Rio de la Plata estuarine system: Relationship between river flow and frontal variability

• Published in: Advances in space research 2008, Vol.41 (11), p.1876-1881
• Main Authors: Nagy, G.J., Severov, D.N., Pshennikov, V.A., De los Santos, M., Lagomarsino, J.J., Sans, K., Morozov, E.G.
• Format: Article
• Language: English
• Subjects: Climate change; ENSO; Rio de la Plata estuary; River flow; SeaWIFS frontal variability
• ISSN: 0273-1177; 1879-1948
• DOI: 10.1016/j.asr.2007.11.027

This paper deals with the application of SeaWIFS images to characterize spatial and temporal variability of fronts in the Rio de la Plata estuarine system over the period 2000–2003. We aim to depict the relationship between river outflow and variability of fronts’ loci on monthly to ENSO-related timescales and the influence of the winds along Rio de la Plata (axial winds) on the abrupt changes in frontal dynamics over synoptic timescales. During the studied period both La Niña (July 1999–June 2000) and El Niño (April 2002–May 2003) events induced significant displacements of fronts. Three distinct fronts were analyzed between river, estuarine, coastal and marine waters of the Rio de la Plata: Main Turbidity Front, Main Marine Front, and Secondary Marine Front. Their number, location and separation seem to be mainly related to river outflow and second, to fresh (>8 m/s) axial winds. During low discharge periods (i.e. summer time and/or La Niña events) these winds induce abrupt changes in the location of fronts (100–200 km) and greater separation between them over synoptic timescale, whereas during high river discharge or ENSO years some of the variability of fronts location is explained by the river’s outflow fluctuations, especially by the high variability of the River Uruguay discharge.