Firn Processes

Firn Processes is the geophysical transformation sequence in which snow undergoes densification, recrystallization, and pore closure under the influence of temperature gradients, overburden pressure, and meltwater percolation, ultimately transitioning into glacial ice within the porous, intergranular medium of firn.

142

Publications

9.6K

Citations

397

Authors

184

Institutions

Publications per year

2017–2026

37

Authors

397

  1. MR
    M. R. van den Broeke

    Utrecht University, Netherlands

    14 publications · 1.7K citations

    14

    h-index

  2. RB
    Richard B. Alley

    Pennsylvania State University, United States

    12 publications · 913 citations

    12

    h-index

  3. SL
    Stefan Ligtenberg

    Utrecht University, Netherlands

    10 publications · 1.3K citations

    10

    h-index

  4. CM
    C. Max Stevens

    University of Washington, United States

    9 publications · 603 citations

    9

    h-index

  5. PK
    Peter Kuipers Munneke

    Utrecht University, Netherlands

    8 publications · 712 citations

    8

    h-index

1–5 of 397

Venues

  1. Journal of Glaciology

    28 publications · 1.9K citations

    22

    h-index

  2. ˜The œcryosphere

    18 publications · 1.3K citations

    17

    h-index

  3. Annals of Glaciology

    17 publications · 805 citations

    15

    h-index

  4. Geophysical Research Letters

    11 publications · 774 citations

    11

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 960 citations

    7

    h-index

1–5