GC13J:
The Third Pole Environment (TPE) under Global Changes III

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Session ID#: 15551

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:  Tandong Yao, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, Volker Mosbrugger, Senckenberg, Frankfurt, Germany and Lonnie G Thompson, Ohio State University Main Campus, School of Earth Sciences, Columbus, OH, United States
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:

Jade A DAlpoim Guedes, Washington State University, Pullman, WA, United States
Kun Yang, Chinese Academy of Sciences, Institute of Tibetan Plateau Research, Beijing, China; Center for Earth System Science, Tsinghua University, Beijing, China, Franco Salerno, CNR Water Research Institute, Bari, Italy, Lin Ouyang, Chinese Academy of Sciences, Beijing, China, Nicolas Guyennon, CNR National Research Council, water research institute, Rome, Italy, Lide Tian, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Gianni Tartari, Ev-K2-CNR Committee, Bergamo, Italy
Dr. Dambaru Ballab Kattel, PhD1, Tandong Yao1, Kalim Ullah2 and G M Tarekul Islam3, (1)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (2)COMSATS Institute of Information Technology, Department of Meteorology, Abbottabad, Pakistan, (3)Bangladesh University of Engineering and Technology, Institute of Water and Flood Management, Dhaka, Bangladesh
Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Yongxin Zhang, National Center for Atmospheric Research, Research Applications Laboratory, Boulder, United States
Lei Zhong1, Yaoming Ma2, Weiqiang Ma3, Mijun Zou1 and Yuanyuan Hu1, (1)University of Science and Technology of China, Hefei, China, (2)Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Land-Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment (TPESRE), Beijing, China, (3)Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Land-Atmosphere Interaction and its Climatic Effects Group, State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Beijing, China
Kalim Ullah, Department of Meteorology, COMSATS Institute of Information Technology, Islamabad, Pakistan and Dr. Dambaru Ballab Kattel, PhD, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Jing Gao, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China