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W. D. Smyth and J. N. Moum Marginal instability and deep cycle turbulence in the eastern equatorial Pacific Ocean Geophysical Research Letters 40

Version of Record online: 8 DEC 2013 | DOI: 10.1002/2013GL058403

Key Points

  • Deep cycle turbulence in the equatorial Pacific ocean is marginally unstable
  • Marginal instability indicates the presence of sheared, stratified turbulence
  • Marginal instability can be assessed using historical data

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