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OCEAN THERMAL ENERGY CONVERSION (OTEC)

Marshall DP (1997) Subduction of water masses in aneddying of Marine Research55:201} JC, Nurser AJG and Williams RG (1993).Inferring the subduction rate and period over theNorth of Physical Oceanography23: 1315} S, Rhines PB and Keffer T (1982) North Atlan-tic potential vorticity and its relation to the of Physical Oceanography12:1417} J (1996) OCEAN Circulation Theory. New RT and Regier LA (1992) Vorticity and verticalcirculation at an OCEAN of PhysicalOceanography22: 609} JF (2001) Subduction. In: OCEAN Circulation andClimate: Observing and Modelling the Global OCEAN ,G. Siedler, J. Church and J. Gould (eds), AcademicPress, pp. PB and Schopp R (1991) The wind-driven circula-tion: quasi-geostrophic simulations and theory for non-symmetric of Physical Oceanography21: 1438} RM and Vallis GK (1997) Large-scale circula-tion with small diapycnal diffusion: the two-thermo-cline of Marine Research55: 223} H (1979) Determination of watermass propertiesof water pumped down from the Ekman layer to thegeostrophicSow of the NationalAcademy of Sciences of the USA76: 3051} RG (1991) The role of the mixed layer in settingthe potential vorticity of the main Physical Oceanography21: 1803} RG, Spall MA and Marshall JC (1995) DoesStommel s mixed-layer Demon work?

Marshall DP (1997) Subduction of water masses in an eddying ocean. Journal of Marine Research 55: 201}222. Marshall JC, Nurser AJG and Williams RG (1993).

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