Moisture-Advection Feedback Supports Strong Early-To-Mid Holocene Monsoon Climate on the Eastern Tibetan Plateau as Inferred From a Pollen-Based Reconstruction
Palaeogeography, Palaeoclimatology, Palaeoecology - Netherlands
doi 10.1016/j.palaeo.2014.02.022
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Date
May 1, 2014
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Elsevier BV