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  2. Coriolis force - Wikipedia

    en.wikipedia.org/wiki/Coriolis_force

    The practical impact of the "Coriolis effect" is mostly caused by the horizontal acceleration component produced by horizontal motion. There are other components of the Coriolis effect. Westward-traveling objects are deflected downwards, while eastward-traveling objects are deflected upwards. [44] This is known as the Eötvös effect. This ...

  3. Coriolis field - Wikipedia

    en.wikipedia.org/wiki/Coriolis_field

    Support for the idea that the Coriolis field is a real physical effect and not just a mathematical artifact is justified by Machian theory. It notes that evidence of the field's existence is not only visible to the rotating observer; its distortion is also visible and verifiable for non-rotating onlookers.

  4. 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.

  5. Ocean gyre - Wikipedia

    en.wikipedia.org/wiki/Ocean_gyre

    Gyres are caused by the Coriolis effect; planetary vorticity, horizontal friction and vertical friction determine the circulatory patterns from the wind stress curl . [ 1 ] Gyre can refer to any type of vortex in an atmosphere or a sea , [ 2 ] even one that is human-created, but it is most commonly used in terrestrial oceanography to refer to ...

  6. Wind - Wikipedia

    en.wikipedia.org/wiki/Wind

    The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics and subtropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations.

  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. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The descended air then travels toward the equator along the surface, replacing the air that rose from the equatorial zone, closing the loop of the Hadley cell. [3] The poleward movement of the air in the upper part of the troposphere deviates toward the east, caused by the coriolis acceleration. At the ground level, however, the movement of the ...

  9. Westerlies - Wikipedia

    en.wikipedia.org/wiki/Westerlies

    If the Earth were tidally locked to the Sun, solar heating would cause winds across the mid-latitudes to blow in a poleward direction, away from the subtropical ridge. . However, the Coriolis effect caused by the rotation of Earth tends to deflect poleward winds eastward from north (to the right) in the Northern Hemisphere and eastward from south (to the left) in the Southern Hemisph