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Equivalent blackbody temperature of the top of a severe stormAn RB-57F high-altitude aircraft equipped with Wilde RC-8 cameras and an infrared spectrometer was used in the investigations. A storm was overflown over Graham, Texas, on April 29, 1970. In the experiment, the average radiometric temperature was determined to be very near the environmental temperature near the cloud tops. However, hot and cold regions in and near the updrafts and downdrafts were found to be significantly out of equilibrium. It is recommended that caution should be exercised in determining cloud top altitude from equivalent blackbody temperature.
Document ID
19750049039
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Pitts, D. E.
(NASA Johnson Space Center Houston, Tex., United States)
Reeser, W. K.
Mendlowitz, M. A.
(Lockheed Electronics Co., Inc. Houston, Tex., United States)
Date Acquired
August 8, 2013
Publication Date
June 1, 1975
Publication Information
Publication: Journal of Applied Meteorology
Volume: 14
Subject Category
Meteorology And Climatology
Accession Number
75A33111
Distribution Limits
Public
Copyright
Other

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