OS - Latest Articleshttp://www.ocean-sci.net/2009-06-19T12:05:26+02:00Copernicus Electronic Production Support Officehttp://www.ocean-sci.net/5/203/2009/Geothermal heating, diapycnal mixing and the abyssal circulationGeothermal heating, diapycnal mixing and the abyssal circulation, J. Emile-Geay and G. Madec, Ocean Science, 5, 203-217, 2009Copernicus Electronic Production Support Office2009-06-19T00:00:00+02:002009-06-19T00:00:00+02:00http://www.ocean-sci.net/5/193/2009/A new assessment of the error budget of global mean sea level rate estimated by satellite altimetry over 1993–2008A new assessment of the error budget of global mean sea level rate estimated by satellite altimetry over 1993–2008, M. Ablain, A. Cazenave, G. Valladeau, and S. Guinehut, Ocean Science, 5, 193-201, 2009Copernicus Electronic Production Support Office2009-06-17T00:00:00+02:002009-06-17T00:00:00+02:00http://www.ocean-sci.net/5/191/2009/Corrigendum to "A new method for forming approximately neutral surfaces" published in Ocean Sci., 5, 155–172, 2009Corrigendum to "A new method for forming approximately neutral surfaces" published in Ocean Sci., 5, 155–172, 2009, A. Klocker, T. J. McDougall, and D. R. Jackett, Ocean Science, 5, 191-191, 2009Copernicus Electronic Production Support Office2009-06-10T00:00:00+02:002009-06-10T00:00:00+02:00http://www.ocean-sci.net/5/173/2009/Evaluating two numerical advection schemes in HYCOM for eddy-resolving modelling of the Agulhas CurrentEvaluating two numerical advection schemes in HYCOM for eddy-resolving modelling of the Agulhas Current, B. C. Backeberg, L. Bertino, and J. A. Johannessen, Ocean Science, 5, 173-190, 2009Copernicus Electronic Production Support Office2009-06-02T00:00:00+02:002009-06-02T00:00:00+02:00http://www.ocean-sci.net/5/155/2009/A new method for forming approximately neutral surfacesA new method for forming approximately neutral surfaces, A. Klocker, T. J. McDougall, and D. R. Jackett, Ocean Science, 5, 155-172, 2009Copernicus Electronic Production Support Office2009-05-28T00:00:00+02:002009-05-28T00:00:00+02:00http://www.ocean-sci.net/5/141/2009/Deep currents in the Gulf of Guinea: along slope propagation of intraseasonal wavesDeep currents in the Gulf of Guinea: along slope propagation of intraseasonal waves, C. Guiavarc'h, A. M. Treguier, and A. Vangriesheim, Ocean Science, 5, 141-153, 2009Copernicus Electronic Production Support Office2009-05-18T00:00:00+02:002009-05-18T00:00:00+02:00http://www.ocean-sci.net/5/115/2009/Ekman layers in the Southern Ocean: spectral models and observations, vertical viscosity and boundary layer depthEkman layers in the Southern Ocean: spectral models and observations, vertical viscosity and boundary layer depth, S. Elipot and S. T. Gille, Ocean Science, 5, 115-139, 2009Copernicus Electronic Production Support Office2009-05-14T00:00:00+02:002009-05-14T00:00:00+02:00http://www.ocean-sci.net/5/101/2009/Molecular biology techniques and applications for ocean sensingMolecular biology techniques and applications for ocean sensing, J. P. Zehr, I. Hewson, and P. Moisander, Ocean Science, 5, 101-113, 2009Copernicus Electronic Production Support Office2009-05-08T00:00:00+02:002009-05-08T00:00:00+02:00http://www.ocean-sci.net/5/91/2009/The density of seawater as a function of salinity (5 to 70 g kg<sup>&minus;1</sup>) and temperature (273.15 to 363.15 K)The density of seawater as a function of salinity (5 to 70 g kg<sup>&minus;1</sup>) and temperature (273.15 to 363.15 K), F. J. Millero and F. Huang, Ocean Science, 5, 91-100, 2009Copernicus Electronic Production Support Office2009-05-05T00:00:00+02:002009-05-05T00:00:00+02:00http://www.ocean-sci.net/5/73/2009/"Scale oriented" embedded modeling of the North-Western Mediterranean in the frame of MFSTEP"Scale oriented" embedded modeling of the North-Western Mediterranean in the frame of MFSTEP, C. Estournel, F. Auclair, M. Lux, C. Nguyen, and P. Marsaleix, Ocean Science, 5, 73-90, 2009Copernicus Electronic Production Support Office2009-04-27T00:00:00+02:002009-04-27T00:00:00+02:00