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The result was to shift the intertropical convergence zone southwards.

The debris ends up concentrated by circular, clockwise ocean currents within an oblong-shaped convergence zone.

Dr James Renwick says small changes to the South Pacific convergence zone can also add to dramatic weather variability.

The results show that the convergence zone is clearly visible at between 56.5 and 57 degrees south.

These droughts resulted from something completely new to scientists: unusually warm Atlantic sea-surface temperatures, which shifted the rain-bearing inter-tropical convergence zone northward of the Amazon.