atmospheric tide oor Noorse Bokmål

atmospheric tide

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en
Pressure waves in the atmosphere similar to the tides of the ocean, produced by the gravitational influence of the moon and by thermal expansion and contraction.

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Atmosfærisk tidevann

en
global-scale periodic oscillations of the atmosphere, analogous to ocean tides
nb
periodiske svingninger i atmosfæren på global skala
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Atmospheric tides can be measured as regular fluctuations in wind, temperature, density and pressure.
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Atmospheric tides propagate in an atmosphere where density varies significantly with height.
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Therefore, understanding the atmospheric tides is essential in understanding the atmosphere as a whole.
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Atmospheric tides are also produced through the gravitational effects of the Moon.
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Atmospheric tides are global-scale periodic oscillations of the atmosphere.
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Atmospheric tides dominate the dynamics of the mesosphere and lower thermosphere, essential to understanding the atmosphere as a whole.
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Modeling and observations of atmospheric tides are needed in order to monitor and predict changes in the Earth's atmosphere.
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At ground level, atmospheric tides can be detected as regular but small oscillations in surface pressure with periods of 24 and 12 hours.
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Atmospheric waves with periods which are harmonics of 1 solar day (e.g. 24 hours, 12 hours, 8 hours... etc.) are known as atmospheric tides.
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The largest-amplitude atmospheric tides are mostly generated in the troposphere and stratosphere when the atmosphere is periodically heated as water vapour and ozone absorb solar radiation during the day.
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In the mesosphere (heights of ~ 50 – 100 km) atmospheric tides can reach amplitudes of more than 50 m/s and are often the most significant part of the motion of the atmosphere.
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The rotation period of Venus may represent an equilibrium state between tidal locking to the Sun's gravitation, which tends to slow rotation, and an atmospheric tide created by solar heating of the thick Venusian atmosphere.
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Although atmospheric tides share much in common with ocean tides they have two key distinguishing features: i) Atmospheric tides are primarily excited by the Sun's heating of the atmosphere whereas ocean tides are primarily excited by the Moon's gravitational field.
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This means that most atmospheric tides have periods of oscillation related to the 24-hour length of the solar day whereas ocean tides have periods of oscillation related both to the solar day as well as to the longer lunar day (time between successive lunar transits) of about 24 hours 51 minutes.
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The solution represents atmospheric waves and tides.
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God established the laws that guide the heavenly bodies, which influence earth’s weather, tides, atmosphere, and the very existence of life on this planet.
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Man knows that the heavenly bodies exercise a controlling influence over our weather, tides and atmosphere, yet how utterly impotent he is in exercising any command!
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The primary source for the 24-hr tide is in the lower atmosphere where surface effects are important.
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Although atmospheric tides share much in common with ocean tides they have two key distinguishing features:
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Although atmospheric tides share much in common with ocean tides they have two key distinguishing features:
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Therefore, learning about atmospheric tides is essential in understanding the atmosphere as a whole.
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6 Effects of atmospheric tide
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ii) Atmospheric tides propagate in an atmosphere where density varies significantly with height.
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atmospheric tides are eigenmodes of the atmosphere described by Hough functions
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Atmospheric tides dominate the dynamics of the mesosphere and lower thermosphere, essential to understanding the atmosphere as a whole.
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