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  2. Coriolis frequency - Wikipedia

    en.wikipedia.org/wiki/Coriolis_frequency

    Alternatively, if the Coriolis parameter is small, the effect of the Earth's rotation is small since only a small fraction of the centripetal force on the body is canceled by the Coriolis force. Thus the magnitude of f {\displaystyle f} strongly affects the relevant dynamics contributing to the body's motion.

  3. Geostrophic current - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_current

    The Coriolis force acts at right angles to the flow, and when it balances the pressure gradient force, the resulting flow is known as geostrophic. As stated above, the direction of flow is with the high pressure to the right of the flow in the Northern Hemisphere , and the high pressure to the left in the Southern Hemisphere .

  4. Coriolis force - Wikipedia

    en.wikipedia.org/wiki/Coriolis_force

    The definition of the Coriolis effect from the Glossary of Meteorology; The Coriolis Effect — a conflict between common sense and mathematics PDF-file. 20 pages. A general discussion by Anders Persson of various aspects of the coriolis effect, including Foucault's Pendulum and Taylor columns. The coriolis effect in meteorology PDF-file. 5 ...

  5. Coriolis–Stokes force - Wikipedia

    en.wikipedia.org/wiki/Coriolis–Stokes_force

    In fluid dynamics, the Coriolis–Stokes force is a forcing of the mean flow in a rotating fluid due to interaction of the Coriolis effect and wave-induced Stokes drift. This force acts on water independently of the wind stress. [1] This force is named after Gaspard-Gustave Coriolis and George Gabriel Stokes, two

  6. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    It descends, creating a cold, dry high-pressure area. At the polar surface level, the mass of air is driven away from the pole toward the 60th parallel, replacing the air that rose there, and the polar circulation cell is complete. As the air at the surface moves toward the equator, it deviates westwards, again as a result of the Coriolis ...

  7. Fictitious force - Wikipedia

    en.wikipedia.org/wiki/Fictitious_force

    An example of a pseudo force as defined by Iro is the Coriolis force, maybe better to be called: the Coriolis effect. [ 4 ] [ 5 ] [ 6 ] The gravitational force would also be a fictitious force (pseudo force) in a field model in which particles distort spacetime due to their mass, such as in the theory of general relativity .

  8. Coriolis force - en.wikipedia.org

    en.wikipedia.org/api/rest_v1/page/mobile-html/...

    In physics, the Coriolis force is an inertial (or fictitious) force that acts on objects in motion within a frame of reference that rotates with respect to an inertial frame. In a reference frame with clockwise rotation, the force acts to the left of the motion of the object. In one with anticlockwise (or counterclockwise) rotation, the force ...

  9. Taylor column - Wikipedia

    en.wikipedia.org/wiki/Taylor_column

    A Taylor column is a fluid dynamics phenomenon that occurs as a result of the Coriolis effect. It was named after Geoffrey Ingram Taylor. Rotating fluids that are perturbed by a solid body tend to form columns parallel to the axis of rotation called Taylor columns.