Hydrothermal Surface-Wave Instability and the Kuramoto-Sivas(6)

2021-04-05 08:21

We consider a system formed by an infinite viscous liquid layer with a constant horizontal temperature gradient, and a basic nonlinear bulk velocity profile. In the limit of long-wavelength and large nondimensional surface tension, we show that hydrotherma

III.PERTURBATIONTHEORY

Letusconsiderthefollowingperturbationstothebasicstate:

u=ub+ (u0+ u1+....),(13a)

w= 2(w0+ w1+...),(13b)

p=pb+ (p0+ p1+...),(13c)

θ=θb+ (θ0+ θ1+...),(13d)

η=ηb+ (η0+ η1+...),

where isasmallparameter.Next,weintroducetheslowvariablesaccordingto

ξ= (x ct),(13e)(14)

τ= 2t,(15)

andwesupposethattheperturbationsdependon(x,t)through(ξ,τ)only.Wenowmakemoreprecisethemeaningoflargealbeit niteforS,byassumingthat

S= 2

S~O( 0).

Weareable,atthispoint,toobtainanorderbyordersolutiontotheproblembyintegrationsinthezvariable.Ateachorder,thebulkequationsandtheboundaryconditionsatthebottomyieldu,w,θ,pintermsofthreearbitraryfunctions,whichwillbedeterminedintermsofη0bytheboundaryconditionsattheupperfreesurface.However,aswehavefourequations,acompatibilityconditionwillariseateachorder.Explicitly,atorder 0,weget:


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