Dynamic Response of Glaciers on the Tibetan Plateau to Climate Change
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©TU Berlin
DynRG-TiP Project
The project took part within the DFG (Deutsche Forschung Gemeinschaft) Priority Programme 1372:
"Tibetan Plateau: Formation-Climate-Ecosystems" (TiP)
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Fig.1: One day on Zhadang Glacier,
click to start animation!
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© T.P. - TU Dresden, F.M. - Chair of Climatology
Like Antarctica and the Arctic, the Tibetan Plateau (TiP) is a key area of the globe. It is a determining factor
for the Asian Monsoon system, and its glaciers are characteristic elements of the natural environment, forming water
resources of cardinal importance for both ecosystems and millions of people living in the surrounding regions.
Within a large consortium of Chinese and German research teams, the TU Berlin, in association with the
TU Dresden
and the
RWTH Aachen
focused on the Glaciers evolution and response in the last decades.
Because of their remoteness, relatively few is known about Tibetan glacier's response to climate change:
this encouraged further studies of high relevance. The central goal of the project was to improve our understanding
of atmosphere-cryosphere interactions on the TiP by adding new data and improved methods combining field studies
(meteorology and climatology, glaciology and glacial hydrology), remote sensing and numerical modelling.
Field studies and remote sensing analyses were focused on glaciers in the Nyainqentanglha Mountains near Nam Co, where the
Institute of Tibetan Plateau Research (ITP)
of the Chinese Academy of Sciences (CAS) operates a research station.
Events and Activities:
- 14.-18. January 2013, Oberjoch:
2nd BMBF-TiP Central Asia Young Scientists Meeting
- 16.-20. January 2012, Oberjoch: BMBF-TiP Central Asia Young Scientists Meeting
- 2.-6. March 2011, Hamburg, Germany: 7th Sino-German Workshop on Tibetan Plateau Research
Research Activities:
Field Investigations
Three field campaigns where carried out in close cooperation with the ITP, they ended successfully
with the installation of two Automatic Weather Stations on the Zhadang Glacier.
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© TU Berlin
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Remote Sensing
Remote sensing techniques are essential for all research activities within the project. A glacier
inventory for the whole Nyainqentanglha range was generated using automated remote sensing and GIS.
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© T.B. - TU Dresden
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Numerical Modelling
Regional Atmospheric Modelling
Glaciological Modelling
A framework combining glaciological and atmospherical models is currently in development. The
system is based on the state-of-the-art Weather Research and Forecasting (WRF-ARW) modeling system.
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© F.M. - Chair of Climatology
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