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Estimation of the Mean Annual Surface Temperature and Surface Frost Number Using the MODIS Land Surface Temperature Products for Mapping Permafrost in China
permafrost MAST surface frost number remote sensing MODIS, China
2013/9/2
n this paper, we propose a pragmatic scheme for estimation of MAST and surface frost number, based on the assumption that the average of maximum and minimum land surface temperature (LST) represents t...
Monitoring and modeling the infl uence of snow pack and organic soil on a permafrost active layer, Qinghai – Tibetan Plateau of China
Qinghai–Tibetan Plateau Active layer Organic soil Snow pack CoupModel
2013/9/2
As a result of global warming, the depth of the permafrost active layer on the Qinghai–Tibet Plateau (QTP) hasbeen increasing progressively during thepast few decades. The Cold and Arid Regions Enviro...
OBJECT BASED THERMOKARST LAKE CHANGE MAPPING AS PART OF THE ESA DATA USER ELEMENT (DUE) PERMAFROST
lake change Hexagon Rapideye thermokarst arctic relational features
2014/6/12
This study presents an approach to quantify thermokarst lake change and lake object structure change in spatial very high resolution remote sensing data as part of ESAs "Data User Element Permafrost"....