Sediment in the Río de La Plata

(Click on image for larger view.)

On March 31, 2012, the Moderate Resolution Imaging Spectrometer (MODIS) on the Terra satellite captured this view of muddy water from the Paranà River flowing into the Río de La Plata, a funnel-shaped estuary on the eastern coast of South America with a drainage area that covers about 20 percent of the continent.

The Paraná River, the second longest river in South America after the Amazon, provides three-quarters of the water that enters the estuary, with the remainder arriving from the Uruguay River. Topsoil running off agricultural fields upstream and flowing into the Paranà as a result of rainstorms likely produced the heavy load of brown sediment visible in the river water.

The image offers a glimpse of the complicated mixing processes that occur at the interface of the muddy fresh water from the Paranà and the ocean water of the South Atlantic in an area known as a turbidity front. The location of the turbidity front varies over the course of the year. It tends to be in its westernmost position during the summer when river discharge is at a minimum and the predominant winds are from the northeast, while it reaches its easternmost position in the spring when strong winds from the southwest are present.

References:
Framinan, M. (1999) Study of the Río de la Plata Turbidity Front, Part 1: Spatial and Temporal Distribution. Continental Shelf Research, 1259-1267.
Acha, E. (2008) An Overview of Physical and Ecological Processes in the Río de la Plata Estuary. Continental Shelf Research. 28(13) 1579-1588.
NASA image by Jeff Schmaltz, LANCE/EOSDIS MODIS Rapid Response. Caption by Adam Voiland.

Instrument:
Terra - MODIS