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  2. Earth's rotation - Wikipedia

    en.wikipedia.org/wiki/Earth's_rotation

    The tangential speed of Earth's rotation at a point on Earth can be approximated by multiplying the speed at the equator by the cosine of the latitude. [42] For example, the Kennedy Space Center is located at latitude 28.59° N, which yields a speed of: cos(28.59°) × 1,674.4 km/h = 1,470.2 km/h.

  3. Coriolis frequency - Wikipedia

    en.wikipedia.org/wiki/Coriolis_frequency

    The rotation rate of the Earth (Ω = 7.2921 × 10 −5 rad/s) can be calculated as 2π / T radians per second, where T is the rotation period of the Earth which is one sidereal day (23 h 56 min 4.1 s). [2] In the midlatitudes, the typical value for is about 10 −4 rad/s.

  4. Earth orientation parameters - Wikipedia

    en.wikipedia.org/wiki/Earth_Orientation_Parameters

    Universal time tracks the Earth's rotation in time, which performs one revolution in about 24 hours. The Earth's rotation is uneven, so UT is not linear with respect to atomic time. It is practically proportional to the sidereal time, which is also a direct measure of Earth rotation. The excess revolution time is called length of day (LOD).

  5. Celestial navigation - Wikipedia

    en.wikipedia.org/wiki/Celestial_navigation

    When time at the prime meridian (or another starting point) is accurately known, celestial navigation can determine longitude, and the more accurately latitude and time are known, the more accurate the longitude determination. The angular speed of the Earth is latitude-dependent. At the poles, or latitude 90°, the rotation velocity of the ...

  6. Polar ice is melting and changing Earth’s rotation. It’s ...

    www.aol.com/polar-ice-melting-changing-earth...

    Very little is known about what’s going on roughly 1,800 miles below the Earth’s surface, and it’s not clear why the core’s speed is changing. “It’s fundamentally unpredictable ...

  7. Geosynchronous orbit - Wikipedia

    en.wikipedia.org/wiki/Geosynchronous_orbit

    A geosynchronous orbit (sometimes abbreviated GSO) is an Earth-centered orbit with an orbital period that matches Earth's rotation on its axis, 23 hours, 56 minutes, and 4 seconds (one sidereal day). The synchronization of rotation and orbital period means that, for an observer on Earth's surface, an object in geosynchronous orbit returns to ...

  8. Melting ice is slowing Earth's rotation, shifting its axis ...

    www.aol.com/news/melting-ice-slowing-earths-spin...

    Meanwhile, the slow rebound of the Earth’s crust in some high-latitude regions after the removal of Ice Age glaciers works in the opposite direction, speeding up the planet’s spin.

  9. Earth Is Spinning Faster Than Usual, Giving Us the Shortest ...

    www.aol.com/earth-spinning-faster-usual-giving...

    This minuscule change in time means we might need to consider a negative leap second. Earth Is Spinning Faster Than Usual, Giving Us the Shortest Day EVER Recorded Skip to main content