Frozen Ground Temperature

Frozen Ground Temperature is a thermal state variable that denotes the temperature condition of soil or rock maintaining a phase of water in solid form below 0°C, distinguishing it from unfrozen ground by the presence of ice as a defining constituent.

180

Publications

8.3K

Citations

514

Authors

223

Institutions

Publications per year

2017–2026

62

Authors

514

  1. VE
    V. E. Romanovsky

    University of Alaska Fairbanks, United States

    5 publications · 524 citations

    5

    h-index

  2. AP
    Agus P. Sasmito

    McGill University, Canada

    5 publications · 258 citations

    5

    h-index

  3. AR
    Ahmed Rouabhi

    École Nationale Supérieure des Mines de Paris, France

    5 publications · 436 citations

    5

    h-index

  4. MA
    Mahmoud A. Alzoubi

    McGill University, Canada

    5 publications · 258 citations

    5

    h-index

  5. SL
    Sharon L. Smith

    Geological Survey of Canada, Canada

    4 publications · 256 citations

    4

    h-index

1–5 of 514

Venues

  1. Cold Regions Science and Technology

    16 publications · 635 citations

    15

    h-index

  2. Permafrost and Periglacial Processes

    16 publications · 932 citations

    14

    h-index

  3. ˜The œcryosphere

    4 publications · 180 citations

    4

    h-index

  4. Engineering Geology

    4 publications · 159 citations

    4

    h-index

  5. Computers and Geotechnics

    4 publications · 383 citations

    4

    h-index

1–5