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Mapped polygon pattern geomorphometry from HRSC-AX, 2009, IWS Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, HCP Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, CALM Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, AD4 Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, AD3 Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, AD2 Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, Act-IWS Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, Isdammen Adventdalen, Svalbard (NO)
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
Geomorphological main terraces from Landsat 2000-2001, Lena Delta, Laptev and East Siberian Sea Region (RU)
This data set provides a detailed inventory of lakes in the Lena Delta, northern Siberia, with respect to the lakes' association with one of the three geomorphological main... -
Arctic Coastal Dynamics Classification Database
An important outcome of Arctic Coastal Dynamics I was the segmentation and characterization of the entire circum-Arctic coastline by regional experts which is presented in this... -
Robust trends of landscape dynamics in the Arctic Lena Delta with temporally dense Landsat time-series stacks
The robust Theil-Sen regression algorithm was used to calculate trend parameters (slope, intercept, confidence intervals) on Landsat time-series stack in the north-east Siberian... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 62°N - 64°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 60°N - 62°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 58°N - 60°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 56°N - 58°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 54°N - 56°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 52°N - 54°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 18N, 50°N - 52°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 17N, 62°N - 64°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,... -
Trends of Land Surface Change from Landsat time-series 1999-2014, Eastern Canada, UTM Zone 17N, 60°N - 62°N (CA)
The Hot Spot Regions of Permafrost Change (HRPC) product maps changes in surface characteristics using the full Landsat archive (TM, ETM+, OLI) for the peak summer season (July,...