Intense upper ocean mixing due to large aggregations of spawning fish
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://www.nature.com/articles/s41561-022-00916-3.pdf
Reference59 articles.
1. Thorpe, S. A. The Turbulent Ocean (Cambridge Univ. Press, 2005).
2. Winters, K. B., Lombard, P. N., Riley, J. J. & D’Asaro, E. A. Available potential energy and mixing in density-stratified fluids. J. Fluid Mech. 289, 115–128 (1995).
3. Osborn, T. R. Estimates of the local rate of vertical diffusion from dissipation measurements. J. Phys. Oceanogr. 10, 83–89 (1980).
4. Oakey, N. S. Determination of the rate of dissipation of turbulent energy from simultaneous temperature and velocity shear microstructure measurements. J. Phys. Ocean. 12, 256–271 (1982).
5. Smyth, W. D. & Moum, J. N. Marginal instability and deep cycle turbulence in the eastern equatorial Pacific Ocean. Geophys. Res. Lett. 40, 6181–6185 (2013).
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