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Observations of Shoaling Density Current Regime Changes in Internal Wave Interactions ArchiMer
Solodoch, Aviv; Molemaker, Jeroen M.; Srinivasan, Kaushik; Berta, Maristella; Marie, Louis; Jagannathan, Arjun.
We present in situ and remote observations of a Mississippi plume front in the Louisiana Bight. The plume propagated freely across the bight, rather than as a coastal current. The observed cross-front circulation pattern is typical of density currents, as are the small width (approximate to 100 m) of the plume front and the presence of surface frontal convergence. Acomparison of observations with stratified density current theory is conducted. Additionally, subcritical to supercritical transitions of frontal propagation speed relative to internal gravity wave (IGW) speed are demonstrated to occur. That is in part due to IGW speed reduction with decrease in seabed depth during the frontal propagation toward the shore. Theoretical steady-state density...
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Ano: 2020 URL: https://archimer.ifremer.fr/doc/00667/77867/80010.pdf
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Why Does the Deep Western Boundary Current “Leak” around Flemish Cap? ArchiMer
Solodoch, Aviv; Mcwilliams, James C.; Stewart, Andrew L.; Gula, Jonathan; Renault, Lionel.
The southward flowing deep limb of the Atlantic Meridional Overturning Circulation is comprised of both the Deep Western Boundary Current (DWBC) and interior pathways. The latter are fed by “leakiness” from the DWBC in the Newfoundland Basin. However, the cause of this leakiness has not yet been explored mechanistically. Here the statistics and dynamics of the DWBC leakiness in the Newfoundland Basin are explored using two float data sets and a high-resolution numerical model. The float leakiness around Flemish Cap is found to be concentrated in several areas (“hotspots”) that are collocated with bathymetric curvature and steepening. Numerical particle advection experiments reveal that the Lagrangian mean velocity is offshore at these hotspots, while...
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Ano: 2020 URL: https://archimer.ifremer.fr/doc/00630/74184/73787.pdf
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