Pingo Formation
Pingo Formation is a geomorphological process denoting the development of conical ice-cored hills in permafrost regions, distinguished by the upward growth of a frozen core due to hydrostatic or hydraulic pressure within saturated, unconsolidated sediments.
82
Publications
3K
Citations
187
Authors
111
Institutions
Publications per year
2017–2026
16
82
1–5 of 82
187
9
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
6 publications · 188 citations
6
h-index
5
h-index
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
4 publications · 131 citations
4
h-index
3
h-index
1–5 of 187
111
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
6 h-index
23 publications
746 citations
University of Copenhagen
Copenhagen, Denmark
6 h-index
12 publications
185 citations

Hokkaido University
Sapporo, Japan
5 h-index
8 publications
281 citations

University of British Columbia
Vancouver, Canada
4 h-index
4 publications
412 citations

Lomonosov Moscow State University
Moscow, Russia
3 h-index
15 publications
1.5K citations

Aberystwyth University
Aberystwyth, United Kingdom
3 h-index
3 publications
85 citations
University of Liège
Liège, Belgium
3 h-index
3 publications
150 citations

Kazan Federal University
Kazan’, Russia
3 h-index
6 publications
218 citations
1–8 of 111
7 publications · 205 citations
7
h-index
7 publications · 105 citations
7
h-index
6 publications · 409 citations
6
h-index
4 publications · 109 citations
4
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QR · 3 publications · 57 citations
3
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1–5