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- W1884718507 abstract "[1] Diapycnal mixing caused through breaking of large-amplitude internal lee waves generated by sub-inertial diurnal tides, which are modulated with a 18.6-year period, is hypothesized to be fundamental to both the intermediate-layer ventilation and the bi-decadal oscillation around the North Pacific Ocean. The first observational evidence of such wave breaking is presented here. The breaking wave observed had ∼200 m height and ∼1 km width, and its associated diapycnal mixing was estimated to be ∼1.5 m2 s−1, with a temporal average ∼104 times larger than typical values in the open oceans. Our estimate suggests that a similar mixing process occurs globally, particularly around the Pacific and Antarctic Oceans." @default.
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- W1884718507 date "2010-02-01" @default.
- W1884718507 modified "2023-10-10" @default.
- W1884718507 title "Breaking of unsteady lee waves generated by diurnal tides" @default.
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- W1884718507 doi "https://doi.org/10.1029/2009gl041456" @default.
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