OSD - Latest Articleshttp://www.ocean-sci-discuss.net/2010-02-09T13:31:17+01:00Copernicus Electronic Production Support Officehttp://www.ocean-sci-discuss.net/7/291/2010/Automated gas bubble imaging at sea floor – a new method of in situ gas flux quantificationAutomated gas bubble imaging at sea floor – a new method of in situ gas flux quantification, K. Thomanek, O. Zielinski, H. Sahling, and G. Bohrmann, Ocean Science Discussions, 7, 291-334, 2010Copernicus Electronic Production Support Office2010-02-09T00:00:00+01:002010-02-09T00:00:00+01:00http://www.ocean-sci-discuss.net/7/251/2010/A numerical scheme to calculate temperature and salinity dependent air-water transfer velocities for any gasA numerical scheme to calculate temperature and salinity dependent air-water transfer velocities for any gas, M. T. Johnson, Ocean Science Discussions, 7, 251-290, 2010Copernicus Electronic Production Support Office2010-02-04T00:00:00+01:002010-02-04T00:00:00+01:00http://www.ocean-sci-discuss.net/7/207/2010/Wind forcing effects on coastal circulation and eddy formation around a capeWind forcing effects on coastal circulation and eddy formation around a cape, P. De Gaetano, M. Burlando, A. M. Doglioli, and A. A. Petrenko, Ocean Science Discussions, 7, 207-249, 2010Copernicus Electronic Production Support Office2010-02-02T00:00:00+01:002010-02-02T00:00:00+01:00http://www.ocean-sci-discuss.net/7/177/2010/The role of continental shelves in nitrogen and carbon cyclingThe role of continental shelves in nitrogen and carbon cycling, K. Fennel, Ocean Science Discussions, 7, 177-205, 2010Copernicus Electronic Production Support Office2010-01-29T00:00:00+01:002010-01-29T00:00:00+01:00http://www.ocean-sci-discuss.net/7/143/2010/Exchange across the shelf break at high southern latitudesExchange across the shelf break at high southern latitudes, J. M. Klinck and M. S. Dinniman, Ocean Science Discussions, 7, 143-176, 2010Copernicus Electronic Production Support Office2010-01-26T00:00:00+01:002010-01-26T00:00:00+01:00http://www.ocean-sci-discuss.net/7/121/2010/Operational oceanography in support to indicator reportingOperational oceanography in support to indicator reporting, J. A. Johannessen, G. Coppini, F. Soulat, and G. Larnicol, Ocean Science Discussions, 7, 121-141, 2010Copernicus Electronic Production Support Office2010-01-18T00:00:00+01:002010-01-18T00:00:00+01:00http://www.ocean-sci-discuss.net/7/91/2010/Long term trends in the sea surface temperature of the Black SeaLong term trends in the sea surface temperature of the Black Sea, G. I. Shapiro, D. L. Aleynik, and L. D. Mee, Ocean Science Discussions, 7, 91-119, 2010Copernicus Electronic Production Support Office2010-01-18T00:00:00+01:002010-01-18T00:00:00+01:00http://www.ocean-sci-discuss.net/7/51/2010/Importance of the variability of hydrographic preconditioning for deep convection in the Gulf of Lion, NW MediterraneanImportance of the variability of hydrographic preconditioning for deep convection in the Gulf of Lion, NW Mediterranean, L. Grignon, D. A. Smeed, H. L. Bryden, and K. Schroeder, Ocean Science Discussions, 7, 51-90, 2010Copernicus Electronic Production Support Office2010-01-18T00:00:00+01:002010-01-18T00:00:00+01:00http://www.ocean-sci-discuss.net/7/17/2010/Structure and forcing of the overflow at the Storfjorden sill and its connection to the Arctic coastal polynya in StorfjordenStructure and forcing of the overflow at the Storfjorden sill and its connection to the Arctic coastal polynya in Storfjorden, F. Geyer, I. Fer, and L. H. Smedsrud, Ocean Science Discussions, 7, 17-49, 2010Copernicus Electronic Production Support Office2010-01-05T00:00:00+01:002010-01-05T00:00:00+01:00http://www.ocean-sci-discuss.net/7/1/2010/Stochastic heterogeneity mapping around a Mediterranean salt lensStochastic heterogeneity mapping around a Mediterranean salt lens, G. G. Buffett, C. A. Hurich, E. A. Vsemirnova, R. W. Hobbs, V. Sallarès, R. Carbonell, D. Klaeschen, and B. Biescas, Ocean Science Discussions, 7, 1-15, 2010Copernicus Electronic Production Support Office2010-01-04T00:00:00+01:002010-01-04T00:00:00+01:00