De-xing, W., Shi-zuo, F. The dynamic effects of a finite depth ambient fluid on bottom eddy., Chin. J. Ocean. Limnol. 13, 124–133 (1995). https://doi.org/10.1007/BF02846817
DOI:
De-xing, W., Shi-zuo, F. The dynamic effects of a finite depth ambient fluid on bottom eddy., Chin. J. Ocean. Limnol. 13, 124–133 (1995). https://doi.org/10.1007/BF02846817DOI:
The dynamic effects of a finite depth ambient fluid on bottom eddy
摘要
Abstract
Scaling analysis shows that ifo(ε2
β1ε
γ)∼o(δ)
frontal geostrophic dynamics governs the behavior of an isolated bottom eddy in a finite depth ambient fluid; and that the ambient flow induced by bottom eddy migration satisfies quasi-geostrophic dynamics. This two layer model includes the important processes of advection of bottom eddy due to ambient flow
baroclinic instability
and form drag introduced by Rossby waves. The numerical results show that the three processes enhance the instability and alter the migration speed of the bottom eddy
and that the form drag induces a significant meridional drift of the eddy.
关键词
Keywords
references
Arakawa, A., 1966. Computational design for long term integration of the equations of fluid motion: Two-dimentional incompressible flow, Part 1.J. Comput. Phys. 1: 119–143.
Flierl, G. R., 1984. Rossby wave radiation from a strongly nonlinear warm eddy.J. Phys. Oceanogr. 14: 47–58.
Mory, M., Stern, M. E. and Griffiths, R. W. et al., 1987. Coherent baroclinic eddies on a sloping bottom.J. Fluid Mech. 183: 45–62.
Nof, D., 1983. The translation of isolated cold eddies on a sloping bottom.Deep Sea Res. 30: 171–182.
Whitehead, J. A., Stern, M. E., Flierl, G. R., et al., 1990. Experimental observations of baroclinic eddies on a sloping bottom.J. Geophys. Res. 95(C6): 9585–9610.
Wu Dexing and Feng Shizuo, 1993. On the behaviors of ocean bottom eddy.Chin. J. Oceanol. Limnol. 12 (4): 343–350.
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