Construct · 1 fields · 1 citations

Osborn relation: a standalone construct

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Physical oceanography

an estimate of vertical eddy diffusivity from the measured dissipation rate of turbulent kinetic energy, buoyancy frequency and a mixing efficiency.

In physical oceanography, Osborn relation refers to an estimate of vertical eddy diffusivity from the measured dissipation rate of turbulent kinetic energy, buoyancy frequency and a mixing efficiency. This meaning comes from Osborn (1980) in Journal of Physical Oceanography.[1]

Unit
Recovery means
Measured by

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Nearby constructs

Brunt-Väisälä frequency1 fields · 1 citationsanchor · a standalone construct buoyancy4 fields · 4 citationsjingle · one word, four constructs dissipation4 fields · 7 citationsjingle · one word, four constructs

References

Osborn, T. R. (1980). Estimates of the Local Rate of Vertical Diffusion from Dissipation Measurements. Journal of Physical Oceanography, 10(1), 83-89. https://doi.org/10.1175/1520-0485(1980)010<0083:eotlro>2.0.co;2

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