Firn Layering

Firn Layering is a stratigraphic structure formed within the porous, intermediate stage of snow metamorphism and densification into glacial ice, distinguished by the vertical differentiation of snow and ice layers based on variations in grain size, density, and age resulting from seasonal accumulation and metamorphic processes.

35

Publications

1.5K

Citations

147

Authors

72

Institutions

Publications per year

2017–2026

6

Authors

147

  1. MR
    M. R. Albert

    Cold Regions Research and Engineering Laboratory, United States

    6 publications · 293 citations

    6

    h-index

  2. MR
    M. R. van den Broeke

    Utrecht University, Netherlands

    5 publications · 150 citations

    5

    h-index

  3. UT
    Ulrich Trefzer

    Institute of Bioinformatics and Systems Biology, Germany

    3 publications · 81 citations

    3

    h-index

  4. JR
    Joseph R. McConnell

    Desert Research Institute, United States

    3 publications · 104 citations

    3

    h-index

  5. SK
    Sepp Kipfstuhl

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

    3 publications · 282 citations

    3

    h-index

1–5 of 147

Venues

  1. Journal of Glaciology

    10 publications · 505 citations

    10

    h-index

  2. Annals of Glaciology

    9 publications · 276 citations

    9

    h-index

  3. Journal of Geophysical Research Earth Surface

    3 publications · 131 citations

    3

    h-index

  4. ˜The œcryosphere

    3 publications · 115 citations

    3

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 1 publications · 88 citations

    1

    h-index

1–5