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Differences in the day and night longwave fluxes at satellite altitude for sun-synchronous NOAA-9 nonscanning sensorsThe outgoing LW flux determined by using the data measured by four nonscanning sensors at satellite altitude is reported. The outgoing LW fluxes for MFOV and WFOV sensors at satellite altitude are determined by subtracting the SW fluxes from the total sensors. Results for 1985 and 1986 are discussed. The nighttime LW flux determined by using the MFOV-T channel at the satellite altitude is found to be constant from month to month within 1 W/sq m, while the LW flux from WFOV-T channel varies within 2 to 3 W sq m. The high value for the WFOV-T channel is attributed to the effects of sun-blips on the measurements involved. The main advantage of using day/night longwave flux differences at satellite altitude is that the consistencies of nonscanner sensors can be checked very quickly.
Document ID
19920031297
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Pandey, Dhirendra K.
(ST Systems Corp. Hampton, VA, United States)
Paden, Jack
(ST Systems Corp. Hampton, VA, United States)
Lee, Robert B., III
(NASA Langley Research Center Hampton, VA, United States)
Date Acquired
August 15, 2013
Publication Date
January 1, 1990
Subject Category
Meteorology And Climatology
Meeting Information
Meeting: Conference on Atmospheric Radiation
Location: San Francisco, CA
Country: United States
Start Date: July 23, 1990
End Date: July 27, 1990
Accession Number
92A13921
Funding Number(s)
CONTRACT_GRANT: NAS1-18460
Distribution Limits
Public
Copyright
Other

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