Formation of a shelfbreak front by freshwater discharge

• Published in: Dynamics of atmospheres and oceans Vol. 36; no. 1; pp. 103 - 124
• Main Authors: Narayanan, Chandrasekher, Garvine, Richard W.
• Format: Journal Article Conference Proceeding
• Language: English
• Published: Amsterdam Elsevier B.V 01.11.2002; Elsevier Science
• Subjects: Bottom boundary layer; Coastal currents; Dynamics of the ocean (upper and deep oceans); Earth, ocean, space; Exact sciences and technology; External geophysics; Freshwater discharge; Fronts; Marine; Physics of the oceans; Shelfbreak front; Mid-Atlantic Bight; Coastal currents; Shelfbreak front; Freshwater discharge; Bottom boundary layer; Fronts; Continental shelf; Fresh water; Estuaries; Empirical relation; Primitive equation; Oceanic front; Rivers; Kelvin wave; Three dimensional model; Wave propagation; Coastal current; Numerical simulation; Localization; Boundary layer
• ISSN: 0377-0265; 1872-6879
• DOI: 10.1016/S0377-0265(02)00027-1

The circulation and transport of freshwater generated by an idealized buoyant source is studied using a three-dimensional primitive equation model. Freshwater enters the continental shelf, turns anticyclonically and moves downstream in the direction of Kelvin wave propagation. In the region close to the source, the flow reaches an equilibrium in the bottom boundary layer so that freshwater does not spread offshore any further. This offshore equilibrium distance increases as we move downstream until the freshwater is able to feel the presence of the shelfbreak. A shelfbreak front forms and the shelfbreak prevents any further offshore spreading of freshwater in the bottom boundary layer. Two complimentary mechanisms are responsible for the slow cross-shelf migration of freshwater and subsequent trapping of shelfbreak fronts: bottom stress and topographic changes. The shelfbreak creates an active, dynamic process preventing leakage from the continental shelf region to the slope region. However, the dynamical process that traps the front to the shelfbreak is still unclear. The location of the shelfbreak front depends on four dimensionless parameters: scaled inlet volume transport, scaled breadth, scaled “diffusivity” and scaled shelf width. We develop empirical relations for predicting the location of the frontal bottom intersection, given these parameters.