Abstract

We hereby present two different spectral methods for calculating the density anomaly and the vertical energy flux from synthetic Schlieren data, for a periodic field of linear internal waves (IW) in a density-stratified fluid with a uniform buoyancy frequency. The two approaches operate under different assumptions. The first method (hereafter Mxzt) relies on the assumption of a perfectly periodic IW field in the three dimensions (x, z, t), whereas the second method (hereafter MxtUp) assumes that the IW field is periodic in x and t and composed solely of wave components with downward phase velocity. The two methods have been applied to synthetic Schlieren data collected in the CNRM large stratified water flume. Both methods succeed in reconstructing the density anomaly field. We identify and quantify the source of errors of both methods. A new method mixing the two approaches and combining their respective advantages is then proposed for the upward energy flux. The work presented in this article opens new perspectives for density and energy flux estimates from laboratory experiments data.

Highlights

  • Ocean circulation is forced mechanically by wind stress at the surface and vertical mixing in the interior [1]

  • The conversion rate from the barotropic tide to internal waves is obtained by integrating the vertical energy flux wδp T over a control surface above the topography

  • We have presented two different spectral methods for calculating the density and the vertical energy flux from synthetic Schlieren measurement data, valid for a periodic field of linear internal waves in a density-stratified fluid with a uniform buoyancy frequency N

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Summary

Introduction

Ocean circulation is forced mechanically by wind stress at the surface and vertical mixing in the interior [1]. Here, two methods for the retrieval of the density field, the velocity fields, the pressure perturbation field and the energy flux solely from synthetic Schlieren data They are designed for experiments in which internal waves are excited by a bottom periodic topography oscillating horizontally and wave reflections in the horizontal direction and from the surface are prevented. A similar condition was effectively used by Clark and Sutherland in a study of the internal waves generated by an oscillating cylinder [14] They did not investigate whether the experimental data supported the assumption that the diagnosed region contained no reflected waves, as will be done here, and the uncertainty of the measured energy flux was very large (a factor of ten).

Methods
The Mxzt Method
The MxtUp Method
Vertical Energy Flux
Results
Evaluation of the Methods on Analytic Fields
Analytic IW Fields
Validation and Comparison of Reconstructed Fields
Application to Experimental Data
Presentation of the Laboratory Experiments
Sketch
Density
10. Spectrum
Discussion and Conclusions
Full Text
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