Finite Amplitude Free Convection as an Initial Value Problem—ISource: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 004::page 329Author:Saltzman, Barry
DOI: 10.1175/1520-0469(1962)019<0329:FAFCAA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set of ordinary differential equations governing the time variations of the double-Fourier coefficients for the motion and temperature fields. Non-linear transfer processes are retained and appear as quadratic interactions between the Fourier coefficients. Energy and heat transfer relations appropriate to this Fourier resolution, and a numerical method for solution from arbitrary initial conditions are given. As examples of the method, numerical solutions for a highly truncated Fourier representation are presented. These solutions, which are for a fixed Prandtl number and variable Rayleigh numbers, show the transient growth of convection from small perturbations, and in all cases studied approach steady states. The steady states obtained agree favorably with steady-state solutions obtained by previous investigators.
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contributor author | Saltzman, Barry | |
date accessioned | 2017-06-09T14:12:55Z | |
date available | 2017-06-09T14:12:55Z | |
date copyright | 1962/07/01 | |
date issued | 1962 | |
identifier issn | 0022-4928 | |
identifier other | ams-14856.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150463 | |
description abstract | The Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set of ordinary differential equations governing the time variations of the double-Fourier coefficients for the motion and temperature fields. Non-linear transfer processes are retained and appear as quadratic interactions between the Fourier coefficients. Energy and heat transfer relations appropriate to this Fourier resolution, and a numerical method for solution from arbitrary initial conditions are given. As examples of the method, numerical solutions for a highly truncated Fourier representation are presented. These solutions, which are for a fixed Prandtl number and variable Rayleigh numbers, show the transient growth of convection from small perturbations, and in all cases studied approach steady states. The steady states obtained agree favorably with steady-state solutions obtained by previous investigators. | |
publisher | American Meteorological Society | |
title | Finite Amplitude Free Convection as an Initial Value Problem—I | |
type | Journal Paper | |
journal volume | 19 | |
journal issue | 4 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1962)019<0329:FAFCAA>2.0.CO;2 | |
journal fristpage | 329 | |
journal lastpage | 341 | |
tree | Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 004 | |
contenttype | Fulltext |