Difference between revisions of "Atmospheric Tide"
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Latest revision as of 16:00, 30 March 2007
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Atmospheric Tide
Defined in analogy to the oceanic tide as an atmospheric motion
on a worldwide scale, in which vertical accelerations are neglected
(but compressibility is taken into account). Also called atmospheric
oscillation .
Both the sun and moon produce atmospheric tides; and there
exist both gravitational tides and thermal tides. The harmonic
component of greatest amplitude, the 12-hour or semidiurnal solar
atmospheric tide, is both gravitational and thermal in origin,
the fact that it is greater than the corresponding lunar atmospheric
tide being ascribed usually to a resonance in the atmosphere with
a free period very close to the tidal period. Other tides of 6,
8, and 24 hours have been observed.
References
This article is based on NASA's Dictionary of Technical Terms for Aerospace Use
