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Redistribution of energy available for ocean mixing by long-range propagation of internal waves

Matthew H. Alford ()
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Matthew H. Alford: University of Washington

Nature, 2003, vol. 423, issue 6936, 159-162

Abstract: Abstract Ocean mixing, which affects pollutant dispersal, marine productivity and global climate1, largely results from the breaking of internal gravity waves—disturbances propagating along the ocean's internal stratification. A global map of internal-wave dissipation would be useful in improving climate models, but would require knowledge of the sources of internal gravity waves and their propagation. Towards this goal, I present here computations of horizontal internal-wave propagation from 60 historical moorings and relate them to the source terms of internal waves as computed previously2,3. Analysis of the two most energetic frequency ranges—near-inertial frequencies and semidiurnal tidal frequencies—reveals that the fluxes in both frequency bands are of the order of 1 kW m-1 (that is, 15–50% of the energy input) and are directed away from their respective source regions. However, the energy flux due to near-inertial waves is stronger in winter, whereas the tidal fluxes are uniform throughout the year. Both varieties of internal waves can thus significantly affect the space-time distribution of energy available for global mixing.

Date: 2003
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DOI: 10.1038/nature01628

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