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Day length fluctuations

Index Day length fluctuations

The length of the day, which has increased over the long term of Earth's history due to tidal effects, is also subject to fluctuations on a shorter scale of time. [1]

19 relations: Angular momentum, Angular velocity, Atmosphere of Earth, Atomic clock, Cambridge University Press, Continental drift, Cryosphere, Earth's rotation, Ekman layer, El Niño, Friction, General circulation model, History of Earth, International Earth Rotation and Reference Systems Service, Laser rangefinder, Moment of inertia, Prevailing winds, Tidal acceleration, Trade winds.

Angular momentum

In physics, angular momentum (rarely, moment of momentum or rotational momentum) is the rotational equivalent of linear momentum.

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Angular velocity

In physics, the angular velocity of a particle is the rate at which it rotates around a chosen center point: that is, the time rate of change of its angular displacement relative to the origin.

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Atmosphere of Earth

The atmosphere of Earth is the layer of gases, commonly known as air, that surrounds the planet Earth and is retained by Earth's gravity.

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Atomic clock

An atomic clock is a clock device that uses an electron transition frequency in the microwave, optical, or ultraviolet region of the electromagnetic spectrum of atoms as a frequency standard for its timekeeping element.

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Cambridge University Press

Cambridge University Press (CUP) is the publishing business of the University of Cambridge.

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Continental drift

Continental drift is the movement of the Earth's continents relative to each other, thus appearing to "drift" across the ocean bed.

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Cryosphere

The cryosphere (from the Greek κρύος kryos, "cold", "frost" or "ice" and σφαῖρα sphaira, "globe, ball") is those portions of Earth's surface where water is in solid form, including sea ice, lake ice, river ice, snow cover, glaciers, ice caps, ice sheets, and frozen ground (which includes permafrost).

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Earth's rotation

Earth's rotation is the rotation of Planet Earth around its own axis.

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Ekman layer

The Ekman layer is the layer in a fluid where there is a force balance between pressure gradient force, Coriolis force and turbulent drag.

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El Niño

El Niño is the warm phase of the El Niño Southern Oscillation (commonly called ENSO) and is associated with a band of warm ocean water that develops in the central and east-central equatorial Pacific (between approximately the International Date Line and 120°W), including off the Pacific coast of South America.

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Friction

Friction is the force resisting the relative motion of solid surfaces, fluid layers, and material elements sliding against each other.

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General circulation model

A general circulation model (GCM) is a type of climate model.

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History of Earth

The history of Earth concerns the development of planet Earth from its formation to the present day.

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International Earth Rotation and Reference Systems Service

The International Earth Rotation and Reference Systems Service (IERS), formerly the International Earth Rotation Service, is the body responsible for maintaining global time and reference frame standards, notably through its Earth Orientation Parameter (EOP) and International Celestial Reference System (ICRS) groups.

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Laser rangefinder

A laser rangefinder is a rangefinder that uses a laser beam to determine the distance to an object.

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Moment of inertia

The moment of inertia, otherwise known as the angular mass or rotational inertia, of a rigid body is a tensor that determines the torque needed for a desired angular acceleration about a rotational axis; similar to how mass determines the force needed for a desired acceleration.

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Prevailing winds

Prevailing winds are winds that blow predominantly from a single general direction over a particular point on the Earth's surface.

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Tidal acceleration

Tidal acceleration is an effect of the tidal forces between an orbiting natural satellite (e.g. the Moon), and the primary planet that it orbits (e.g. Earth).

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Trade winds

The trade winds are the prevailing pattern of easterly surface winds found in the tropics, within the lower portion of the Earth's atmosphere, in the lower section of the troposphere near the Earth's equator.

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Redirects here:

Changes of the length of day, Fluctuations in the length of day, Fluctuations of the length of day, Length-of-day variation.

References

[1] https://en.wikipedia.org/wiki/Day_length_fluctuations

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