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Atlantic Ocean

Brazil-Malvinas Confluence region

Image of the month - February 2005

The region of Confluence of the Brazil and Malvinas Currents (Southwest Atlantic) is a very energetic complex region. Contrasts in sea surface temperature, in Chlorophyll-a concentration and the local maximum in eddy kinetic energy make satellite infrared (IR) color imagery and satellite altimetry particularly appropriate tools to study the Confluence region.
Data from satellites provide valuable information in this area, which, like most of the southern hemisphere oceans, has few in situ time series observations. Satellite data provide information about spatial scales as small as 1 km (e.g. filaments are visible with MODIS) to several hundred of kilometers (Zapiola Rise) and from time scales of 24 hours to more than 10 years.

The variability of thermal fronts is discussed with nine years of AVHRR data (1987-1995) using a gradient based edge detector [Saraceno et al., 2004].
The time-space distribution of chlorophyll-a is examined using 6 years (1998-2003) of sea surface color images from SeaWiFS [Saraceno et al., 2005].
Root mean square of Sea Level Anomaly obtained from 11 years of Sea Surface Height from ERS + Topex/Poseidon + Jason-1. Dash-dot lines are mean position of Brazil Current Front and Subantarctic Front (SAF).

 

 

These means fields allow to establish biophysical provinces in the South West Atlantic ocean:
   - Background colors represent the six ranges of chl-a magnitudes identified with an histogram method.
   - Regions obtained (solid black lines) retrieves Longhurst (1998) Provinces (dash-dot red lines).
   - Three new provinces are identified: the Overshoot, the Patagonian Shelf Break (PSB) and the Zapiola Rise Provinces (Saraceno, 2005).
 
SATL: South Atlantic Gyral Province
SSTC: South Subtropical Convergence Province
BRAZ: Brazil Current Costal Province
FLKD: Southwest Atlantic Shelves Province
SANT: Subantartic Water Ring Province

Simultaneous high resolution (1.1 km) MODIS SST and color images document the meso- and sub-meso-scale structures [Barré et al., 2005].

References

  • Saraceno, M., C. Provost, A. R. Piola, J. Bava, and A. Gagliardini, Brazil Malvinas Frontal System as seen from 9 years of advanced very high resolution radiometer data, J. Geophys. Res., 109, C05027, doi:10.1029/2003JC002127, 2004.
  • Saraceno, M., C. Provost, A. R. Piola, On the relationship of satellite retrieved surface temperature fronts and chlorophyll-a in the Western South Atlantic, JGR, 110, C11016, doi:10.1029/2004JC002736, 2005.
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