Bounds on dissipation for Navier-Stokes flow with Kolmogorov forcing

Citation
S. Childress et al., Bounds on dissipation for Navier-Stokes flow with Kolmogorov forcing, PHYSICA D, 158(1-4), 2001, pp. 105-128
Citations number
25
Categorie Soggetti
Physics
Journal title
PHYSICA D
ISSN journal
01672789 → ACNP
Volume
158
Issue
1-4
Year of publication
2001
Pages
105 - 128
Database
ISI
SICI code
0167-2789(20011015)158:1-4<105:BODFNF>2.0.ZU;2-K
Abstract
In this paper, bounds on average viscous dissipation are derived for Kolmog orov flow in a spatially periodic domain with steady and unsteady forcing, at arbitrarily large Grash of number G. For a force of the form F-0 sin mzi or F-0 sin mz cos omega ti, we derive various bounds on the total dissipat ion in the flow, D-u,, as well as on the dissipation D-m obtained from the x-velocity averaged over the x, y plane (the mean velocity of the flow). We derive upper bounds on D-u and D-v = D-u - D-m, as well as lower bounds on D-m and D-m /D-u, adopting constraints of the kind introduced by Howard an d Busse and assuming a steady force. The background flow method introduced by Doering and Constantin is used to obtain an improved lower bound on D-m/ D-u of O(G(-1)), and a lower bound on D-u, of O(G(-1/2)) where G := F0L3/nu (2) is the Grashof number. Some of these results are then generalized to t ime-periodic forcing. Direct numerical simulation of the flow indicates tha t these bounds leave substantial gaps at large Grashof number G, the calcul ated D-m (G) and D-u (G) being 0 (G(-1/2)) and O(1), respectively, as G --> infinity. Our theoretical bounds on D-m, D-u are shown to be attained by s teady laminar-type flows for neighboring forcing functions, which seems to indicate that these bounds cannot be improved by adding further dynamical c onstraints. However, our elementary upper bound on D-v can probably be impr oved by placing more constraints on the flows. These results serve to empha size the difference between boundary-driven turbulence and body-force drive n turbulence where the appropriate dissipation bound is believed saturated at least up to logarithms. (C) 2001 Elsevier Science B.V. All rights reserv ed.