School of Geographic Sciences, Nantong University, 999 Tongjing Road, Nantong, 226007, China
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Yujie He
Chinese Research Academy of Environmental Sciences, No.8 Dayangfang, Chaoyang District, 100012, Beijing, China
Department of Ecosystem and Landscape Dynamics, Institute for Biodiversity and
Ecosystem Dynamics, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands
Jianjun Chen
College of Geomatics and Geoinformation, Guilin University of Technology, 12 Jiangan Road, Guilin, 541004, China
Guangxi Key Laboratory of Spatial Information and Geomatics, 12 Jiangan Road, Guilin, 541004, China
Qingbai Wu
State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Yu Qin
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment
and Resources, Chinese Academy of Sciences, 320 Donggang West Road, 730000, Lanzhou, Gansu, China
Key Laboratory of Ecohydrology of Inland River Basin, Chinese Academy of Sciences, Lanzhou 730000, China
University of Chinese Academy Sciences, Beijing, 100049, China
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Cumulative views and downloads
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Total article views: 3,241 (including HTML, PDF, and XML)
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Total article views: 4,041 (including HTML, PDF, and XML)
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Total article views: 3,241 (including HTML, PDF, and XML)
Thereof 2,980 with geography defined
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Total article views: 800 (including HTML, PDF, and XML)
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Coarse-fragment soil on the Qinghai–Tibetan Plateau has different thermal and hydrological properties to soils commonly used in modeling studies. We took soil samples and measured their physical properties in a laboratory, which were used in a model to simulate their effects on permafrost dynamics. Model errors were reduced using the measured properties, in which porosity played an dominant role.
Coarse-fragment soil on the Qinghai–Tibetan Plateau has different thermal and hydrological...
