Mountain Wave Shear is a type of wind shear characterized by abrupt changes in wind velocity and direction caused by gravity waves generated when airflow is forced over mountainous terrain, distinguished from other forms of wind shear by its orographically induced, oscillatory nature in the lee of topographic barriers.
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2017–2026
7
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- KPKlaus P. Hoinka
Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR), Germany
2 publications · 33 citations
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- JD
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United States Naval Research Laboratory
Washington, United States
4 h-index
5 publications
339 citations
Centre National de la Recherche Scientifique
Paris, France
3 h-index
8 publications
181 citations
NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
7 publications
367 citations
University of Reading
Reading, United Kingdom
2 h-index
6 publications
122 citations
University of Lisbon
Lisbon, Portugal
2 h-index
4 publications
98 citations
Zhejiang University
Hangzhou, China
1 h-index
1 publications
12 citations
Scripps Institution of Oceanography
La Jolla, United States
1 h-index
1 publications
45 citations
LIAG Institute for Applied Geophysics
Hanover, Germany
1 h-index
1 publications
67 citations
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Venues
- Journal of the Atmospheric Sciences
8 publications · 581 citations
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- Quarterly Journal of the Royal Meteorological Society
5 publications · 148 citations
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- Monthly Weather Review
3 publications · 63 citations
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- Atmospheric Research
3 publications · 62 citations
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- Tellus A Dynamic Meteorology and Oceanography
2 publications · 33 citations
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