HESS Hydrology and Earth System Sciences HESS Hydrol. Earth Syst. Sci. 1607-7938 Copernicus Publications Göttingen, Germany 10.5194/hess-13-1103-2009 Recent advances on the study of atmosphere-land interaction observations on the Tibetan Plateau Ma Y. 1 2 Wang Y. 1 Wu R. 1 Hu Z. 2 Yang K. 1 Li M. 2 Ma W. 2 Zhong L. 1 Sun F. 2 Chen X. 1 Zhu Z. 1 Wang S. 1 Ishikawa H. 3 Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China Disaster Prevention Research Institute, Kyoto University, Kyoto 611-0011, Japan 09 07 2009 13 7 1103 1111 Copyright: © 2009 Y. Ma et al. 2009 This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/ This article is available from https://hess.copernicus.org/articles/13/1103/2009/hess-13-1103-2009.html The full text article is available as a PDF file from https://hess.copernicus.org/articles/13/1103/2009/hess-13-1103-2009.pdf

As a unique geological and geographical unit, the Tibetan Plateau dramatically impacts the world's environment and especially controls climatic and environmental changes in China, Asia and even in the Northern Hemisphere. Tibetan Plateau, therefore, provides a field laboratory for studying global change. With support from various agencies in the People's Republic of China, a Tibetan Observation and Research Platform (TORP) is now implementing. Firstly the background of the establishment of the TORP, the establishing and monitoring plan of long-term scale (5–10 years) of the TORP has been introduced. Then the preliminary observational analysis results, such as the characteristics of land surface heat fluxes and CO<sub>2</sub> flux partitioning (diurnal variation and inter-monthly variation etc.), the characteristics of atmospheric and soil variables, the structure of the Atmospheric Boundary Layer (ABL) and the turbulent characteristics have also been shown in this paper.

 European Commission CEOP-AEGIS - Coordinated Asia-European long-term Observing system of Qinghai – Tibet Plateau hydro-meteorological processes and the Asian-monsoon systEm with Ground satellite Image data and numerical Simulations (212921) References Asanuma, J., Ishikawa H., Tamagawa, I., Ma, Y., Hayashi, T., Qi, Y., and Wang, J.: Application of the band-pass covariance technique to portable flux measurements over the Tibetan Plateau, Water Resour. Res., 41, W09407, https://doi.org/10.1029/2005WR003954, 2005. Chen, X., Ma, Y., Sun, F., Li, M., and Wang, S.: The rainy season character of tropsphere at Mt. Qomolangma Region, Plateau Meteorology, 26(6), 1280–1286, 2007. Chen, X., Ma, Y., Li, M., Ma, W., and Wang, H.: Analyses on near surface layer atmospheric characteristics and soil features in northern Tibetan Plateau, Plateau Meteorology, 27(5), 941–948, 2008. 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