Geostrophic Wind
Geostrophic Wind is a theoretical wind velocity field that arises as a steady-state balance between the pressure gradient force and the Coriolis force, characterized by flow parallel to straight isobars in the absence of friction and vertical motion.
484
Publications
28.2K
Citations
942
Authors
351
Institutions
Publications per year
2017–2026
42
Parents
484
1–5 of 484
942
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NSF National Center for Atmospheric Research, United States
8 publications · 583 citations
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1–5 of 942
351

NSF National Center for Atmospheric Research
Boulder, United States
21 h-index
41 publications
4.1K citations
Royal Netherlands Meteorological Institute
De Bilt, The Netherlands
12 h-index
30 publications
2.5K citations
Met Office
Exeter, United Kingdom
12 h-index
17 publications
854 citations
University of Washington
Seattle, United States
11 h-index
21 publications
1.6K citations
Wageningen University & Research
Wageningen, The Netherlands
10 h-index
22 publications
2.1K citations
Goddard Space Flight Center
Greenbelt, United States
10 h-index
17 publications
659 citations
NOAA National Weather Service
Silver Spring, United States
9 h-index
9 publications
253 citations

Swedish Meteorological and Hydrological Institute
Norrköping, Sweden
8 h-index
15 publications
1.3K citations
1–8 of 351
64 publications · 4.3K citations
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JGR · 44 publications · 3.6K citations
27
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41 publications · 1.9K citations
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53 publications · 2.9K citations
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30 publications · 1.4K citations
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