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Dynamics
of the Agulhas Current Region |
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Region of Study Time Series |
Project
Description & Objectives Monitoring both the Agulhas transport into the South Atlantic in the upper kilometer of the ocean and the number of rings shed at its retroflection provides a means of detecting any substantial changes in inter-ocean water exchanges. After calibrating the observations with an array of inverted (IES) echo sounds, satellite altimetry has been used to estimate inter-ocean exchange between the Indian and Atlantic Oceans and has been maintained since 1993. The transfer of warm water from
the Indian Ocean to the South Atlantic subtropical gyre takes place in
the form of rings and filament formed when the Agulhas Current
retroflects south of Africa between 15°E and 25°E. It has been observed a closed
correlation between the transport of this current and the shedding of
rings (Goni et al, JMR, vol.55, 861-883, 1997). We provide here
the estimated time series of the location of the jet and of the
geostrophic transport of the Agulhas Current using a combination of
Satellite altimetry fields and climatological hydrography. Location of the Agulhas Current
jet Transport of the Agulhas Current Near-real time monitoring of
these
parameters Please direct your questions to: Gustavo Goni |
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