Buoyant Motion of a Turbulent ThermalSource: Journal of the Atmospheric Sciences:;2018:;volume 075:;issue 009::page 3233DOI: 10.1175/JAS-D-17-0371.1Publisher: American Meteorological Society
Abstract: AbstractBy introducing an equivalence between magnetostatics and the equations governing buoyant motion, we derive analytical expressions for the acceleration of isolated density anomalies (thermals). In particular, we investigate buoyant acceleration, defined as the sum of the Archimedean buoyancy B and an associated perturbation pressure gradient. For the case of a uniform spherical thermal, the anomaly fluid accelerates at 2B/3, extending the textbook result for the induced mass of a solid sphere to the case of a fluid sphere. For a more general ellipsoidal thermal, we show that the buoyant acceleration is a simple analytical function of the ellipsoid?s aspect ratio. The relevance of these idealized uniform-density results to turbulent thermals is explored by analyzing direct numerical simulations of thermals at a Reynolds number (Re) of 6300. We find that our results fully characterize a thermal?s initial motion over a distance comparable to its length. Beyond this buoyancy-dominated regime, a thermal develops an ellipsoidal vortex circulation and begins to entrain environmental fluid. Our analytical expressions do not describe the total acceleration of this mature thermal, but they still accurately relate the buoyant acceleration to the thermal?s mean Archimedean buoyancy and aspect ratio. Thus, our analytical formulas provide a simple and direct means of estimating the buoyant acceleration of turbulent thermals.
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| contributor author | Tarshish, Nathaniel | |
| contributor author | Jeevanjee, Nadir | |
| contributor author | Lecoanet, Daniel | |
| date accessioned | 2019-09-19T10:07:54Z | |
| date available | 2019-09-19T10:07:54Z | |
| date copyright | 6/28/2018 12:00:00 AM | |
| date issued | 2018 | |
| identifier other | jas-d-17-0371.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4261879 | |
| description abstract | AbstractBy introducing an equivalence between magnetostatics and the equations governing buoyant motion, we derive analytical expressions for the acceleration of isolated density anomalies (thermals). In particular, we investigate buoyant acceleration, defined as the sum of the Archimedean buoyancy B and an associated perturbation pressure gradient. For the case of a uniform spherical thermal, the anomaly fluid accelerates at 2B/3, extending the textbook result for the induced mass of a solid sphere to the case of a fluid sphere. For a more general ellipsoidal thermal, we show that the buoyant acceleration is a simple analytical function of the ellipsoid?s aspect ratio. The relevance of these idealized uniform-density results to turbulent thermals is explored by analyzing direct numerical simulations of thermals at a Reynolds number (Re) of 6300. We find that our results fully characterize a thermal?s initial motion over a distance comparable to its length. Beyond this buoyancy-dominated regime, a thermal develops an ellipsoidal vortex circulation and begins to entrain environmental fluid. Our analytical expressions do not describe the total acceleration of this mature thermal, but they still accurately relate the buoyant acceleration to the thermal?s mean Archimedean buoyancy and aspect ratio. Thus, our analytical formulas provide a simple and direct means of estimating the buoyant acceleration of turbulent thermals. | |
| publisher | American Meteorological Society | |
| title | Buoyant Motion of a Turbulent Thermal | |
| type | Journal Paper | |
| journal volume | 75 | |
| journal issue | 9 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/JAS-D-17-0371.1 | |
| journal fristpage | 3233 | |
| journal lastpage | 3244 | |
| tree | Journal of the Atmospheric Sciences:;2018:;volume 075:;issue 009 | |
| contenttype | Fulltext |