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¡¡¡¡Cryospheric observation has been initiated in 1958 in China marked as the first glaciolo-gy station established at the headwater of Urumqi River£¬ Tianshan in the west of China.Later£¬ stations in cryospheric region of China have been gradually constructed. Consider thevast area in the western plateau and mountainous regions£¬ these stations are far from satisfy-ing the needs for scientific research and operational applications. Since the year 1998£¬ a cam-paign named Innovation Reform was launched by the Chinese Academy of Sciences £¨CAS£© £¬designing and constructions of field observational stations have been speeded up. In the last15 years£¬ mainly through CAS and China Meteorological Administration £¨CMA£©£¬ stationsthat observing cryospheric components cover the major geography units of the cold regions inChina comprises a fairly nice network£¬ although still leave some geographic gaps in west Ti-bet and northeast China. With the deep understanding of regional climate system£¬ the ob-served variables at these stations are no longer limited to cryopshere itself£¬ but also interac-tions of cryosphere with other spheres such as atmosphere and biosphere. For instance£¬ au-tomatic weather stations£¬ eddy covariance£¬ boundary layer structures£¬ land surface processesinclucling hydrological and ecological processes are also observed. These observations enableto investigate cryospheric change dynamics and their effects on other spheres£¬