Ekman Balance is a dynamical equilibrium in geophysical fluid dynamics, within the broader context of geostrophic balance, that describes the balance between the viscous frictional forces, the Coriolis force, and the horizontal pressure gradient in the planetary boundary layer, specifically accounting for turbulent drag effects in the Ekman layer.
28
Publications
1.4K
Citations
64
Authors
38
Institutions
Publications per year
2017–2026
5
Parents
Publications
28
1–5 of 28
Authors
64
- TK
3
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- RK
2
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- HL
2
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- AP
2
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- SC
2
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1–5 of 64
Institutions
38
Scripps Institution of Oceanography
La Jolla, United States
6 h-index
7 publications
479 citations
University of California San Diego
San Diego, United States
5 h-index
5 publications
383 citations
Woods Hole Oceanographic Institution
Falmouth, United States
4 h-index
6 publications
377 citations
Naval Postgraduate School
Monterey, United States
3 h-index
3 publications
191 citations
Ludwig-Maximilians-Universität München
Munich, Germany
2 h-index
4 publications
92 citations
National Taiwan University
Taipei, Taiwan
2 h-index
3 publications
65 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
2 h-index
4 publications
96 citations
Oregon State University
Corvallis, United States
2 h-index
9 publications
558 citations
1–8 of 38
Venues
- Journal of Physical Oceanography
7 publications · 491 citations
7
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- Journal of Geophysical Research Atmospheres
JGR · 5 publications · 398 citations
5
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- Journal of the Atmospheric Sciences
4 publications · 131 citations
4
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- Quarterly Journal of the Royal Meteorological Society
3 publications · 151 citations
3
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- Geophysical Research Letters
2 publications · 76 citations
2
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1–5