Available potential energy gain from mixing due to the nonlinearity of the equation of state in a global ocean model
Densification in the ocean interior upon mixing at high latitudes, due to the nonlinear equation of state (EoS) of seawater, enhances the meridional overturning circulation (MOC). However, recent calculations using numerical simulations of global ocean circulation have shown that the nonlinearity of...
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Veröffentlicht in: | Geophysical research letters 2013-05, Vol.40 (10), p.2224-2228 |
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Sprache: | eng |
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