Aspect of oscillatory along-shelf flow in the vicinity of an isolated submarine canyon
Résumé
Selected results are presented from a closely coupled laboratory-numerical model study of the
oscillatory flow of a linearly stratified fluid in the vicinity of an isolated submarine canyon. It is shown that the
boundary condition applied along the model floor in the numerical experiments is critically important in having
the numerical model simulate the laboratory experiments. Furthermore, it is shown that enhanced viscosities,
which assure the numerical stability, must be applied with care because they may change the flow fields. A
scaling argument is advanced which predicts the strength of the time-mean flow generated by the background
current.The sensitivity of the flow field to changes in some of the system parameters is discussed. Finally, some
initial results for flows generated in the presence of boundary turbulence are also discussed.
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