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  2. Coriolis force - Wikipedia

    en.wikipedia.org/wiki/Coriolis_force

    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 ...

  3. Coriolis–Stokes force - Wikipedia

    en.wikipedia.org/wiki/Coriolis–Stokes_force

    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]

  4. Coriolis effect (perception) - Wikipedia

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

    Coriolis effect (perception) In psychophysical perception, the Coriolis effect (also referred to as the Coriolis illusion or the vestibular Coriolis effect) is the misperception of body orientation due to head movement while under the effect of rotation, often inducing nausea. [1][2][3] This effect comes about as the head is moved in contrary ...

  5. Ocean gyre - Wikipedia

    en.wikipedia.org/wiki/Ocean_gyre

    In oceanography, a gyre (/ ˈdʒaɪər /) is any large system of circulating ocean surface currents, particularly those involved with large wind movements. Gyres are caused by the Coriolis effect; planetary vorticity, horizontal friction and vertical friction determine the circulatory patterns from the wind stress curl (torque).

  6. Coriolis frequency - Wikipedia

    en.wikipedia.org/wiki/Coriolis_frequency

    The Coriolis frequency ƒ, also called the Coriolis parameter or Coriolis coefficient, [1] is equal to twice the rotation rate Ω of the Earth multiplied by the sine of the latitude . The rotation rate of the Earth (Ω = 7.2921 × 10 −5 rad/s) can be calculated as 2 π / T radians per second, where T is the rotation period of the Earth which ...

  7. Rotating reference frame - Wikipedia

    en.wikipedia.org/wiki/Rotating_reference_frame

    the centrifugal force, the Coriolis force, and, for non-uniformly rotating reference frames, the Euler force. Scientists in a rotating box can measure the rotation speed and axis of rotation by measuring these fictitious forces. For example, Léon Foucault was able to show the Coriolis force that results from Earth's rotation using the Foucault ...

  8. Gaspard-Gustave de Coriolis - Wikipedia

    en.wikipedia.org/wiki/Gaspard-Gustave_de_Coriolis

    Gaspard-Gustave de Coriolis (French: [ɡaspaʁ ɡystav də kɔʁjɔlis]; 21 May 1792 – 19 September 1843) was a French mathematician, mechanical engineer and scientist. He is best known for his work on the supplementary forces that are detected in a rotating frame of reference, leading to the Coriolis effect. He was the first to apply the ...

  9. Taylor column - Wikipedia

    en.wikipedia.org/wiki/Taylor_column

    Taylor column. Motion of fluid above and below a moving object is forced to circulate, and are thus restricted to be within a column extended by the object in the axis of rotation. A Taylor column is a fluid dynamics phenomenon that occurs as a result of the Coriolis effect. It was named after Geoffrey Ingram Taylor.