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General circulation of the atmosphere

General circulation of the atmosphere.jpg Universal anemographThumbnailsDiagram of Curtiss hydro-aëroplaneUniversal anemographThumbnailsDiagram of Curtiss hydro-aëroplaneUniversal anemographThumbnailsDiagram of Curtiss hydro-aëroplaneUniversal anemographThumbnailsDiagram of Curtiss hydro-aëroplaneUniversal anemographThumbnailsDiagram of Curtiss hydro-aëroplane
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“In the accompanying figure the solid arrows in the interior part represent the resultant motions of the winds (longer arrows indicating greater velocities), in case of an earth with a homogeneous surface over both hemispheres, in which the motions would be symmetrical in both and the same at all longitudes, and the equatorial and tropical calm belts would be situated at equal distances from each pole. The dotted arrows indicate the strong, almost eastern motion of the air at all latitudes at some high altitude, as that of the cirrus clouds.

Author
Aërial Navigation
A Popular Treatise on the Growth of Air Craft and on Aëronautical Meteorology
By Albert Francis Zahm
Published in 1911
Available from gutenberg.org
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