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Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data

Author

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  • G. D. Egbert

    (College of Oceanic and Atmospheric Sciences, Oregon State University)

  • R. D. Ray

    (NASA Goddard Space Flight Center, Code 926)

Abstract

How and where the ocean tides dissipate their energy are long-standing questions1 that have consequences ranging from the history of the Moon2 to the mixing of the oceans3. Historically, the principal sink of tidal energy has been thought to be bottom friction in shallow seas4,5. There has long been suggestive evidence6,7, however, that tidal dissipation also occurs in the open ocean through the scattering by ocean-bottom topography of surface tides into internal waves, but estimates of the magnitude of this possible sink have varied widely3,8,9,10,11. Here we use satellite altimeter data from Topex/Poseidon to map empirically the tidal energy dissipation. We show that approximately 1012 watts—that is, 1 TW, representing 25–30% of the total dissipation—occurs in the deep ocean, generally near areas of rough topography. Of the estimated 2 TW of mixing energy required to maintain the large-scale thermohaline circulation of the ocean12, one-half could therefore be provided by the tides, with the other half coming from action13 on the surface of the ocean.

Suggested Citation

  • G. D. Egbert & R. D. Ray, 2000. "Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data," Nature, Nature, vol. 405(6788), pages 775-778, June.
    • Handle: RePEc:nat:nature:v:405:y:2000:i:6788:d:10.1038_35015531
    DOI: 10.1038/35015531
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    Cited by:

    1. Hemer, Mark A. & Manasseh, Richard & McInnes, Kathleen L. & Penesis, Irene & Pitman, Tracey, 2018. "Perspectives on a way forward for ocean renewable energy in Australia," Renewable Energy, Elsevier, vol. 127(C), pages 733-745.
    2. Roger Samsó & Júlia Crespin & Antonio García-Olivares & Jordi Solé, 2023. "Examining the Potential of Marine Renewable Energy: A Net Energy Perspective," Sustainability, MDPI, vol. 15(10), pages 1-35, May.
    3. Martí Barclay, Vicky & Neill, Simon P. & Angeloudis, Athanasios, 2023. "Tidal range resource of the Patagonian shelf," Renewable Energy, Elsevier, vol. 209(C), pages 85-96.
    4. Robins, Peter E. & Neill, Simon P. & Lewis, Matt J. & Ward, Sophie L., 2015. "Characterising the spatial and temporal variability of the tidal-stream energy resource over the northwest European shelf seas," Applied Energy, Elsevier, vol. 147(C), pages 510-522.
    5. Hermann, Weston A., 2006. "Quantifying global exergy resources," Energy, Elsevier, vol. 31(12), pages 1685-1702.
    6. Zhibin Yang & Zhao Jing & Xiaoming Zhai & Clément Vic & Hui Sun & Casimir Lavergne & Man Yuan, 2024. "Enhanced generation of internal tides under global warming," Nature Communications, Nature, vol. 15(1), pages 1-8, December.
    7. Campbell, Daniel E., 2016. "Emergy baseline for the Earth: A historical review of the science and a new calculation," Ecological Modelling, Elsevier, vol. 339(C), pages 96-125.

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