Rime Fog
Rime Fog is a meteorological phenomenon characterized by the rapid freezing of supercooled water droplets in fog upon contact with surfaces, forming a white, granular ice deposit distinct from other forms of fog-related ice accretion.
6
Publications
286
Citations
16
Authors
9
Institutions
Publications per year
2017–2026
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Desert Research Institute
Reno, United States
2 h-index
4 publications
132 citations

Université du Québec
Québec, Canada
1 h-index
1 publications
37 citations

Czech Academy of Sciences
Prague, Czechia
1 h-index
2 publications
24 citations
Czech Academy of Sciences, Institute of Hydrology
Prague, Czechia
1 h-index
1 publications
12 citations
Czech Geological Survey
Prague, Czechia
1 h-index
1 publications
12 citations
University of Nevada, Reno
Reno, United States
1 h-index
2 publications
24 citations
Scottish Health Services
Aberdeen, United Kingdom
1 h-index
1 publications
29 citations
Czech Academy of Sciences, Institute of Atmospheric Physics
Prague, Czechia
1 h-index
1 publications
12 citations
1–8 of 9
1 publications · 142 citations
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1 publications · 54 citations
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1 publications · 29 citations
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1 publications · 12 citations
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1 publications · 12 citations
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