Oliver, K. I. C. and Tailleux, R. ORCID: https://orcid.org/0000-0001-8998-9107
(2013)
Thermobaric control of gravitational potential energy generation by diapycnal mixing in the deep ocean.
Geophysical Research Letters, 40 (2).
pp. 327-331.
ISSN 0094-8276
doi: 10.1029/2012GL054235
Abstract/Summary
Sources and sinks of gravitational potential energy (GPE) play a rate-limiting role in the large scale ocean circulation. A key source is turbulent diapycnal mixing, whereby irre- versible mixing across isoneutral surfaces is enhanced by turbulent straining of these surfaces. This has motivated international observational efforts to map diapycnal mixing in the global ocean. However, in order to accurately relate the GPE supplied to the large scale circulation by diapycnal mixing to the mixing energy source, it is first necessary to determine the ratio, ξ , of the GPE generation rate to the available potential energy dissipation rate associated with turbulent mixing. Here, the link between GPE and hydro- static pressure is used to derive the GPE budget for a com- pressible ocean with a nonlinear equation of state. The role of diapycnal mixing is isolated and from this a global cli- matological distribution of ξ is calculated. It is shown that, for a given source of mixing energy, typically three times as much GPE is generated if the mixing takes place in bottom waters rather than in the pycnocline. This is due to GPE destruction by cabbelling in the pycnocline, as opposed to thermobaric enhancement of GPE generation by diapycnal mixing in the deep ocean.
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Item Type | Article |
URI | https://reading-clone.eprints-hosting.org/id/eprint/34400 |
Item Type | Article |
Refereed | Yes |
Divisions | Interdisciplinary Research Centres (IDRCs) > Walker Institute Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology |
Uncontrolled Keywords | diapycnal mixing; equation of state; thermodynamics; meridional overturning circulation |
Publisher | American Geophysical Union |
Publisher Statement | Copyright belong to the publisher |
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