Author: Murray Gutnick
Publisher:
ISBN:
Category : Precipitable water
Languages : en
Pages : 48

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Author:
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 310

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Author: John N. Howard
Publisher:
ISBN:
Category : Infrared radiation
Languages : en
Pages : 134

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Author: Norman Sissenwine
Publisher:
ISBN:
Category : Ballistic missiles
Languages : en
Pages : 256

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Author: Russell G. Walker
Publisher:
ISBN:
Category : Bolometer
Languages : en
Pages : 106

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Book Description
A short review is given of the literature pertinent to the bolometric correction. A recommended scale of bolometric corrections is presented based upon recent model atmospheres for stars of early spectral type, and upon stellar energy distributions synthesized from photoelectric observations of stars later than FO V. The reduction of various photoelectrically determined magnitude and color systems to a common system and the further reduction of these measurements to absolute energy units is discussed in some detail. (Author).

Author: Air Force Cambridge Research Laboratories (U.S.). Geophysics Research Directorate
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 128

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Author: Allen E. Cole
Publisher:
ISBN:
Category : Atmosphere
Languages : en
Pages : 52

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Author: Allen E. Cole
Publisher:
ISBN:
Category : Atmospheric density
Languages : en
Pages : 132

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Author: William P. Elliott
Publisher:
ISBN:
Category : Geomorphological tracers
Languages : en
Pages : 50

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Book Description
An empirical relationship between the area in which a given dosage is equalled or exceeded and the value of the dosage itself are developed using Green Glow data. It is found that the logarithm of the area is nearly a linear function of the logarithm of the dosage divided by the source strength and multiplied by a representative wind speed. These results differ only slightly from similar results obtained from Prairie Grass data. Observations of the time of first arrival of the tracer near ground level at distances of 8 and 16 miles from the source indicate that the tracer material which first arrives has travelled with a wind speed greater than the surface wind (about 15 ft). It would be necessary to have wind speed measurements between 50 and 100 ft above ground in order to estimate the time of first arrival at these distances even though the source is no higher than 15 ft.

Author: Murray Gutnick
Publisher:
ISBN:
Category : Hygrometry
Languages : en
Pages : 56

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