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

Item

ITEM ACTIONSEXPORT

Add to Basket

Local TagsRelease HistoryDetailsSummary

Released

Journal Article

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

Authors

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;

External Ressource

No external resources are shared

Fulltext (public)

There are no public fulltexts stored in PIKpublic

Supplementary Material (public)

There is no public supplementary material available

Citation

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

Abstract

There is no abstract available