A possible generation mechanism for internal waves near the edge of a submesoscale eddy

Recently, it has been shown for the first time by observations that an anticyclonic mesoscale eddy can generate internal waves (wavelengths of 0.4 to 1 km) that carry energy away from the eddy. In the present study, we investigate a possible mechanism for generating internal waves near the edge of a...

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Veröffentlicht in:Tellus. Series A, Dynamic meteorology and oceanography Dynamic meteorology and oceanography, 2021-01, Vol.73 (1), p.1-11
Hauptverfasser: Chunchuzov, I.P., Johannessen, O.M., Marmorino, G.O.
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Sprache:eng
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