Internal lee waves are a player in ocean dynamics that may make an important contribution to deep-ocean mixing. They warrant serious consideration for inclusion in the next generation of climate models.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Schiermeier, Q. Nature 447, 522–524 (2007).
Nikurashin, M. & Ferrari, R. Geophys. Res. Lett. 40, 3133–3137 (2013).
Alford, M. H. et al. J. Phys. Oceanogr. 41, 2211–2222 (2011).
MacKinnon, J., Laurent, L. S. & Garabato, A. N. in Ocean Circulation and Climate: A 21st Century Perspective 2nd edn (eds Siedler, G., Griffies, S., Gould, J. & Church, J.) (Academic, 2013).
Melet, A., Hallberg, R., Legg, S. & Polzin, K. J. Phys. Oceanogr. 43, 602–615 (2013).
Talley, L. D. Oceanography 26, 80–97 (2013).
Polzin, K. L. Ocean Modelling 30, 298–309 (2009).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
MacKinnon, J. Mountain waves in the deep ocean. Nature 501, 321–322 (2013). https://doi.org/10.1038/501321a
Published:
Issue Date:
DOI: https://doi.org/10.1038/501321a