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

hdl:10013/epic.48764

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

Herzschuh, Ulrike

, Borkowski, Janett, Schewe, J., Mischke, Steffen and Tian, Fang ;

Contact

Ulrike.Herzschuh [ at ] awi.de

Abstract

Item Type

Article

Authors

Herzschuh, Ulrike

, Borkowski, Janett, Schewe, J., Mischke, Steffen and Tian, Fang ;

Divisions

AWI Organizations > Geosciences > Permafrost Research

Primary Division

Organizations > AWI Organizations > Geosciences > Permafrost Research

Programs

Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales

Primary Topic

Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales

Publication Status

Published

Eprint ID

41948

Cite as

Herzschuh, U. , Borkowski, J. , Schewe, J. , Mischke, S. and 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), pp. 44-54 .