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Scale interactions between an internal seiche and double diffusion

N. Castro-Folker* and M. Stastna

  • Department of Applied Mathematics, University of Waterloo, Ontario N2L 3G1, Canada

  • *ncastrof@uwaterloo.ca

Phys. Rev. Fluids 8, 034801 – Published 7 March, 2023

DOI: https://doi.org/10.1103/PhysRevFluids.8.034801

Abstract

We investigate the interaction between laboratory scale internal seiches and double-diffusive instabilities in the diffusive-convection regime using two-dimensional, high-resolution numerical simulations. A natural separation exists between the scale of the seiche and the scale of the mature instability. We report on how instabilities are modulated by, and how they modulate, the internal seiches. We find that seiche evolution leads to an earlier onset of instabilities compared to either an initially still fluid with a flat (i.e., seiche-free) interface, or an initially flat interface with an imposed stable shear current. We find that double-diffusion increases the buoyancy frequency and thereby decreases the period of the seiche. We interpret both mechanisms using existing internal wave theories. Additionally, we find that the combined viscous dissipation due to double-diffusive structures and shear stress induced by the seiche is greater than the viscous dissipation produced by either phenomenon in isolation. We discuss implications for more realistic configurations in which the internal seiche degenerates into a nonlinear internal wave train, how the observed mutual modulation may or may not manifest at the field scale, and how the full equation of state for sea water causes double-diffusive structures to grow asymmetrically in contrast to results using a linear equation of state.

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