Articles | Volume 21, issue 1
Nonlin. Processes Geophys., 21, 237–250, 2014
https://doi.org/10.5194/npg-21-237-2014
Nonlin. Processes Geophys., 21, 237–250, 2014
https://doi.org/10.5194/npg-21-237-2014

Research article 21 Feb 2014

Research article | 21 Feb 2014

An experimental study of regime transitions in a differentially heated baroclinic annulus with flat and sloping bottom topographies

M. Vincze1, U. Harlander1, Th. von Larcher2, and C. Egbers1 M. Vincze et al.
  • 1Department of Aerodynamics and Fluid Mechanics, Brandenburg University of Technology Cottbus-Senftenberg, Cottbus, Germany
  • 2Institute for Mathematics, Freie Universität Berlin, Berlin, Germany

Abstract. A series of laboratory experiments has been carried out in a thermally driven rotating annulus to study the onset of baroclinic instability, using horizontal and uniformly sloping bottom topographies. Different wave flow regimes have been identified and their phase boundaries – expressed in terms of appropriate non-dimensional parameters – have been compared to the recent numerical linear stability analysis of von Larcher et al. (2013). In the flat bottom case, the numerically predicted alignment of the boundary between the axisymmetric and the regular wave flow regime was found to be consistent with the experimental results. However, once the sloping bottom end wall was introduced, the detected behaviour was qualitatively different from that of the simulations. This disagreement is thought to be the consequence of nonlinear wave–wave interactions that could not be resolved in the framework of the numerical study. This argument is supported by the observed development of interference vacillation in the runs with sloping bottom, a mixed flow state in which baroclinic wave modes exhibiting different drift rates and amplitudes can co-exist.

Download