by meso-scale eddiesEntrainment in the Denmark Strait overflow plume by meso-scale eddies, G. Voet and D. Quadfasel, Ocean Science, 6, 301-310, 2010Copernicus Electronic Production Support Office2010-03-01T00:00:00+01:002010-03-01T00:00:00+01:00http://www.ocean-sci.net/6/285/2010/On contribution of horizontal and intra-layer convection to the formation of the Baltic Sea cold intermediate layerOn contribution of horizontal and intra-layer convection to the formation of the Baltic Sea cold intermediate layer, I. Chubarenko and N. Demchenko, Ocean Science, 6, 285-299, 2010Copernicus Electronic Production Support Office2010-02-26T00:00:00+01:002010-02-26T00:00:00+01:00http://www.ocean-sci.net/6/269/2010/Impact of global ocean model resolution on sea-level variability with emphasis on interannual time scalesImpact of global ocean model resolution on sea-level variability with emphasis on interannual time scales, T. Penduff, M. Juza, L. Brodeau, G. C. Smith, B. Barnier, J.-M. Molines, A.-M. Treguier, and G. Madec, Ocean Science, 6, 269-284, 2010Copernicus Electronic Production Support Office2010-02-25T00:00:00+01:002010-02-25T00:00:00+01:00http://www.ocean-sci.net/6/263/2010/Preface "Operational oceanography in the Mediterranean Sea: the second stage of development"Preface "Operational oceanography in the Mediterranean Sea: the second stage of development", N. Pinardi and G. Coppini, Ocean Science, 6, 263-267, 2010Copernicus Electronic Production Support Office2010-02-18T00:00:00+01:002010-02-18T00:00:00+01:00http://www.ocean-sci.net/6/247/2010/Characterization of mixing errors in a coupled physical biogeochemical model of the North Atlantic: implications for nonlinear estimation using Gaussian anamorphosisCharacterization of mixing errors in a coupled physical biogeochemical model of the North Atlantic: implications for nonlinear estimation using Gaussian anamorphosis, D. Béal, P. Brasseur, J.-M. Brankart, Y. Ourmières, and J. Verron, Ocean Science, 6, 247-262, 2010Copernicus Electronic Production Support Office2010-02-17T00:00:00+01:002010-02-17T00:00:00+01:00http://www.ocean-sci.net/6/235/2010/Assessment of sensor performanceAssessment of sensor performance, C. Waldmann, M. Tamburri, R. D. Prien, and P. Fietzek, Ocean Science, 6, 235-245, 2010Copernicus Electronic Production Support Office2010-02-17T00:00:00+01:002010-02-17T00:00:00+01:00http://www.ocean-sci.net/6/219/2010/Heat in the Barents Sea: transport, storage, and surface fluxesHeat in the Barents Sea: transport, storage, and surface fluxes, L. H. Smedsrud, R. Ingvaldsen, J. E. Ø. Nilsen, and Ø. Skagseth, Ocean Science, 6, 219-234, 2010Copernicus Electronic Production Support Office2010-02-11T00:00:00+01:002010-02-11T00:00:00+01:00