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Stability of stratified downslope flows with an overlying stagnant isolating layer

Published online by Cambridge University Press:  25 November 2016

Arjun Jagannathan*
Affiliation:
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA
Kraig B. Winters
Affiliation:
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA
Laurence Armi
Affiliation:
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA
*
Email address for correspondence: agjagann@ucsd.edu

Abstract

We investigate the dynamic stability of stratified flow configurations characteristic of hydraulically controlled downslope flow over topography. Extraction of the correct ‘base state’ for stability analysis from spatially and temporally evolving flows that exhibit instability is not easy since the observed flow in most cases has already been modified by nonlinear interactions between the instability modes and the mean flow. Analytical studies, however, can yield steady solutions under idealized conditions which can then be analysed for stability. Following the latter approach, we study flow profiles whose essential character is determined by recently obtained solutions of Winters & Armi (J. Fluid Mech., vol. 753, 2014, pp. 80–103) for topographically controlled stratified flows. Their condition of optimal control necessitates a streamline bifurcation which then naturally produces a stagnant isolating layer overlying an accelerating stratified jet in the lee of the topography. We show that the inclusion of the isolating layer is an essential component of the stability analysis and further clarify the nature and mechanism of the instability in light of the wave-interaction theory. The spatial stability problem is also briefly examined in order to estimate the downstream location where finite-amplitude features might be manifested in streamwise slowly varying flows over topography.

Type
Papers
Copyright
© 2016 Cambridge University Press 

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References

Armi, L. & Mayr, G. J. 2007 Continuously stratified flows across an alpine crest with a pass: shallow and deep föhn. Q. J. R. Meteorol. Soc. 133 (623), 459477.Google Scholar
Baines, P. G. & Mitsudera, H. 1994 On the mechanism of shear flow instabilities. J. Fluid Mech. 276, 327342.Google Scholar
Bell, T. Jr. 1974 Effects of shear on the properties of internal gravity wave modes. Deutsche Hydrografische Zeitschrift 27 (2), 5762.Google Scholar
Beluši’c, D., Pasarić, M. & Orlić, M. 2004 Quasi-periodic bora gusts related to the structure of the troposphere. Q. J. R. Meteorol. Soc. 130 (598), 11031121.CrossRefGoogle Scholar
Carpenter, J. R., Balmforth, N. J. & Lawrence, G. A. 2010 Identifying unstable modes in stratified shear layers. Phys. Fluids 22 (5), 054104.Google Scholar
Carpenter, J. R., Tedford, E. W., Heifetz, E. & Lawrence, G. A. 2011 Instability in stratified shear flow: review of a physical interpretation based on interacting waves. Appl. Mech. Rev. 64 (6), 060801.Google Scholar
Clark, T. L. & Farley, R. D. 1984 Severe downslope windstorm calculations in two and three spatial dimensions using anelastic interactive grid nesting: a possible mechanism for gustiness. J. Atmos. Sci. 41 (3), 329350.Google Scholar
Farmer, D. & Armi, L. 1999 Stratified flow over topography: the role of small-scale entrainment and mixing in flow establishment. Proc. R. Soc. Lond. A 455, 32213258.CrossRefGoogle Scholar
Gaster, M. 1962 A note on the relation between temporally-increasing and spatially-increasing disturbances in hydrodynamic stability. J. Fluid Mech. 14 (2), 222224.CrossRefGoogle Scholar
Howard, L. N. 1961 Note on a paper of John W. Miles. J. Fluid Mech. 10 (4), 509512.Google Scholar
Huerre, P., Batchelor, G. K., Moffatt, H. K. & Worster, M. G. 2000 Open shear flow instabilities. In Perspectives in Fluid Dynamics, pp. 159229. Cambridge University Press.Google Scholar
Lilly, D. K. 1978 A severe downslope windstorm and aircraft turbulence event induced by a mountain wave. J. Atmos. Sci. 35 (1), 5977.Google Scholar
Long, R. R. 1955 Some aspects of the flow of stratified fluids. III. Continuous density gradients. Tellus 7, 341357.Google Scholar
Miles, J. W. 1961 On the stability of heterogeneous shear flows. J. Fluid Mech. 10 (4), 496508.Google Scholar
Moum, J. N., Farmer, D. M., Smyth, W. D., Armi, L. & Vagle, S. 2003 Structure generation of turbulence at interfaces strained by internal solitary waves propagating shoreward over the continental shelf. J. Phys. Oceanogr. 33 (10), 20932112.Google Scholar
Peltier, W. R. & Scinocca, J. F. 1990 The origin of severe downslope windstorm pulsations. J. Atmos. Sci. 47 (24), 28532870.Google Scholar
Scinocca, J. F. & Peltier, W. R. 1989 Pulsating downslope windstorms. J. Atmos. Sci. 46 (18), 28852914.2.0.CO;2>CrossRefGoogle Scholar
Smith, R. B. 1985 On severe downslope winds. J. Atmos. Sci. 42 (23), 25972603.2.0.CO;2>CrossRefGoogle Scholar
Smith, R. B. 1991 Kelvin–Helmholtz instability in severe downslope wind flow. J. Atmos. Sci. 48 (10), 13191324.Google Scholar
Tisseur, F. & Meerbergen, K. 2001 The quadratic eigenvalue problem. SIAM Rev. 43 (2), 235286.Google Scholar
Winters, K. B. 2016 The turbulent transition of a supercritical downslope flow: sensitivity to downstream conditions. J. Fluid Mech. 792, 9971012.Google Scholar
Winters, K. B. & Armi, L. 2014 Topographic control of stratified flows: upstream jets, blocking and isolating layers. J. Fluid Mech. 753, 80103.Google Scholar
Winters, K. B. & Riley, J. J. 1992 Instability of internal waves near a critical level. Dyn. Atmos. Oceans 16 (3–4), 249278.CrossRefGoogle Scholar

Jagannathan et al. supplementary movie

Isopycnals from a statistically steady state non-linear simulation of stratified flow over a smooth topography for the optimal upstream solution of Winters and Armi (2014). The spatial development of finite amplitude billow structures in the lee region can be observed in this movie.

Download Jagannathan et al. supplementary movie(Video)
Video 7.8 MB