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  2. 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 ...

  3. 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.

  4. Coriolis frequency - Wikipedia

    en.wikipedia.org/wiki/Coriolis_frequency

    Thus the Coriolis parameter, , is the angular velocity or frequency required to maintain a body at a fixed circle of latitude or zonal region. If the Coriolis parameter is large, the effect of the Earth's rotation on the body is significant since it will need a larger angular frequency to stay in equilibrium with the Coriolis forces.

  5. Geostrophic current - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_current

    A geostrophic current is an oceanic current in which the pressure gradient force is balanced by the Coriolis effect. The direction of geostrophic flow is parallel to the isobars, 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.

  6. Polar easterlies - Wikipedia

    en.wikipedia.org/wiki/Polar_easterlies

    Cold air subsides at the poles creating high pressure zones, forcing an equatorward outflow of air; that outflow is then deflected westward by the Coriolis effect. Unlike the westerlies in the middle latitudes and trade winds in tropics, the polar easterlies are often weak and irregular. Note, winds are named based on where they came from.

  7. Coriolis force - en.wikipedia.org

    en.wikipedia.org/.../page/mobile-html/Coriolis_force

    Deflection of an object due to the Coriolis force is called the Coriolis effect. Though recognized previously by others, the mathematical expression for the Coriolis force appeared in an 1835 paper by French scientist Gaspard-Gustave de Coriolis , in connection with the theory of water wheels .

  8. Coriolis effect (perception) - Wikipedia

    en.wikipedia.org/wiki/Coriolis_effect_(perception)

    There is also the pseudo-Coriolis effect (also referred to as the optokinetic pseudo-Coriolis effect), which takes place when there is no physical circular movement, only visual. [ 8 ] [ 9 ] Perceptually it feels the same as the Coriolis effect, being perceived as self motion inducing the same kind of nausea and often the cause of motion sickness.

  9. 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 .

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