Titlebook: Compendium of Meteorology; H. R. Byers,H. E. Landsberg,H. G. Houghton,Thomas Book 1951 American Meteorological Society 1951 atmospheric s

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of the Society, through the offices of the Secretary and the Executive Secretary, and by correspondence. All of the Americas are represented in the membership of the Society as well as many foreign countries.978-1-940033-70-9

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The Composition of Atmospheric Airheir absolute quantities. This applies not only to the main components, but also to rare species of polyatomic molecules whose importance in the radiation balance is often quite out of proportion to their actual quantity. Any observed variation in the composition of air—with time, with geographical

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Long-Wave Radiationetical calculations and not through measurements. These calculations are, nevertheless, based on experiments in the laboratory and in the atmosphere. The atmospheric radiation is very seldom measured from balloons [3] or from aircraft [17], but quite frequently on the ground where the radiation from

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Visibility in Meteorologyuman vision which determine how far a given object can be seen at such and such a moment. This important distance, when referred to the ordinary objects which lie around the horizon of a meteorological observer, is called by meteorologists “the visibility”; it is not with any hope of changing this t

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Universal Aspects of Atmospheric Electricitypresent universal aspects of atmospheric electricity. Of course one sees lightning and hears thunder, but these are heralds of an impetuous, stormy aspect of atmospheric electricity which is not universal. Lightning is seldom seen in the polar regions and even in temperate latitudes it is seen only

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Ions in the Atmospheree which are regarded as normal and to include in the discussions, which are of necessity brief, only those items which are most important. References to investigations have also been restricted to those regarded as most pertinent to the subject at hand.