Permafrost Thaw

Permafrost Thaw is a cryospheric process in which perennially frozen ground (permafrost) warms to the melting point and undergoes a phase change from ice-rich frozen conditions to seasonally or permanently unfrozen soil, sediment, or rock, thereby altering ground thermal, hydrological, and mechanical properties.

1.6K

Publications

123.6K

Citations

4.1K

Authors

1.2K

Institutions

Publications per year

2017–2026

669

Authors

4.1K

  1. VE
    V. E. Romanovsky

    University of Alaska Fairbanks, United States

    49 publications · 11.3K citations

    38

    h-index

  2. GG
    Guido Grosse

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

    55 publications · 9K citations

    37

    h-index

  3. EA
    Edward A. G. Schuur

    University of Florida, United States

    39 publications · 11.3K citations

    33

    h-index

  4. SV
    Steven V. Kokelj

    Government of Northwest Territories, Canada

    33 publications · 3.3K citations

    28

    h-index

  5. JB
    Julia Boike

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

    32 publications · 5.4K citations

    24

    h-index

1–5 of 4.1K

Venues

  1. Permafrost and Periglacial Processes

    131 publications · 9.4K citations

    55

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 57 publications · 8.8K citations

    49

    h-index

  3. Geophysical Research Letters

    63 publications · 8.1K citations

    46

    h-index

  4. Environmental Research Letters

    ERL · 55 publications · 4.4K citations

    40

    h-index

  5. ˜The œcryosphere

    52 publications · 2.9K citations

    33

    h-index

1–5