A two-dimensional prognostic model was employed to examine the mutualintrusion of a gravity current and the formation of a density front.The results indicated strong vertical motion near the front and,with Earth rotation included, a baroclinic alongshore jet. Comparisonwith observations from the New England shelf-slope front indicatedthat the model gives a realistic description of the frontal structureand the mean southward current.
CITATION STYLE
Wang, D.-P. (1984). Mutual Intrusion of a Gravity Current and Density Front Formation. Journal of Physical Oceanography, 14(7), 1191–1199. https://doi.org/10.1175/1520-0485(1984)014<1191:mioagc>2.0.co;2
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