This rapid transition 5,500 years ago from a warm humid and wet environment to what we have today stems from a cooling of northern high latitudes. The cooler temperatures in the north weakened the high altitude Tropical Easterly Jet, which consistently brought moisture into northern Africa. Due to the weakening of the Tropical Easterly Jet, the African Easterly Jet strengthened, which indirectly i... more

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Sarah Terris
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