Area-dosage Relationships and Time of Tracer Arrival in the Green Glow Program

Area-dosage Relationships and Time of Tracer Arrival in the Green Glow Program PDF

Author: William P. Elliott

Publisher:

Published: 1961

Total Pages: 50

ISBN-13:

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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.

Area-dosage Relationships and Time of Tracer Arrival in the Green Glow Program

Area-dosage Relationships and Time of Tracer Arrival in the Green Glow Program PDF

Author: William P. Elliott

Publisher:

Published: 1961

Total Pages: 0

ISBN-13:

DOWNLOAD EBOOK →

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.

Summary of One Year of Data from the Cape Kennedy WIND System

Summary of One Year of Data from the Cape Kennedy WIND System PDF

Author: Joan Dwyer

Publisher:

Published: 1965

Total Pages: 86

ISBN-13:

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In July of 1962, an automatic computer-controlled meteorological data acquisition and processing system became operational at Cape Kennedy, Florida. One year of data from this Weather Information Network and Display (WIND) System has been edited. Selected parameters are presented in climatological summaries in this report. (Author).