Coriolis Parameter
The Coriolis Parameter is a scalar quantity in geophysical fluid dynamics defined as twice the angular velocity of planetary rotation projected onto the local vertical direction, serving as a coefficient that quantifies the magnitude of the Coriolis effect at a given latitude.
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ON THE WIND-DRIVEN OCEAN CIRCULATION
Walter Munk · Journal of Meteorology · 1950 · 944 citations · Full text
Coriolis effects in the yrast states
F.S. Stephens, R. S. Simon · Nuclear Physics A · 1972 · 544 citations
Coriolis effects and rotation alignment in nuclei
F. S. Stephens · Reviews of Modern Physics · 1975 · 460 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
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47 publications
3.1K citations
Massachusetts Institute of Technology
Cambridge, United States
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27 publications
1.9K citations

Centre National de la Recherche Scientifique
Paris, France
15 h-index
30 publications
1.2K citations
University of Cambridge
Cambridge, United Kingdom
11 h-index
19 publications
615 citations
University of Miami
Coral Gables, United States
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17 publications
518 citations
University of Washington
Seattle, United States
10 h-index
16 publications
798 citations
University of Reading
Reading, United Kingdom
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19 publications
1.7K citations
The University of Tokyo
Tokyo, Japan
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15 publications
356 citations
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JGR · 33 publications · 1.9K citations
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