Generation of slow large scales in forced rotating stratified turbulence

By L. Smith, Fabian Waleffe. Journal of Fluid Mechanics, 2002

221 citations recorded by the source corpus.

Subfields: Molecular Biology, Oceanography

View Paper: https://www.semanticscholar.org/paper/7f80e68a8af5b94b63d24d46a6c95940dff0a51d

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Citations in the corpus

The energy cascade in a strongly stratified fluid (2006, methodology): “Although they observe the same kind of weak growth in kρ =0 modes as Smith & Waleffe (2002), they do not interpret this growth as a sign of an inverse energy cascade.”
Inverse cascade and symmetry breaking in rapidly rotating Boussinesq convection (2014, unknown): “For example, inverse cascade of energy from the small forcing scale to the largest available scale has been observed in forced rotating turbulence 1,2 and forced rotating stably-stratiﬁed turbulence 3 in tri-periodic domains.”
Stratified turbulence dominated by vortical motion (2004, methodology): “In forced simulations of stratified turbulence in a periodic domain, a slow transfer of energy into the horizontally averaged flow (modes with kh = 0) has been observed ( Smith & Waleffe 2002; Laval et al. 2003).”
Scaling analysis and simulation of strongly stratified turbulent flows (2007, methodology): “The choice m = 2 defines the classical Taylor microscale used by Riley & deBruynKops (2003). This choice is more problematic from a theoretical point of view, because it puts too much weight on the small scales, and will therefore be dependent on the Reynolds number.”
Fourth-Order Time-Stepping for Stiff PDEs (2005, methodology): “This technique has been used for PDEs by Milewski and Tabak [44], Maday, Patera, and Rønquist [40], Smith and Waleffe [55, 56], Fornberg and Driscoll [20], Trefethen [60], Boyd [7], and Cox and Matthews [14].”