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1951
This discussion will be devoted to a brief study of those interrelations between the optical properties of the atmosphere and the characteristics of human 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 ...
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This discussion will be devoted to a brief study of those interrelations between the optical properties of the atmosphere and the characteristics of human 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 ...
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Meteorology and Atmospheric Physics, 1975
The general large‐scale circulation of the global atmosphere has its basic driving mechanism in the equator‐poleward temperature gradients in both hemispheres. It has become increasingly obvious over the last few decades that to understand and predict the behavior of the atmosphere at any point, it is essential to understand the behavior of the total ...
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The general large‐scale circulation of the global atmosphere has its basic driving mechanism in the equator‐poleward temperature gradients in both hemispheres. It has become increasingly obvious over the last few decades that to understand and predict the behavior of the atmosphere at any point, it is essential to understand the behavior of the total ...
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Scientific American, 1976
The visible features of the giant planet reflect the circulation of its atmosphere. A model reproducing those features should apply to other planetary atmospheres, including the earth's.
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The visible features of the giant planet reflect the circulation of its atmosphere. A model reproducing those features should apply to other planetary atmospheres, including the earth's.
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Meteorological data and meteorological changes
Eos, Transactions American Geophysical Union, 1929This report deals with climatic changes as read from the geologic record which shows among other, things that the Earth has undergone at irregular intervals measured by thousands of years wide‐spread glaciation with its attendant lowering of temperature and the destruction of all forms of life in the regions of most intense glaciation.
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