Understanding mixing efficiency in the oceans: do the nonlinearities of the equation of state for seawater matter?
There exist two central measures of turbulent mixing in turbulent stratified fluids that are both caused by molecular diffusion: 1) the dissipation rate <i>D</i>(APE) of available potential energy APE; 2) the turbulent rate of change <i>W</i>&a...
Main Author: | R. Tailleux |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2009-07-01
|
Series: | Ocean Science |
Online Access: | http://www.ocean-sci.net/5/271/2009/os-5-271-2009.pdf |
Similar Items
-
Estimating Lorenz's Reference State in an Ocean with a Nonlinear Equation of State for Seawater
by: Saenz, Juan A., et al.
Published: (2015) -
Preface "An historical perspective on the development of the Thermodynamic Equation of Seawater – 2010"
by: R. Tailleux, et al.
Published: (2012-03-01) -
History of the Equation of State of Seawater
by: Frank J. Millero
Published: (2010-09-01) -
Increase in sea level variability with ocean warming associated with the nonlinear thermal expansion of seawater
by: Matthew J. Widlansky, et al.
Published: (2020-08-01) -
The hydrothermal alteration of oceanic basalts by seawater.
by: Humphris, Susan Elizabeth
Published: (2010)