Articles | Volume 6, issue 2
https://doi.org/10.5194/os-6-563-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.On the numerical resolution of the bottom layer in simulations of oceanic gravity currents
Related subject area
Approach: Numerical Models | Depth range: Bottom Boundary Layer | Geographical range: All Geographic Regions | Phenomena: Temperature, Salinity and Density Fields
Reconstructing bottom water temperatures from measurements of temperature and thermal diffusivity in marine sediments
Ocean Sci., 11, 559–571,
2015Cited articles
Coleman, G. N., Ferziger, J. H., and Spalart, P. R.: A numerical study of the turbulent Ekman layer, J. Fluid. Mech., 213, 313–348, 1990.
Ezer, T.: Entrainment, diapycnal mixing and transport in three-dimensional bottom gravity current simulations using the Mellor-Yamada turbulence scheme, Ocean Model., 9, 151–168, 2005.
Ezer, T. and Mellor, G. L.: A generalized coordinate ocean model and a comparison of the bottom boundary layer dynamics in terrain-following and in z-level grids, Ocean Model., 6, 379–403, 2004.
Ezer, T. and Weatherly, G. L.: A numerical study of the interaction between a deep cold jet and the bottom boundary layer of the ocean? J. Phys. Oceanogr., 20, 801–816, 1990.
Griffiths, R. W.: Gravity currents in rotating systems, Ann. Rev. Fluid Mech., 18, 59–89, 1986.