Show simple item record

contributor authorSaltzman, Barry
date accessioned2017-06-09T14:12:55Z
date available2017-06-09T14:12:55Z
date copyright1962/07/01
date issued1962
identifier issn0022-4928
identifier otherams-14856.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150463
description abstractThe 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.
publisherAmerican Meteorological Society
titleFinite Amplitude Free Convection as an Initial Value Problem—I
typeJournal Paper
journal volume19
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1962)019<0329:FAFCAA>2.0.CO;2
journal fristpage329
journal lastpage341
treeJournal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 004
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record