Thermobaric control of gravitational potential energy generation by diapycnal mixing in the deep ocean

Author:

Oliver K. I. C.1,Tailleux R.2

Affiliation:

1. National Oceanography Centre, Southampton; University of Southampton; UK

2. Department of Meteorology; University of Reading; Reading UK

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference25 articles.

1. Antonov , J. I. R. A. Locarnini T. P. Boyer A. V. Mishonov H. E. Garcia 2006 World Ocean Atlas 2005, Volume 2: Salinity 182

2. Meridional density gradients do not control the atlantic overturning circulation;Boer;J. Phys. Oceanogr.,2010

3. The duality between the Boussinesq and non-Boussinesq hydrostatic equations of motion;Szoeke;J. Phys. Ocean.,2000

4. Nonlinear limits to ocean thermal structure;Fofonoff;J. Marine Res.,1998

5. Thermal stability of the world ocean thermoclines;Fofonoff;J. Phys. Oceanogr.,2001

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