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The article of record as published may be located at http://dx.doi.org/10.1002/2014JC009947 The layered structure of stratification and mixing on the New England Shelf (NES) in summer is examined by analyzing a comprehensive set of observations of hydrography, currents and turbulence. A clear distinction in mixing characteristics between the midcolumn water (consisting of subsurface stratification, middepth weak stratification and lower-layer stratification) and a well-mixed bottom boundary layer (BBL) is revealed. The combination of subtidal Ekman onshore bottom transport and cross-shore density gradient created a lower-layer stratification that inhibited the upward extension of the BBL turbulence. The BBL mixing was related to strong shear generated by bottom stress, and the magnitude and periodic variation of BBL mixing was determined by both the tidal and subtidal flows. Mixing in the midcolumn water occurred under stably stratified conditions and showed correspondence with the occurrence of near-inertial and semidiurnal internal waves. Positive correlations between buoyancy frequency squared (N2) and shear variance (S2), S2 and dissipation rate (e), N2 and e are established in the midcolumn, but not in the BBL. The midcolumn e was reasonably described by a slightly modified MacKinnon-Gregg (MG) model. The field component of this program was jointly supported by the US Office of Naval Research (grants N00014-95-1-1030, N00014-95-1-0373, and N00014-96-1- 0953) and Fisheries and Oceans of Canada. |
