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New evidence for a reduced water balance in East Africa during the Last Glacial Maximum: Implication for model-data comparison.
Some syntheses of lake-level data for the Last Glacial Maximum (LGM) in East Africa (10degreesN and 30degreesS, East of 25degreesE) show apparently wetter conditions than present for some basins, whereas palaeovegetation reconstruction indicates a generally dry climate. PMIP GCM simulations for the
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