The effect of secondary circulation on the salt distribution in a sinuous coastal plain estuary: Satilla River, GA, USA

• Published in: Continental shelf research Vol. 29; no. 1; pp. 15 - 28
• Main Authors: Seim, H.E., Blanton, J.O., Elston, S.A.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.01.2009
• Subjects: Axial salinity distribution; Brackish; Channel meanders; Freshwater; Lateral salinity distribution; Marine; Neap–spring cycle; Salt exchange; Secondary circulation; Stratification; USA; ASW, USA, Georgia, Satilla R; Salt exchange; Channel meanders; Secondary circulation; Lateral salinity distribution; Stratification; Neap–spring cycle; Axial salinity distribution
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2008.03.018

An analysis of observational data suggests salt exchange in a sinuous coastal plain estuary is significantly impacted by counter-rotating residual horizontal eddies formed by channel curvature in meandering channels. The parts of adjacent eddies that advect material downstream follow the deep part of the channel where the flow continually criss-crosses from one side of the channel to the other and follows a relatively unimpeded trajectory to the sea. On the other hand, the parts of adjacent eddies that advect material upstream cross the channel at a different location where it encounters a series of shoals. In this case, the resulting upstream transport of salt is relatively inefficient and retards the rate at which salt can disperse upstream into the estuary. The strength of these circulations is modulated by the spring/neap cycle, allowing for a stronger gravitational mode of exchange to develop near neap tides, but has minimal impact on the length of the salt intrusion. It is suggested that the impeded upstream salt transport accounts for the observation that an impulse of river discharge advects a given isohaline 10 km downstream in 20 days, but that after the impulse, 70 days are required to return the isohaline to a similar position, counter to the notion of a simple dependence of intrusion length on river discharge.