The Efficiency of Mixing in Turbulent Patches: Inferences from Direct Simulations and Microstructure Observations
By W. Smyth, James N. Moum, D. Caldwell. 2001
349 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/a0d517ceec7cc8b1e00c5ca50bbfe4fd529511a1
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- L. Umlauf
- H. Burchard
- W. Richard Peltier
- Jeffrey R. Koseff
- Colm‐cille P. Caulfield
- T. Dahl
- K. Winters
- L. Boegman
In Oceanography
- L. Umlauf
- H. Burchard
- W. Richard Peltier
- Colm‐cille P. Caulfield
- T. Dahl
- K. Winters
- John M. Wahr
- M. Tamisiea
Citations in the corpus
- Second-order turbulence closure models for geophysical boundary layers. A review of recent work (2005, background): “This is not different for the field of physical oceanography, where idealised oceanic flows have been simulated with LES (see e.g. Skyllingstad et al., 1999) or DNS (see e.g. Smyth et al., 2001).”
- Density Stratification, Turbulence, but How Much Mixing? (2008, background): “…+ ε) (Ivey & Imberger 1991, Rohr et al. 1984), there is clear consensus from the laboratory and DNS work that Rf is highly variable and changes with mechanism, the evolutionary stage of a turbulent event, and location in the domain (e.g., Barry et al. 2001, Shih et al. 2005, Smyth et al. 2001).”
- Turbulent Mixing of Metal and Silicate during Planet Accretion – and interpretation of the Hf-W chronometer (2010, background): “billows in horizontal flow (Smyth et al., 2001).”
- Turning Ocean Mixing Upside Down (2015, neutral): “…approached the ocean bottom above rough topography but were still in the stratified ocean above the BBL. Numerical simulations and laboratory experiments found that G varies within a factor of 2 of the canonical value of 0.2 (Smyth et al. 2001; Peltier and Caulfield 2003; Mashayek and Peltier 2013a).”
- MIXING EFFICIENCY IN STRATIFIED SHEAR FLOWS (2003, methodology): “First, the effect of variation with Prandtl number, as initially explored by Klaassen & Peltier (1985a) and Smyth et al. (2001), will have to be investigated in detail at sufficiently high Reynolds number and Peclet number to have an intense turbulentmixing phase, as the existence of such a phase…”