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Remote sensing-based permafrost region disturbances: retrogressive thaw slump...
The data quantify the abundance and distribution of the permafrost region disturbance (PRD) of retrogressive thaw slumps, using trend analyses of 30-m-resolution Landsat imagery... -
Distribution of pingos from an IfSAR digital surface model, 2002-2006, wester...
A detailed attributed point feature shapefile of 1247 pingo locations was manually assembled from a 5m resolution digital surface model (DSM) derived from an airborne... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, AD3 Adventdalen, Sv...
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Land Surface Feature Classification from TerraSAR-X, 2013, Lena Delta, Lap...
Land surface features (water, wetland, tundra, and bare surfaces) were classified from TerraSAR-X with a resolution of 5 m for August 2012 and July 2014. The product is based on... -
Frozen State Backscatter Intensity from Sentinel-1, 2015-2016, Usa Basin, Eur...
Frozen state backscatter intensity was derived from Sentinel-1 acquisitions from December 2015 and 2016. By excluding the effects of liquid water content (acquisitions under... -
Coastal Retrogressive Thaw Slumps from GeoEye-1, WorldView-2 and Aerial Photo...
Coastal retrogressive thaw slumps (RTSs) were manually digitized at a 1:2000 scale using ArcMap (ESRI, version 10.3) from high‐resolution satellite images acquired in July (13... -
Remote sensing-based permafrost region disturbances: fire, 1999-2015, Eastern...
The data quantify the abundance and distribution of the permafrost region disturbance (PRD) wildfire, using trend analyses of 30-m-resolution Landsat imagery from 1999-2015 and... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, IWS Adventdalen, Sv...
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
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... -
Trend analysis of lake dynamics from Landsat time-series 1999-2014, Central Y...
The dataset was created with a methodology based on machine-learning based classification of robust trends of multi-spectral indices of Landsat data (TM,ETM+, OLI) and... -
Quantification of shoreline movements from satellite remote sensing, 1951-201...
The Arctic is warming, but the impacts on its coasts are not well documented. To better understand the reaction of Arctic coasts to increasing environmental pressure, shoreline... -
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... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, Act-IWS Adventdalen...
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Remote sensing-based permafrost region disturbances: fire, 1999-2015, Alaska ...
The data quantify the abundance and distribution of the permafrost region disturbance (PRD) wildfire, using trend analyses of 30-m-resolution Landsat imagery from 1999-2015 and... -
Remote sensing-based permafrost region disturbances: lakes, 1999-2014, Alaska...
The data quantify the abundance and distribution of the permafrost region disturbance (PRD) of lakes and their dynamics, using trend analyses of 30-m-resolution Landsat imagery...