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Satellite Data in Meteorological Research
A workshop was held in Boulder, CO from 25 to 31 August 1965 with the purpose of acquainting members of the university community with the latest techniques for using satellite...- publication PDF
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A Thermopile Temperature Sensitivity Calibration Procedure for Eppley Broadba...
This article does not have an abstract or article summary.- publication PDF
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Cloud Particle Measurement Symposium: Summaries and Abstracts
This report includes: Symposium Summaries: Forward Scattering Spectrometer Probes Summary /James E. Dye Optical Array Probes Summary /William A. Cooper General Topics...- publication PDF
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A Generalized Theoretical Analysis of Cross-correlation and Cross-spectra for...
In the analysis of data obtained from SA systems, the most common approach is to assume models of the diffraction pattern without relating it to the statistical properties of...- publication PDF
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Particulate Models: Their Validity and Application; A Workshop Held at the Na...
A workshop on particulate models was held at NCAR in Boulder, Colorado on 21 August 1970 to create more realistic models of atmospheric particulates that are required for...- publication PDF
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Sky Brightness Photometer
This report explains the design development of, and includes the operation manual for, a Sky Brightness Photometer developed by NCAR. This photometer was developed to make...- publication PDF
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Monthly Mean Global Satellite Data Sets Available in CCM History Tape Format
This report describes work completed on the National Aeronautics and Space Administration (NASA) project, "Intercomparison of Satellite-Based Global Data Sets with Global...- publication PDF
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Preprocessing of Airborne Pyranometer Data
Eppley pyranometers are employed to measure the up- and downwelling short wavelength radiation fluxes in the atmosphere. The quality of the data used to investigate the...- publication PDF
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Atlas of Computed Infrared Atmospheric Absorption Spectra: Atmospheric Transm...
An atlas of atmospheric absorption calculations is presented for a vertical path through the atmosphere above altitudes of 4, 14, 30, 40, 45, and 54 km. The calculations are...- publication PDF
