{ "id": "physics/0304080", "version": "v1", "published": "2003-04-22T07:32:56.000Z", "updated": "2003-04-22T07:32:56.000Z", "title": "Forced Stratified Turbulence: Successive Transitions with Reynolds Number", "authors": [ "Jean-Philippe Laval", "James C. McWilliams" ], "comment": "8 pages, 5 figures (submitted to Phys. Rev. E)", "journal": "Phys. Rev. E, vol 68, 036308 (2003)", "doi": "10.1103/PhysRevE.68.036308", "categories": [ "physics.flu-dyn", "physics.ao-ph", "physics.geo-ph" ], "abstract": "Numerical simulations are made for forced turbulence at a sequence of increasing values of Reynolds number, R, keeping fixed a strongly stable, volume-mean density stratification. At smaller values of R, the turbulent velocity is mainly horizontal, and the momentum balance is approximately cyclostrophic and hydrostatic. This is a regime dominated by so-called pancake vortices, with only a weak excitation of internal gravity waves and large values of the local Richardson number, Ri, everywhere. At higher values of R there are successive transitions to (a) overturning motions with local reversals in the density stratification and small or negative values of Ri; (b) growth of a horizontally uniform vertical shear flow component; and (c) growth of a large-scale vertical flow component. Throughout these transitions, pancake vortices continue to dominate the large-scale part of the turbulence, and the gravity wave component remains weak except at small scales.", "revisions": [ { "version": "v1", "updated": "2003-04-22T07:32:56.000Z" } ], "analyses": { "keywords": [ "reynolds number", "forced stratified turbulence", "successive transitions", "uniform vertical shear flow", "vertical shear flow component" ], "tags": [ "journal article" ], "publication": { "publisher": "APS", "journal": "Phys. Rev. E" }, "note": { "typesetting": "TeX", "pages": 8, "language": "en", "license": "arXiv", "status": "editable" } } }