Interpretation of palaeomonsoon dynamics on the Eastern Tibetan Plateau from a 10 kyr peat record of dust deposition and regional atmospheric model simulations
The Holocene evolution of the Asian monsoon remains poorly constrained due to the lack of information on past wind trajectories and intensities in central Asia. Mineral dust mobilized from aeolian deposits, transported by atmospheric currents and deposited in environmental archives such as peatlands...
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Imperial College London
2011
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.535459 |