The front on the Northern Flank of Georges Bank in spring : 2. Cross-frontal fluxes and mixing

buoyancy fluxes are downward and most intense, reaching values of 5 � 10 � 7 W/kg, near the bottom at the edge of the bank and decrease both on- and off-bank. Horizontal, crossbank buoyancy fluxes are partitioned into mean, tidal pumping, and nontidal eddy components and are computed as a function of cross-isobath/vertical position by averaging in the along-isobath direction. The tidal pumping component is dominant over most of the cross-bank section with a peak value of � 1 � 10 � 4 W/kg, directed off-bank near the bank edge. A diagnosed tidal vertical velocity field is used with mean buoyancy gradients to compute the along-isopycnal skew flux. The horizontal component of this skew flux has similar spatial structure and magnitude to that of the observed tidal pumping flux. The divergent component of the skew flux, at depths above the bottom boundary layer, appears to be convergent north of the bank edge and divergent at the bank edge, suggesting that tidally driven advective processes drive buoyant bank water downward and off-bank at mid-depth and force the upwelling of deep, dense water near the bottom at the bank edge. INDEX TERMS: 4528 Oceanography: Physical: Fronts and jets; 4568 Oceanography: Physical: Turbulence, diffusion, and mixing processes; 4560 Oceanography: Physical: Surface waves and tides (1255); 4544 Oceanography: Physical: Internal and inertial waves; KEYWORDS: Georges Bank, tidal mixing front, GLOBEC, internal tide, skew eddy flux, turbulent mixing

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