GC12C:
The Third Pole Environment (TPE) under Global Changes II

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Session ID#: 15546

Session Description:
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. Like the Arctic and Antarctica, the 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 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 Third Pole atmosphere, cryosphere, hydrosphere, and biosphere and their interactions with global change. Related contributions are welcomed.
Primary Convener:  Tandong Yao, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Conveners:  Lonnie G Thompson, Ohio State University Main Campus, School of Earth Sciences, Columbus, OH, United States, Volker Mosbrugger, Senckenberg, Frankfurt, Germany and Fan Zhang, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Chairs:  Lonnie G Thompson, Ohio State University Main Campus, School of Earth Sciences, Columbus, OH, United States, Volker Mosbrugger, Senckenberg, Frankfurt, Germany and Tandong Yao, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
OSPA Liaison:  Volker Mosbrugger, Senckenberg, Frankfurt, Germany

Cross-Listed:
  • A - Atmospheric Sciences
  • B - Biogeosciences
  • C - Cryosphere
  • H - Hydrology
Index Terms:

1616 Climate variability [GLOBAL CHANGE]
1621 Cryospheric change [GLOBAL CHANGE]
1631 Land/atmosphere interactions [GLOBAL CHANGE]
1655 Water cycles [GLOBAL CHANGE]

Abstracts Submitted to this Session:

Fahu Chen, Lanzhou University, MOE Key Lab of Western China's Environmental System, Lanzhou, China, Dongju Zhang, Lanzhou University, MOE Key Laboratory of Western China's Environmental Systems, College of Earth Environmental Sciences, Lanzhou, China and Guanghui Dong, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, China
Melanie Marie Perello, Indiana University Purdue University Indianapolis, Indianapolis, IN, United States, Broxton W Bird, Indiana University Purdue University Indianapolis, Department of Earth Sciences, Indianapolis, IN, United States, Yanbin Lei, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, Pratigya J Polissar, Lamont-Doherty Earth Observatory, Palisades, United States, Lonnie G Thompson, Ohio State University Main Campus, School of Earth Sciences, Columbus, OH, United States and Tandong Yao, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Binita Phartiyal, Birbal Sahni Institute of Paleosciences, Lucknow, India
Juzhi Hou1, Mingda Wang1, Yue He1 and Jie Liang2, (1)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (2)Chinese Academy of Sciences, Beijing, China
Debarati NAG, Birbal Sahni Institute of Palaeobotany, Lucknow, India and Binita Phartiyal, Birbal Sahni Institute of Paleosciences, Lucknow, India
Jussi Griessinger1, Achim Braeuning1, Haifeng Zhu Sr.2, Eryuan Liang3, Jakob Wernicke Jr.1 and Philipp Hochreuther1, (1)University of Erlangen-Nuremberg, Erlangen, Germany, (2)Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (3)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Yangjian Zhang, IGSNRR Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China