Atmospheric Icing
Atmospheric Icing is a meteorological phenomenon characterized by the formation of ice on solid surfaces due to the freezing of supercooled water droplets in the atmosphere, distinguishing it from other forms of icing by its direct dependence on in-cloud or precipitation-derived liquid water interacting with sub-freezing surface temperatures.
251
Publications
12.1K
Citations
700
Authors
232
Institutions
Publications per year
2017–2026
73
251
1–5 of 251
700
13
h-index
10
h-index
9
h-index
NSF National Center for Atmospheric Research, United States
9 publications · 643 citations
9
h-index
9
h-index
1–5 of 700
232
Université du Québec à Chicoutimi
Saguenay, Canada
15 h-index
38 publications
2.1K citations

Glenn Research Center
Cleveland, United States
15 h-index
48 publications
2K citations

NSF National Center for Atmospheric Research
Boulder, United States
13 h-index
34 publications
1.9K citations
Natural Sciences and Engineering Research Council of Canada
Ottawa, Canada
10 h-index
23 publications
1.1K citations
Hydro-Québec
Montreal, Canada
10 h-index
23 publications
1.1K citations

University of Alberta
Edmonton, Canada
8 h-index
12 publications
200 citations
Environment and Climate Change Canada
Ottawa, Canada
8 h-index
17 publications
2.4K citations

Chongqing University
Chongqing, China
7 h-index
28 publications
1.3K citations
1–8 of 232
9 publications · 715 citations
9
h-index
10 publications · 561 citations
9
h-index
7 publications · 639 citations
7
h-index
JAMC · 6 publications · 250 citations
6
h-index
6 publications · 171 citations
6
h-index
1–5