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 |
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Sprache: | eng |
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