Abstract
Current numerical models of oceanic circulation differentiate between the eddy diffusion and viscosity transport along the geopotential horizontal and vertical directions only. In order to model the effect of anisotropic turbulence as diffusive transport along and across
Cite
CITATION STYLE
APA
Kirwan, A. D. (1983). On “Oceanic Isopycnal Mixing By Coordinate Rotation.” Journal of Physical Oceanography, 13(7), 1318–1319. https://doi.org/10.1175/1520-0485(1983)013<1318:oimbcr>2.0.co;2
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free