Moisture-advection feedback supports strong early-to-mid Holocene monsoon 
climate on the eastern Tibetan Plateau as inferred from a pollen-based 
reconstruction

Herzschuh, U.; Borkowski, J.; Schewe, Jacob; Mischke, S.; Tian, F.

doi:10.1016/j.palaeo.2014.02.022

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Moisture-advection feedback supports strong early-to-mid Holocene monsoon climate on the eastern Tibetan Plateau as inferred from a pollen-based reconstruction

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Herzschuh, U.
Potsdam Institute for Climate Impact Research and Cooperation Partners;

Borkowski, J.
Potsdam Institute for Climate Impact Research and Cooperation Partners;

/persons/resource/Schewe

Schewe, Jacob
Potsdam Institute for Climate Impact Research;

Mischke, S.
Potsdam Institute for Climate Impact Research and Cooperation Partners;

Tian, F.
Potsdam Institute for Climate Impact Research and Cooperation Partners;

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Herzschuh, U., Borkowski, J., Schewe, J., Mischke, S., Tian, F. (2014): 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, 402, 44-54.
https://doi.org/10.1016/j.palaeo.2014.02.022

Cite as: https://publications.pik-potsdam.de/pubman/item/item_19537

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