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 ORCID: https://orcid.org/0000-0003-0999-1261, Borkowski, Janett, Schewe, J., Mischke, Steffen and Tian, Fang
;
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Ulrike.Herzschuh [ at ] awi.de
Abstract
Item Type
Article
Authors
Herzschuh, Ulrike ORCID: https://orcid.org/0000-0003-0999-1261, Borkowski, Janett, Schewe, J., Mischke, Steffen and Tian, Fang
;
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Primary Division
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
.
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