Permafrost Soils

Permafrost Soils is a type of mountain soil characterized by the presence of perennially frozen ground that remains at or below 0°C for at least two consecutive years, distinguishing it from other mountain soils by its persistent cryotic conditions and associated cryogenic processes.

973

Publications

58.5K

Citations

2.7K

Authors

824

Institutions

Publications per year

2017–2026

386

Authors

2.7K

  1. XW
    Xiaodong Wu

    Northwest Institute of Eco-Environment and Resources, China

    40 publications · 1.7K citations

    25

    h-index

  2. LZ
    Lin Zhao

    Chinese Academy of Sciences, China

    38 publications · 2K citations

    24

    h-index

  3. GH
    Gustaf Hugelius

    Stockholm University, Sweden

    26 publications · 5K citations

    24

    h-index

  4. YL
    Yuanming Lai

    Chinese Academy of Sciences, China

    29 publications · 1.7K citations

    23

    h-index

  5. QW
    Qingbai Wu

    Chinese Academy of Sciences, China

    28 publications · 1.4K citations

    21

    h-index

1–5 of 2.7K

Venues

  1. Cold Regions Science and Technology

    81 publications · 3.5K citations

    38

    h-index

  2. Permafrost and Periglacial Processes

    43 publications · 1.8K citations

    26

    h-index

  3. Geoderma

    29 publications · 1.4K citations

    23

    h-index

  4. CATENA

    30 publications · 1.1K citations

    21

    h-index

  5. Biogeosciences

    21 publications · 3.6K citations

    20

    h-index

1–5