Ridge-top Flow
Ridge-Top Flow is a meteorological phenomenon characterized by the accelerated and often turbulent airflow that occurs when wind passes over the crest of a topographic ridge, distinguished from surrounding wind patterns by its enhancement due to orographic lifting and flow compression at the summit.
51
Publications
2.7K
Citations
115
Authors
52
Institutions
Publications per year
2017–2026
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1–5 of 51
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Commonwealth Scientific and Industrial Research Organisation, Australia
3 publications · 182 citations
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Commonwealth Scientific and Industrial Research Organisation
Canberra, Australia
3 h-index
9 publications
644 citations
Met Office
Exeter, United Kingdom
2 h-index
4 publications
496 citations

University of Leeds
Leeds, United Kingdom
2 h-index
3 publications
88 citations
Marine Scotland
Edinburgh, United Kingdom
2 h-index
2 publications
102 citations
North Carolina State University
Raleigh, United States
2 h-index
5 publications
153 citations

Pacific Northwest National Laboratory
Richland, United States
2 h-index
3 publications
492 citations
Technical University of Denmark
Kongens Lyngby, Denmark
2 h-index
4 publications
221 citations
Woods Hole Oceanographic Institution
Falmouth, United States
2 h-index
2 publications
81 citations
1–8 of 52
8 publications · 380 citations
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3 publications · 55 citations
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3 publications · 86 citations
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3 publications · 138 citations
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2 publications · 310 citations
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