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The data suggested that during this period the Sahara started losing its vegetation. The reduced plant growth led to increased airborne dust which cooled the Indian Ocean, shifted the atmospheric circulation patterns and caused a condition similar to today’s El Niño events.

This ultimately led to a large reduction in monsoon moisture across Southeast Asia that lasted more than 1,000 years

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les The team collected stalagmite samples from the caves in Laos and examined the oxygen, carbon isotopes and trace metals. They also conducted different modelling and paleoclimate experiments. <span>The data suggested that during this period the Sahara started losing its vegetation. The reduced plant growth led to increased airborne dust which cooled the Indian Ocean, shifted the atmospheric circulation patterns and caused a condition similar to today’s El Niño events. This ultimately led to a large reduction in monsoon moisture across Southeast Asia that lasted more than 1,000 years, says Kathleen Johnson in a release. She is an associate professor of Earth system science at the University of California and one of the corresponding authors of the paper published in


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