Weak Layer Metamorphism

Weak Layer Metamorphism is a physicochemical process in snowpack evolution that belongs to the category of snow metamorphism phenomena, distinguished by the preferential structural and textural transformation of ice grains within a thin, low-density, and poorly bonded stratum, leading to the formation or enhancement of a persistent weak layer prone to failure under applied loads.

10

Publications

545

Citations

13

Authors

13

Institutions

Publications per year

2017–2026

1

Authors

13

  1. CF
    Charles Fierz

    Swiss Federal Institute for Forest, Snow and Landscape Research, Switzerland

    2 publications · 54 citations

    2

    h-index

  2. DM
    D. M. McClung

    University of British Columbia, Canada

    2 publications · 54 citations

    2

    h-index

  3. JS
    Jürg Schweizer

    Swiss Federal Institute for Forest, Snow and Landscape Research, Switzerland

    2 publications · 51 citations

    2

    h-index

  4. MS
    Matthew Sturm

    Cold Regions Research and Engineering Laboratory, United States

    2 publications · 318 citations

    2

    h-index

  5. CS
    Carl S. Benson

    University of Alaska Fairbanks, United States

    2 publications · 318 citations

    2

    h-index

1–5 of 13

Venues

  1. Journal of Glaciology

    2 publications · 318 citations

    2

    h-index

  2. Annals of Glaciology

    2 publications · 54 citations

    2

    h-index

  3. Icarus

    1 publications · 11 citations

    1

    h-index

  4. Contributions to Mineralogy and Petrology

    1 publications · 60 citations

    1

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 1 publications · 40 citations

    1

    h-index

1–5