atmospheric tide
Quick Summary
An atmospheric tide refers to the tidal movements within the Earth's atmosphere. These movements are similar to ocean tides but are primarily caused by daily temperature changes, rather than the gravitational pull of the Moon and Sun.1
While ocean tides are a direct result of the gravitational forces exerted by the Moon and Sun on Earth's water bodies, atmospheric tides are a less significant component of atmospheric motion. They are a detectable meteorological phenomenon, but their influence is minor compared to other atmospheric processes.23
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