Stratified turbulence: A possible interpretation of some geophysical turbulence measurements
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
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.
isopycnic slope spectra, internal gravity-waves, columnar vortex pair, fluid, number, ocean
IdentifiersURN: urn:nbn:se:kth:diva-17708DOI: 10.1175/2007jas2455.1ISI: 000257796200022ScopusID: 2-s2.0-52049122392OAI: oai:DiVA.org:kth-17708DiVA: diva2:335753
QC 201005252010-08-052010-08-05Bibliographically approved