Journal of Fluid Mechanics

  • Journal of Fluid Mechanics / Volume 676 / June 2011, pp 546-571
  • Copyright © Cambridge University Press 2011. The online version of this article is published within an Open Access environment subject to the conditions of the Creative Commons Attribution-NonCommercial-ShareAlike licence <http://creativecommons.org/licenses/by-nc-sa/2.5/>. The written permission of Cambridge University Press must be obtained for commercial re-use.
  • DOI: http://dx.doi.org/10.1017/jfm.2011.69 (About DOI), Published online: 27 April 2011
  • OPEN ACCESS

Papers

Low Rossby limiting dynamics for stably stratified flow with finite Froude number

BETH A. WINGATEa1 c1, PEDRO EMBIDa2, MIRANDA HOLMES-CERFONa3 and MARK A. TAYLORa4

a1 MS D413, Los Alamos National Laboratory, Los Alamos, NM 87544, USA

a2 Department of Mathematics and Statistics, the University of New Mexico, Albuquerque, NM 87131, USA

a3 New York University, Courant Institute of Mathematical Sciences, New York, NY 10012, USA

a4 Sandia National Laboratories, Albuquerque, NM 87185, USA

Abstract

In this paper, we explore the strong rotation limit of the rotating and stratified Boussinesq equations with periodic boundary conditions when the stratification is order 1 ([Rossby number] Ro = ε, [Froude number] Fr = O(1), as ε → 0). Using the same framework of Embid & Majda (Geophys. Astrophys. Fluid Dyn., vol. 87, 1998, p. 1), we show that the slow dynamics decouples from the fast. Furthermore, we derive equations for the slow dynamics and their conservation laws. The horizontal momentum equations reduce to the two-dimensional Navier–Stokes equations. The equation for the vertically averaged vertical velocity includes a term due to the vertical average of the buoyancy. The buoyancy equation, the only variable to retain its three-dimensionality, is advected by all three two-dimensional slow velocity components. The conservation laws for the slow dynamics include those for the two-dimensional Navier–Stokes equations and a new conserved quantity that describes dynamics between the vertical kinetic energy and the buoyancy. The leading order potential enstrophy is slow while the leading order total energy retains both fast and slow dynamics. We also perform forced numerical simulations of the rotating Boussinesq equations to demonstrate support for three aspects of the theory in the limit Ro → 0: (i) we find the formation and persistence of large-scale columnar Taylor–Proudman flows in the presence of O(1) Froude number; after a spin-up time, (ii) the ratio of the slow total energy to the total energy approaches a constant and that at the smallest Rossby numbers that constant approaches 1 and (iii) the ratio of the slow potential enstrophy to the total potential enstrophy also approaches a constant and that at the lowest Rossby numbers that constant is 1. The results of the numerical simulations indicate that even in the presence of the low wavenumber white noise forcing the dynamics exhibit characteristics of the theory.

(Received May 27 2009)

(Revised January 26 2011)

(Accepted February 08 2011)

(Online publication April 27 2011)

Key words:

  • quasi-geostrophic flows;
  • rotating flows;
  • stratified flows

Correspondence:

c1 Email address for correspondence: wingate@lanl.gov

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