Evaluation of Satellite Observing Network for Project "Space Track"

Evaluation of Satellite Observing Network for Project Author: G. R. Miczaika
Publisher:
ISBN:
Category : Artificial satellites
Languages : en
Pages : 42

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Evaluation of Satellite Observing Network for Project "Space Track"

Evaluation of Satellite Observing Network for Project Author: G. R. Miczaika
Publisher:
ISBN:
Category : Artificial satellites
Languages : en
Pages : 42

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An Estimate of Precipitable Water Along High-altitude Ray Paths

An Estimate of Precipitable Water Along High-altitude Ray Paths PDF Author: Murray Gutnick
Publisher:
ISBN:
Category : Precipitable water
Languages : en
Pages : 48

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Air Force Surveys in Geophysics

Air Force Surveys in Geophysics PDF Author:
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 158

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An Investigation of a Perennially Frozen Lake

An Investigation of a Perennially Frozen Lake PDF Author: David F. Barnes
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ISBN:
Category : Ice
Languages : en
Pages : 158

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Effective Transmission of Thermal Radiation from Nuclear Detonations in Real Atmospheres

Effective Transmission of Thermal Radiation from Nuclear Detonations in Real Atmospheres PDF Author: John P. Cahill
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ISBN:
Category : Atomic bomb
Languages : en
Pages : 94

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Refinements in Utilization of Contour Charts for Climatically Specified Wind Profiles

Refinements in Utilization of Contour Charts for Climatically Specified Wind Profiles PDF Author: Allen E. Cole
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ISBN:
Category : Meteorology
Languages : en
Pages : 40

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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
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ISBN:
Category : Geomorphological tracers
Languages : en
Pages : 50

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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.

Mean Annual Mid-latitude Moisture Profiles to 31 Km

Mean Annual Mid-latitude Moisture Profiles to 31 Km PDF Author: Murray Gutnick
Publisher:
ISBN:
Category : Hygrometry
Languages : en
Pages : 56

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Guide for Computation of Horizontal Geodetic Surveys

Guide for Computation of Horizontal Geodetic Surveys PDF Author: Harry R. Kahler
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ISBN:
Category : Geodesy
Languages : en
Pages : 144

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Military Applications of Supercooled Cloud and Fog Dissipation

Military Applications of Supercooled Cloud and Fog Dissipation PDF Author: C. S. Downie
Publisher:
ISBN:
Category : Fog
Languages : en
Pages : 66

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