OSD - Latest Articleshttp://www.ocean-sci-discuss.net/2008-07-17T15:35:59+02:00Copernicus Electronic Production Support Officehttp://www.ocean-sci-discuss.net/5/375/2008/Development of thermodynamic potentials for fluid water, ice and seawater: a new standard for oceanographyDevelopment of thermodynamic potentials for fluid water, ice and seawater: a new standard for oceanography, R. Feistel, D. G. Wright, K. Miyagawa, J. Hruby, D. R. Jackett, T. J. McDougall, and W. Wagner, Ocean Science Discussions, 5, 375-418, 2008Copernicus Electronic Production Support Office2008-07-11T00:00:00+02:002008-07-11T00:00:00+02:00http://www.ocean-sci-discuss.net/5/327/2008/Sensors for physical fluxes at the sea surface: energy, heat, water, saltSensors for physical fluxes at the sea surface: energy, heat, water, salt, R. A. Weller, E. F. Bradley, J. Edson, C. Fairall, I. Brooks, M. J. Yelland, and R. W. Pascal, Ocean Science Discussions, 5, 327-373, 2008Copernicus Electronic Production Support Office2008-07-11T00:00:00+02:002008-07-11T00:00:00+02:00http://www.ocean-sci-discuss.net/5/281/2008/Geothermal heating, diapycnal mixing and the abyssal circulationGeothermal heating, diapycnal mixing and the abyssal circulation, J. Emile-Geay and G. Madec, Ocean Science Discussions, 5, 281-325, 2008Copernicus Electronic Production Support Office2008-07-07T00:00:00+02:002008-07-07T00:00:00+02:00http://www.ocean-sci-discuss.net/5/255/2008/Sequential assimilation of multi-mission dynamical topography into a global finite-element ocean modelSequential assimilation of multi-mission dynamical topography into a global finite-element ocean model, S. Skachko, S. Danilov, T. Janjić, J. Schröter, and D. Sidorenko, Ocean Science Discussions, 5, 255-279, 2008Copernicus Electronic Production Support Office2008-06-20T00:00:00+02:002008-06-20T00:00:00+02:00http://www.ocean-sci-discuss.net/5/213/2008/North Indian Ocean variability during the Indian Ocean dipoleNorth Indian Ocean variability during the Indian Ocean dipole, J. Brown, C. A. Clayson, L. Kantha, and T. Rojsiraphisal, Ocean Science Discussions, 5, 213-253, 2008Copernicus Electronic Production Support Office2008-06-09T00:00:00+02:002008-06-09T00:00:00+02:00http://www.ocean-sci-discuss.net/5/187/2008/A new parameterisation of salinity advection to prevent stratification from running away in a simple estuarine modelA new parameterisation of salinity advection to prevent stratification from running away in a simple estuarine model, S. Blaise and E. Deleersnijder, Ocean Science Discussions, 5, 187-211, 2008Copernicus Electronic Production Support Office2008-06-02T00:00:00+02:002008-06-02T00:00:00+02:00http://www.ocean-sci-discuss.net/5/163/2008/Joint effect of the western and eastern Pacific warm pools on ENSO cycleJoint effect of the western and eastern Pacific warm pools on ENSO cycle, Q. Qi, Y. Hou, Q. Zhang, and T. Yan, Ocean Science Discussions, 5, 163-185, 2008Copernicus Electronic Production Support Office2008-05-28T00:00:00+02:002008-05-28T00:00:00+02:00http://www.ocean-sci-discuss.net/5/135/2008/The structure of the Persian Gulf outflow subjected to density variationsThe structure of the Persian Gulf outflow subjected to density variations, A. A. Bidokhti and M. Ezam, Ocean Science Discussions, 5, 135-161, 2008Copernicus Electronic Production Support Office2008-05-22T00:00:00+02:002008-05-22T00:00:00+02:00http://www.ocean-sci-discuss.net/5/123/2008/Coastal upwelling along the southwest coast of India – ENSO modulationCoastal upwelling along the southwest coast of India – ENSO modulation, K. Muni Krishna, Ocean Science Discussions, 5, 123-134, 2008Copernicus Electronic Production Support Office2008-04-21T00:00:00+02:002008-04-21T00:00:00+02:00http://www.ocean-sci-discuss.net/5/103/2008/A comparison between vertical motions measured by ADCP and inferred from temperature dataA comparison between vertical motions measured by ADCP and inferred from temperature data, H. van Haren, Ocean Science Discussions, 5, 103-121, 2008Copernicus Electronic Production Support Office2008-04-14T00:00:00+02:002008-04-14T00:00:00+02:00