Firn Formation

Firn Formation is a geophysical process denoting the transitional stage in snowpack metamorphism wherein snow densifies into granular ice through prolonged compaction and recrystallization under overburden pressure, distinguishing it from both seasonal snow and glacial ice by its intermediate density and grain structure.

27

Publications

1.1K

Citations

64

Authors

44

Institutions

Publications per year

2017–2026

3

Authors

64

  1. RB
    Richard B. Alley

    Pennsylvania State University, United States

    5 publications · 272 citations

    5

    h-index

  2. DW
    D.S. Wilkinson

    McMaster University, Canada

    2 publications · 72 citations

    2

    h-index

  3. CC
    Chester C. Langway

    University at Buffalo, State University of New York, United States

    2 publications · 65 citations

    2

    h-index

  4. WA
    W. Ambach

    Universität Innsbruck, Austria

    2 publications · 30 citations

    2

    h-index

  5. KK
    Katsuhisa Kawashima

    Railway Technical Research Institute, Japan

    2 publications · 39 citations

    2

    h-index

1–5 of 64

Venues

  1. Journal of Glaciology

    11 publications · 513 citations

    11

    h-index

  2. Annals of Glaciology

    4 publications · 67 citations

    4

    h-index

  3. Quaternary Science Reviews

    2 publications · 83 citations

    2

    h-index

  4. Tellus B

    2 publications · 187 citations

    2

    h-index

  5. Geophysical Research Letters

    1 publications · 29 citations

    1

    h-index

1–5