Occluded Fronts
An Occluded Front is a synoptic-scale front, formed during the advanced stage of cyclone evolution, wherein a cold front overtakes a warm front, resulting in the lifting of the warm air mass aloft and the merging of the two frontal boundaries into a single complex front characterized by a combination of cold and warm front properties.
21
Publications
835
Citations
56
Authors
38
Institutions
Publications per year
2017–2026
1
21
1–5 of 21
56
4
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38
University of Washington
Seattle, United States
6 h-index
12 publications
457 citations

University of Helsinki
Helsinki, Finland
3 h-index
4 publications
119 citations
Met Office
Exeter, United Kingdom
2 h-index
4 publications
84 citations

NSF National Center for Atmospheric Research
Boulder, United States
2 h-index
4 publications
206 citations
University of Miami
Coral Gables, United States
1 h-index
1 publications
10 citations
Manash Kozybayev North Kazakhstan University
Petropavl, Kazakhstan
1 h-index
1 publications
26 citations

St Petersburg University
Saint Petersburg, Russia
1 h-index
1 publications
26 citations
National Research Nuclear University MEPhI
Moscow, Russia
1 h-index
2 publications
52 citations
1–8 of 38
7 publications · 500 citations
7
h-index
JAMC · 2 publications · 41 citations
2
h-index
BAMS · 2 publications · 104 citations
2
h-index
1 publications · 12 citations
1
h-index
1 publications · 16 citations
1
h-index
1–5