Destructive Metamorphism

Destructive Metamorphism is a sub-process within snow metamorphism characterized by the breakdown and rounding of ice crystal edges and bonds due to temperature gradient-driven vapor transport, distinguishing it from constructive metamorphism by its dominance in rapidly equilibrating snowpacks under strong thermal gradients.

8

Publications

916

Citations

16

Authors

10

Institutions

Publications per year

2017–2026

2

Variants

Equitemperature Metamorphism

Authors

16

  1. DM
    D. Marbouty

    Centre National de Recherches Météorologiques, France

    2 publications · 260 citations

    2

    h-index

  2. JA
    John Abrahamson

    University of Canterbury, New Zealand

    1 publications · 16 citations

    1

    h-index

  3. JT
    Jan T. M. Lenaerts

    Utrecht University, Netherlands

    1 publications · 158 citations

    1

    h-index

  4. WJ
    William J. Sacks

    NSF National Center for Atmospheric Research, United States

    1 publications · 158 citations

    1

    h-index

  5. AG
    A. G. Slater

    University of Colorado Boulder, United States

    1 publications · 158 citations

    1

    h-index

1–5 of 16

Venues

  1. Journal of Glaciology

    3 publications · 276 citations

    3

    h-index

  2. 1

    h-index

  3. Water Resources Research

    1 publications · 42 citations

    1

    h-index

  4. ˜The œcryosphere

    1 publications · 26 citations

    1

    h-index

  5. 1

    h-index

1–5