Numerical Simulation of Three-Dimensional, Shape-Preserving Convective ElementsSource: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002::page 322Author:Fox, Douglas G.
DOI: 10.1175/1520-0469(1972)029<0322:NSOTDS>2.0.CO;2Publisher: American Meteorological Society
Abstract: The motions resulting from the sudden release of a fixed amount of buoyancy in an incompressible fluid are simulated. Solutions are allowed to reach a steady state in the finite computed volume by the introduction of a dynamical stretching of the coordinate system. Fully nonlinear, transformed, and finite-differenced Navier-Stokes equations are integrated in time over a three-dimensional grid. It is shown that a steady-state solution to the transformed equations is equivalent to a self-preserving solution in real space. Physically realistic results are presented for a range of Reynolds numbers between 10 and 100. In a strongly diffusive regime the simulation agrees with an existing theoretical solution. Reynolds numbers of order 50 are sufficient to reproduce many of the features of laboratory experiments.
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| contributor author | Fox, Douglas G. | |
| date accessioned | 2017-06-09T14:16:17Z | |
| date available | 2017-06-09T14:16:17Z | |
| date copyright | 1972/03/01 | |
| date issued | 1972 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-16128.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151877 | |
| description abstract | The motions resulting from the sudden release of a fixed amount of buoyancy in an incompressible fluid are simulated. Solutions are allowed to reach a steady state in the finite computed volume by the introduction of a dynamical stretching of the coordinate system. Fully nonlinear, transformed, and finite-differenced Navier-Stokes equations are integrated in time over a three-dimensional grid. It is shown that a steady-state solution to the transformed equations is equivalent to a self-preserving solution in real space. Physically realistic results are presented for a range of Reynolds numbers between 10 and 100. In a strongly diffusive regime the simulation agrees with an existing theoretical solution. Reynolds numbers of order 50 are sufficient to reproduce many of the features of laboratory experiments. | |
| publisher | American Meteorological Society | |
| title | Numerical Simulation of Three-Dimensional, Shape-Preserving Convective Elements | |
| type | Journal Paper | |
| journal volume | 29 | |
| journal issue | 2 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1972)029<0322:NSOTDS>2.0.CO;2 | |
| journal fristpage | 322 | |
| journal lastpage | 341 | |
| tree | Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 002 | |
| contenttype | Fulltext |