Search from over 60,000 research works

Advanced Search

Negative available potential energy dissipation as the fundamental criterion for double diffusive instabilities

[thumbnail of APE_dissipation_R3_centaur.pdf]
APE_dissipation_R3_centaur.pdf - Accepted Version (3MB)
Restricted to Repository staff only
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Tailleux, R. orcid id iconORCID: https://orcid.org/0000-0001-8998-9107 (2024) Negative available potential energy dissipation as the fundamental criterion for double diffusive instabilities. Journal Of Fluid Mechanics, 994. A5. ISSN 1469-7645 doi: 10.1017/jfm.2024.647

Abstract/Summary

The background potential energy (BPE) is the only reservoir that double diffusive instabilities can tap their energy from when developing from an unforced motionless state with no available potential energy (APE). Recently, Middleton and Taylor linked the extraction of BPE into APE to the sign of the diapycnal component of the buoyancy flux, but their criterion can only predict diffusive convection instability, not salt finger instability. Here, we show that the problem can be corrected if the sign of the APE dissipation rate is used instead, making it emerge as the most fundamental criterion for double diffusive instabilities. A theory for the APE dissipation rate for a two-component fluid relative to its single-component counterpart is developed as a function of three parameters: the diffusivity ratio, the density ratio, and a spiciness parameter. The theory correctly predicts the occurrence of both salt finger and diffusive convection instabilities in the laminar unforced regime, while more generally predicting that the APE dissipation rate for a two-component fluid can be enhanced, suppressed, or even have the opposite sign compared to that for a single-component fluid, with important implications for the study of ocean mixing. Because negative APE dissipation can also occur in stably stratified single-component and doubly stable two-component stratified fluids, we speculate that only the thermodynamic theory of exergy can explain its physics; however, this necessitates accepting that APE dissipation is a conversion between APE and the internal energy component of BPE, in contrast to prevailing assumptions.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/116978
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 negative dissipation, mixing, double-diffusion, salt fingers, diffusive convection, thermohaline staircases, available potential energy
Publisher Cambridge University Press
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar