Ice-Wedge Polygons is a periglacial landform characterized by a polygonal pattern of ground cracks filled with ice, formed through thermal contraction processes in permafrost regions, distinguished by the systematic development of ice wedges that delineate the polygonal network.
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2017–2026
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142
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186
University of Alaska Fairbanks
Fairbanks, United States
18 h-index
51 publications
2.7K citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
14 h-index
55 publications
2.9K citations
Los Alamos National Laboratory
Los Alamos, United States
11 h-index
35 publications
2.6K citations
Oak Ridge National Laboratory
Oak Ridge, United States
11 h-index
32 publications
1.6K citations
Carleton University
Ottawa, Canada
9 h-index
15 publications
650 citations
Université Laval
Québec, Canada
8 h-index
22 publications
1.1K citations
University of Connecticut
Storrs, United States
8 h-index
14 publications
968 citations
Woodwell Climate Research Center
Falmouth, United States
7 h-index
11 publications
412 citations
1–8 of 186
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- Permafrost and Periglacial Processes
20 publications · 872 citations
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- Geografiska Annaler Series A Physical Geography
8 publications · 196 citations
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- Remote Sensing
8 publications · 447 citations
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- The cryosphere
7 publications · 333 citations
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- Canadian Journal of Earth Sciences
7 publications · 625 citations
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