Permafrost

Permafrost is a cryospheric ground condition in which subsurface earth materials (soil, sediment, or rock, with included ice and organic matter) remain at or below 0 °C for at least two consecutive years.

3.9K

Publications

274.9K

Citations

7.8K

Authors

1.8K

Institutions

Publications per year

2017–2026

1.4K

Authors

7.8K

  1. VE
    V. E. Romanovsky

    University of Alaska Fairbanks, United States

    88 publications · 17.5K citations

    59

    h-index

  2. GG
    Guido Grosse

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    77 publications · 12K citations

    47

    h-index

  3. QW
    Qingbai Wu

    Chinese Academy of Sciences, China

    88 publications · 7K citations

    45

    h-index

  4. EA
    Edward A. G. Schuur

    University of Florida, United States

    53 publications · 19.7K citations

    44

    h-index

  5. BE
    Bernd Etzelmüller

    University of Oslo, Norway

    52 publications · 6.8K citations

    43

    h-index

1–5 of 7.8K

Venues

  1. Permafrost and Periglacial Processes

    380 publications · 30.8K citations

    93

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 94 publications · 13.2K citations

    62

    h-index

  3. Geophysical Research Letters

    104 publications · 13.5K citations

    61

    h-index

  4. ˜The œcryosphere

    119 publications · 9.4K citations

    55

    h-index

  5. Cold Regions Science and Technology

    194 publications · 9K citations

    54

    h-index

1–5