Thermohaline intrusions created isopycnically at oceanic fronts are inclined to isopycnals
- 1 July 1986
- journal article
- Published by Springer Nature in Nature
- Vol. 322 (6078) , 446-449
- https://doi.org/10.1038/322446a0
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- The response of the upper ocean to solar heating. I: The mixed layerQuarterly Journal of the Royal Meteorological Society, 1986
- The GATE Lagrangian Batfish ExperimentDeep Sea Research Part A. Oceanographic Research Papers, 1985
- On the Parameterization of Diapycnal Fluxes due to Double-Diffusive IntrusionsJournal of Physical Oceanography, 1982
- Redistribution of scalars during upper ocean frontogenesis: A numerical modelQuarterly Journal of the Royal Meteorological Society, 1980
- The vertical length scale of double-diffusive intrusionsDeep Sea Research Part A. Oceanographic Research Papers, 1979
- Thermohaline intrusions lie across isopycnalsNature, 1979
- Double-diffusive intrusions into a density gradientJournal of Geophysical Research, 1978
- Microstructure and fine structure in an upper ocean frontal regimeJournal of Geophysical Research, 1978
- A Note on the Lateral Mixing of Water MassesJournal of Physical Oceanography, 1977
- Wave-induced shear instability in the summer thermoclineJournal of Fluid Mechanics, 1968