Primary Convener:
Shilong Piao, Peking University

Convener:
Lonnie Thompson, Ohio State University Main Campus
Andreas Mulch, Senckenberg Biodiversity and Climate Research Centre (SBiK-F)
Fan Zhang, Chinese Academy of Sciences

Chair:
Shilong Piao, Peking University
Lonnie Thompson, Ohio State University Main Campus
Tao Wang, Institute of Tibetan Plateau Research, Chinese Academy of Sciences

The Tibetan Plateau and surrounding mountain regions, known as the Third Pole, cover an area of > 5 million km² and are considered to be the water tower of Asia. The Pan Third Pole expands on both the north-south and the east-west directions, going across the Tibetan Plateau, Pamir, Hindu Kush, Iran Plateau, Caucasian and Carpathian, covering an area of about 20 million km². Like the Arctic and Antarctica, the Pan Third Pole’s environment is extremely sensitive to global climate change. In recent years, scientists from around the globe have increased observational, remote sensing and numerical modeling research related to the Pan Third Pole in an effort to quantify and predict past, current and future scenarios. Co-sponsored by TPE (www.tpe.ac.cn), this session is dedicated to studies of Pan Third Pole atmosphere, cryosphere, hydrosphere, and biosphere and their interactions with global change. Related contributions are welcomed.

Index Terms
1616 Climate variability
1621 Cryospheric change
1631 Land|atmosphere interactions
1655 Water cycles

Neighborhoods:
3. Earth Covering