Frozen soil degradation and its effects on surface hydrology in the northern Tibetan Plateau

Frozen soil was simulated at six seasonally frozen and seven permafrost stations over the northern Tibetan Plateau using the Variable Infiltration Capacity (VIC) model for the period of 1962–2009. The VIC model resolved the seasonal cycle and temporal evolution of the observed soil temperatures and...

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Vydáno v:	Journal of geophysical research. Atmospheres Ročník 120; číslo 16; s. 8276 - 8298
Hlavní autoři:	Cuo, Lan, Zhang, Yongxin, Bohn, Theodore J., Zhao, Lin, Li, Jialuo, Liu, Qiming, Zhou, Bingrong
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Washington Blackwell Publishing Ltd 27.08.2015
Témata:	Air temperature Base flow climate change Conduction heating Conductive heat transfer Daily temperatures Degradation Environmental degradation Evapotranspiration Frozen ground frozen soil degradation Frozen soils Geophysics Heat conduction Hydrologic processes hydrological modeling Hydrology Ice Ice melting Infiltration capacity Liquids Long-term changes Moisture content Permafrost Plateaus Precipitation Precipitation effects Seasonal variation Soil Soil (material) Soil degradation Soil layers Soil moisture Soil temperature Soil temperature effects Stations surface hydrology Temperature effects the Tibetan Plateau Trends Tibetan Plateau China, People's Rep., Xizang, Tibetan Plateau
ISSN:	2169-897X, 2169-8996
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