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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Moving Boundary PDE Model Implementation,d the formation of precipitation elements. A distinction must be made between condensation in the liquid phase and in the solid phase. There are also differences between the formation of solid and liquid precipitation elements. A brief discussion of the artificial dissipation of fog will also be included.

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Long-Wave Radiationuation that went beyond the formulation of empirical equations to approximate their average values. The theoretical deductions concerning the radiation in the atmosphere are much more extensive, and it would be most desirable to support them by careful measurements, especially since the experimental tools are available.

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Polarization of Skylighticity of the determination of neutral points, more attention was paid later on to their study and soon a complete picture of diurnal, seasonal, and secular variations in the position of the Arago and Babinet points was obtained.

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Precipitation Electricitycharge production and transport processes in the atmosphere. One serious difficulty in the proper evaluation of precipitation electric phenomena is that the data thus far collected have been limited to a relatively few geographical regions and with few exceptions have covered only short periods of time. Many of the data are contradictory.

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Book 1951ns, and the advancement of its professional ideals." The organization of the Society took place in affiliation with the American Association for the Advancement of Science at Saint Louis, Missouri, December 29, 1919, and its incorporation, at Washington, D. C., January 21, 1920. The work of the Soci

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SpringerBriefs in Computer Science and electromagnetic nature. In the lower layers of the atmosphere the radiation of the radioactive substances that are contained in the air and in the uppermost strata of the earth’s crust is the principal source of this ion formation.

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The Composition of Atmospheric Airlocation, with height, with the seasons, or with meteorological conditions—seriously affects our conception of the processes in the atmosphere. It follows from this that the present article must lay its emphasis on facts in order to see where our knowledge is still inadequate.

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