Late glacial to Holocene climate and vegetation changes on the Tibetan Plateau inferred from fossil pollen records in lacustrine sediments

Late glacial to Holocene climate and vegetation changes on the Tibetan Plateau inferred from fossil pollen records in lacustrine sediments

The past climate in central Asia, and especially on the Tibetan Plateau (TP), is of great importance for an understanding of global climate processes and for predicting the future climate. As a major influence on the climate in this region, the Asian Summer Monsoon (ASM) and its evolutionary history...

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Bibliographic Details
Main Author: Wang, Yongbo
Format: Doctoral Thesis
Language:English
Published: Universität Potsdam 2011
Subjects:
Asiatischer Sommermonsun
ASM
Holozän
Seesedimente
Pollen
Hochland von Tibet
Asian Summer Monsoon
Holocene
Lake sediments
Tibetan Plateau
Earth sciences
Online Access:http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-63155
http://opus.kobv.de/ubp/volltexte/2013/6315/

Internet

http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-63155
http://opus.kobv.de/ubp/volltexte/2013/6315/

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