Improved bounds on horizontal convection

被引:7
|
作者
Rocha, Cesar B. [1 ]
Bossy, Thomas [2 ]
Smith, Stefan G. Llewellyn [3 ,4 ]
Young, William R. [4 ]
机构
[1] Woods Hole Oceanog Inst, Dept Phys Oceanog, Woods Hole, MA 02543 USA
[2] Ecole Normale Super Lyon, F-69007 Lyon, France
[3] Univ Calif San Diego, Dept Mech & Aerosp Engn, 9500 Gilman Dr, La Jolla, CA 92093 USA
[4] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA
关键词
ocean circulation; variational methods; ENERGY;
D O I
10.1017/jfm.2019.850
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
For the problem of horizontal convection the Nusselt number based on entropy production is bounded from above by C Ra-1/3 as the horizontal convective Rayleigh number Ra -> infinity for some constant C (Siggers et al., J. Fluid Mech., vol. 517, 2004, pp. 55-70). We re-examine the variational arguments leading to this `ultimate regime' by using the Wentzel-Kramers-Brillouin method to solve the variational problem in the Ra -> infinity limit and exhibiting solutions that achieve the ultimate Ra(1/)3 scaling. As expected, the optimizing flows have a boundary layer of thickness similar to Ra-1/3 pressed against the non-uniformly heated surface; but the variational solutions also have rapid oscillatory variation with wavelength similar to Ra-1/3 along the wall. As a result of the exact solution of the variational problem, the constant C is smaller than the previous estimate by a factor of 2.5 for no-slip and 1.6 for no-stress boundary conditions. This modest reduction in C indicates that the inequalities used by Siggers et al. (J. Fluid Mech., vol. 517, 2004, pp. 55-70) are surprisingly accurate.
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页数:21
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