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  • Antonov, J. I., D. Seidov, T. P. Boyer, R. A. Locarnini, A. V. Mishonov, H. E. Garcia, O. K. Baranova, M. M. Zweng, and D. R. Johnson (2010), World Ocean Atlas 2009, Volume 2: Salinity, edited by S. Levitus, 184 pp., NOAA Atlas NESDIS 69, U.S. Gov. Print. Off., Washington, D. C.
  • Boyer, T. P., et al. (2009), World Ocean Database 2009, edited by S. Levitus, 206 pp., NOAA Atlas NESDIS 66, U.S. Gov. Print. Off., Washington, D. C., DVDs.
  • Carton, J. A., and B. S. Giese (2008), A reanalysis of ocean climate using Simple Ocean Data Assimilation (SODA), Mon. Weather Rev., 136, 29993017.
  • Carton, J. A., B. S. Giese, and S. A. Grodsky (2005), Sea level rise and the warming of the oceans in the Simple Ocean Data Assimilation (SODA) ocean reanalysis, J. Geophys. Res., 110, C09006, doi:10.1029/2004JC002817.
  • Cessi, P. (2007), Regimes of thermocline scaling: The interaction of wind stress and surface buoyancy, J. Phys. Oceanogr., 37, 20092021.
  • Chelton, D. B., M. G. Schlax, and R. M. Samelson (2011), Global observations of nonlinear mesoscale eddies, Prog. Oceanogr., 91, 167216.
  • Compo, G. P., et al. (2011), The Twentieth Century Reanalysis Project. Q. J. R. Meteorol. Soc., 137, 128, doi:10.1002/qj.776.
  • Cunningham, S. A. (2005), RRS Discovery Cruise 279 (04 Apr 10–May 2004): A Transatlantic Hydrography Section at 24.5° N., Cruise Report 54, 1199, Southampton Oceanography Centre. [Available at http://eprints.soton.ac.uk/17527/.]
  • de Boyer Montégut, C., G. Madec, A. S. Fischer, A. Lazar, and D. Iudicone (2004), Mixed layer depth over the global ocean: An examination of profile data and a profile-based climatology, J. Geophys. Res., 109, C12003, doi:10.1029/2004JC002378.
  • Delcroix, T., A. Dessier, Y. Gouriou, and M. McPhaden (2005), Time and space scales for sea surface salinity in the tropical oceans, Deep Sea Res., Part I, 52, 787813.
  • Fratantoni, D. M. (2001), North Atlantic surface circulation during the 1990's observed with satellite-tracked drifters, J. Geophys. Res., 106, (C10), 2206722093.
  • Fu, L.-L. and D. B. Chelton (2001), Large-scale ocean circulation, in Satellite Altimetry and the Earth Sciences: A Handbook of Techniques and Applications, edited by L.-L. Fu, A. Cazenave, pp. 133169, Academic Press, San Diego, Calif.
  • Gill, A. (1982), Atmosphere-Ocean Dynamics, Int. Geophys. Ser., vol. 30, 662 pp., Academic Press, N. Y.
  • Gill, A. E., J. S. A. Green, and A. J. Simmons (1974). Energy partition in the large-scale ocean circulation and the production of mid-ocean eddies, Deep Sea Res., 21, 499528.
  • Gordon, A. L. and C. F. Giulivi (2008), Sea surface salinity trends over 50 years within the Subtropical North Atlantic, Oceanography, 21, 2029.
  • Giese B. S. and S. Ray (2011), El Nino variability in simple ocean data assimilation (SODA), 1871–2008, J. Geophys. Res, 116, C02024, doi:10.1029/2010JC006695.
  • Kara, A. B., P. A. Rochford, and H. E. Hurlburt (2003), Mixed layer depth variability over the global ocean, J. Geophys. Res., 108(C3), 3079, doi:10.1029/2000JC000736.
  • Lagerloef, G., et al. (2008), The Aquarius/SAC-D Mission: Designed to meet the salinity remote-sensing challenge. Oceanography, 21, 6881.
  • Lagerloef, G., F. Wentz, S. Yueh, H. Y. Kao, G. C. Johnson, and J. M. Lyman (2012), Aquarius satellite mission provides new, detailed view of sea surface salinity, State of the Climate in 2011, Bull. Am. Meteorol. Soc., 93, 7, S70S71.
  • Locarnini, R. A., A. V. Mishonov, J. I. Antonov, T. P. Boyer, H. E. Garcia, O. K. Baranova, M. M. Zweng, and D. R. Johnson (2010), World Ocean Atlas 2009, Volume 1: Temperature, edited by S. Levitus, 184 pp., NOAA Atlas NESDIS 68, U.S. Gov. Print. Off., Washington, D. C.
  • Maximenko, N., P. Niiler, M.-H. Rio, O. Melnichenko, L. Centurioni, D. Chambers, V. Zlotnicki, and B. Galperin (2009), Mean dynamic topography of the ocean derived from satellite and drifting buoy data using three different techniques. J. Atmos. Oceanic Technol., 26(9), 19101919.
  • Reverdin, G., E. Kestenare, C. Frankignoul, and T. Delcroix (2007), Surface salinity in the Atlantic Ocean (30S-50N), Prog. Oceanogr., 73, 311340.
  • Schanze, J. J., R. W. Schmitt, and L. L. Yu (2010), The global oceanic freshwater cycle: A state of the art quantification, J. Mar. Res., 68(3–4), 569575.
  • Talley, L. D. (2008), Freshwater transport estimates and the global overturning circulation: Shallow, deep and throughflow components, Prog. Oceanogr., 78, 257303.
  • Uppala, S. M., et al. (2005), The ERA-40 re-analysis, Q. J. R. Meteorol. Soc., 131, 29613012.
  • Woodruff, S. D., et al. (2011), ICOADS Release 2.5: Extensions and enhancements to the surface marine meteorological archive, Int. J. Climatol., 31, 951967.
  • Worthington, L. V. (1976), The formation of salinity-maximum water, Johns Hopkins Oceanogr. Stud., 6, 8591.