Flow Over Ridges is a meteorological phenomenon characterized by the deformation and acceleration of wind flow as it ascends and descends topographic ridges, distinguished from other terrain-induced flows by the generation of lee waves, rotors, and downslope winds specific to two-dimensional orographic obstacles.
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Longitudinal ridges in mass movement deposits
Anja Dufresne, Timothy R. H. Davies · Geomorphology · 2008 · 189 citations
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Met Office
Exeter, United Kingdom
10 h-index
24 publications
1.1K citations
University of Leeds
Leeds, United Kingdom
5 h-index
7 publications
157 citations
University of Washington
Seattle, United States
4 h-index
8 publications
340 citations
The University of Tokyo
Tokyo, Japan
3 h-index
4 publications
201 citations
United States Naval Research Laboratory
Washington, United States
3 h-index
6 publications
96 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
3 h-index
3 publications
68 citations
Bjerknes Centre for Climate Research
Bergen, Norway
3 h-index
3 publications
204 citations
Imperial College London
London, United Kingdom
2 h-index
3 publications
143 citations
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Venues
- Quarterly Journal of the Royal Meteorological Society
19 publications · 955 citations
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- Journal of the Atmospheric Sciences
16 publications · 462 citations
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- Journal of Physical Oceanography
5 publications · 174 citations
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- Boundary-Layer Meteorology
5 publications · 296 citations
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 239 citations
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