Amplitude vacillation in baroclinic flows

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Abstract

This chapter will introduce the phenomenology of vacillation in baroclinic flows based on experimental data, CFD and low-order numerical models. The processes leading to vacillation of a steady baroclinic wave will be discussed in terms of nonlinear interactions between different wave modes and between waves and the azimuthally or longitudinally averaged baroclinic flow. Complementing the review of the literature on amplitude vacillation, some new material will be presented to discuss the effect of the presence of lateral boundary layers in laboratory experiments and of the Prandtl number on feedback between the vacillating waves and the Ekman transport in the boundary layers. In the later sections, other forms of vacillation will be discussed and, finally, the role of vacillation in the transition to chaos and turbulence will be briefly addressed.
Original languageEnglish
Title of host publicationModelling Atmospheric and Oceanic Flow
Subtitle of host publicationInsights from laboratory experiments and numerical simulations.
EditorsThomas von Larcher, Paul D. Williams
PublisherWiley
Pages61-81
Number of pages21
ISBN (Print)978-1-118-85593-5
Publication statusPublished - 2015

Keywords

  • geophysical Fluid dynamics
  • rotating fluids
  • coherent structure
  • Chaos
  • Turbulence

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