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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... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, CALM Adventdalen, S...
Polygonal systems formed by thermal contraction cracking are complex landscape features widespread in terrestrial periglacial regions. The manner in which cracking occurs is... -
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... -
Mapped polygon pattern geomorphometry from HRSC-AX, 2009, AD4 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 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... -
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 polygon pattern geomorphometry from HRSC-AX, 2009, HCP 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 polygon pattern geomorphometry from HRSC-AX, 2009, AD2 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 polygon pattern geomorphometry from HRSC-AX, 2009, Isdammen Adventdale...
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, 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 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... -
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...