Atmospheric cell sizes in the Solar system related to orbital and rotation frequencies of celestial bodies

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Up to now there are 7 rather well s tudied atmos pheres in the s olar s ys tem: Sun's photos phere, Venus , Earth, Mars , Jupiter, Saturn, Titan. They have differing radii, thickness, masses, densities, compositions, physical states, belong to celestial bodies of three types, but one property unites them. They are structurized by inertia-gravity waves (as well as their lithospheres) and obey one law of the wave planetology [2-8 & others]: higher orbital frequency smaller atmospheric granules and, vice versa, lower orbita l frequency larger granules . " Orbits ma ke s tructures " - this three-word sentence is an essence of the wave planetology - the only science uniting all so different heavenly bodies on a basis of their orbital properties. Always present orbital eccentricit ies and frequencies and body rotations are main reasons for their wave structurizat ion. All mentioned atmospheres demonstrate this rather clear. Arranged in a row of diminishing orbital frequencies they show increasing relative atmospheric granule sizes. The relat ion frequency - size is scaled to the photosphere: 1/1month - πR/ 60 (48) o r Ea rth: 1/1 year - πR/4 (R - a body radius).

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