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Stratified turbulence: A possible interpretation of some geophysical turbulence measurements
KTH, School of Engineering Sciences (SCI), Mechanics, Turbulence.
2008 (English)In: Journal of Atmospheric Sciences, ISSN 0022-4928, E-ISSN 1520-0469, Vol. 65, no 7, 2416-2424 p.Article in journal (Refereed) Published
Abstract [en]

Several existing sets of smaller-scale ocean and atmospheric data appear to display Kolmogorov-Obukov-Corrsin inertial ranges in horizontal spectra for length scales up to at least a few hundred meters. It is argued here that these data are inconsistent with the assumptions for these inertial range theories. Instead, it is hypothesized that the dynamics of stratified turbulence explain these data. If valid, these dynamics may also explain the behavior of strongly stratified flows in similar dynamic ranges of other geophysical flows.

Place, publisher, year, edition, pages
2008. Vol. 65, no 7, 2416-2424 p.
Keyword [en]
isopycnic slope spectra, internal gravity-waves, columnar vortex pair, fluid, number, ocean
Identifiers
URN: urn:nbn:se:kth:diva-17708DOI: 10.1175/2007jas2455.1ISI: 000257796200022Scopus ID: 2-s2.0-52049122392OAI: oai:DiVA.org:kth-17708DiVA: diva2:335753
Note
QC 20100525Available from: 2010-08-05 Created: 2010-08-05Bibliographically approved

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