FRONTAL CONVERGENCE CAUSES SEDIMENT TRAPPING IN THE HUDSON RIVER ESTUARY
The trapping of sediment involves the interplay of resuspension, tidal advection and frontogenesis. During flood tides, resuspension tends to be maximal, and the sediment is transported rapidly landward. During the early ebb, the sediment flux reverses, but as the ebb progresses, the near-bottom salinity gradient becomes concentrated in certain zones due to topographic effects. The gradient increases to form bottom fronts, behind which the ebbing flow becomes weak or may even reverse. The flow convergence at these fronts causes rapid convergence of sediment transport. A stunning example of this convergence process was observed in late May, 2001, based on timeseries data from a bottom tripod. Frontal convergence resulted in high concentrations of sediment during the late ebb, which settled during slack water to produce 20 cm of sediment deposition over approximately 1 hour. The following flood remobilized most of the sediment, leaving several cm of net deposition. This intense trapping process continued over several spring-tide periods between late May and late June, yielding approximately 20 cm of net deposition.