Diapycnal flow through the Georges Bank tidal front: A dye tracer study

A fluorescent dye tracer, Fluorescein, injected into the bottom mixed layer at the seaward edge of the tidal front on Georges Bank has provided the fi rst quantitative measurement of an on-bank diapycnal Lagrangian flow throug h the front. From the warming of the dye patch, 2.5x10(-6) degreesC/s and 7 .8x10(-6) degreesC/s on the south flank and northeast peak respectively, as it passed through the frontal temperature gradient we infer an on-bank flo w of 1.9 cm/s on the south flank and 3.2 cm/s on the northeast peak. The he at flux required for this warming is predominantly due to vertical mixing w ithin the tidal front. These observations further demonstrate the utility o f direct Lagrangian measurements and provide quantitative estimates of the cross-frontal exchange on Georges Bank, the focus of the U.S GLOBEC Northwe st Atlantic/Georges Bank Phase III program.