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Beaver Dam Locations from sub-meter resolution Satellite Imagery, 2010-2019, ...
Arctic landscapes are in a state of transition due to changes in climate occurring during both the summer and winter seasons. Scattered observations indicate that beavers... -
Mapped thermokarst ice wedge polygon patterns from GeoEye-1, 2010, Cape Mamon...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Database of Quaternary Deposits from Maps, East and Central Siberia (RU)
This digital database is the product of collaboration between the U.S. Geological Survey, the Alfred Wegener Institute for Polar and Marine Research Potsdam, Foothill College... -
Mapped yedoma ice wedge polygon patterns from GeoEye-1, 2010, Cape Mamontov K...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Beaver Dam Locations from sub-meter resolution Satellite Imagery, 2002-2019, ...
Arctic landscapes are in a state of transition due to changes in climate occurring during both the summer and winter seasons. Scattered observations indicate that beavers... -
Database of Ice-Rich Yedoma Permafrost (IRYP)
We synthesized data on the circum-Arctic and sub-Arctic distribution and thickness of Yedoma for compiling a preliminary circum-polar Yedoma map. For compiling this map, we used... -
Mapped thermokarst ice wedge polygon patterns from GeoEye-1, 2009, Buor Khaya...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Mapped yedoma ice wedge polygon patterns from WorldView-1, 2009, Ebe-Basyn-Si...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Mapped thermokarst ice wedge polygon patterns from WorldView-1, 2009, Ebe-Bas...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Surface Water Area from sub-meter resolution Satellite Imagery, 2002-2019, Ko...
Arctic landscapes are in a state of transition due to changes in climate occurring during both the summer and winter seasons. Scattered observations indicate that beavers... -
Mapped yedoma ice wedge polygon patterns from GeoEye-1, 2009, Buor Khaya, Lap...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Mapped thermokarst ice wedge polygon patterns from WorldView-1, 2008, Norther...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and... -
Mapped yedoma ice wedge polygon patterns from WorldView-1, 2008, Northern Sew...
Detailed calculations of ground-ice volumes in permafrost deposits are necessary to understand and quantify the response of permafrost landscapes to thermal disturbance and...