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Study on potential evapotranspiration and wet-dry condition in the seasonal frozen soil region of northern Tibetan Plateau

ISSN号：1003-7578
期刊名称：《干旱区资源与环境》
时间：0
分类：P315.72[天文地球—地震学;天文地球—固体地球物理学;天文地球—地球物理学] S718.4[农业科学—林学]
作者机构：[1]Nagqu Station of Plateau Climate and Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China, [2]Chongqing Climate Center, Chongqing 401147, China, [3]Inner Mongolia Autonomous Region Meteorological Observatory, Hohhot, Inner Mongolia 010051, China, [4]Shaanxi Province Climate Center, Xi ＇ an, Shaanxi 710015, China
相关基金：Acknowledgments： We gratefully acknowledge the funding received from the National Key Programme for Developing Basic Sciences of China （2010CB951701）, Knowledge Innovation Program of the Chinese Academy of Sciences （KZCX2-YW-Q11-01）, Natural Science Foundation of China （40875005）, European Commission CEOP-AEGIS （Call FP7-ENV-2007-1 Grant No. 212921）, Gansu Science and Technology Key Project （1001JKDA001） and Natural Science Foundation of China for International Cooperation （40810059006）.

作者： HuiGen He[1,2], ZeYong Hu[1], XueYi Xun[1,3], Jun Sun[1], Li Hao[1,4], LiJiao Xu[1], Wen Peng[1]

关键词：季节性冻土地区, 青藏高原北部, 潜在蒸散量, 干湿, 半干旱气候, Penman, 自动气象站, 观测数据, northern Tibetan Plateau, seasonal frozen soil region, potential evapolranspimtion, dynamic and thermal effects, water factor, wet -dry condition

中文摘要：

Correspondence to： Prof. ZeYong Hu, Nagqu Station of Plateau Climate and Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences. No. 320 West Donggang Road, Lanzhou, Gansu 730000, China. Email： zyhu@lzb.ac.cn

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