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
Parents
8
An Experimental Study of Temperature-Gradient Metamorphism
D. Marbouty · Journal of Glaciology · 1980 · 146 citations · Full text
An Experimental Study of Temperature-Gradient Metamorphism
D. Marbouty · Journal of Glaciology · 1980 · 114 citations
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NSF National Center for Atmospheric Research, United States
1 publications · 158 citations
1
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1
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1–5 of 16
10
Centre National de Recherches Météorologiques
Toulouse, France
2 h-index
2 publications
260 citations
Dalhousie University
Halifax, Canada
1 h-index
2 publications
98 citations

NSF National Center for Atmospheric Research
Boulder, United States
1 h-index
3 publications
474 citations

University of Canterbury
Christchurch, New Zealand
1 h-index
2 publications
32 citations

University of Applied Sciences Utrecht
Utrecht, Netherlands
1 h-index
3 publications
474 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
1 h-index
2 publications
52 citations
Utrecht University
Utrecht, The Netherlands
1 h-index
3 publications
474 citations
NOAA National Ice Center
Suitland, United States
1 h-index
1 publications
158 citations
1–8 of 10
3 publications · 276 citations
3
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1 publications · 49 citations
1
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1 publications · 42 citations
1
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1 publications · 26 citations
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Repository · 1 publications · 365 citations
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