Use of satellite, surface, and aerological information for the calculation of thermal radiation fluxes

Details Use of satellite, surface, and aerological information for the calculation of thermal radiation fluxes Use of satellite, surface, and aerological information for the calculation of thermal radiation fluxes

Apr 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992fizao..28..378a&link_type=abstract

Rossiiskaia Akademiia Nauk, Izvestiia, Fizika Atmosfery i Okeana (ISSN 0002-3515), vol. 28, no. 4, April 1992, p. 378-383. In Ru

Computer Science

Sound

Aerology, Atmospheric Sounding, Cloud Physics, Heat Flux, Satellite Observation, Thermal Radiation, Weather Stations, Noaa 9 Satellite, Planetary Waves, Surface Temperature, Vertical Distribution

Scientific paper

Data from the NOAA-9 satellite on cloud amount and cloud upper boundary temperature, data from surface weather stations, and results of aerological sounding of the atmosphere are used to calculate the vertical profiles of upward, downward, and effective fluxes of longwave radiation. A comparison of satellite and surface data on cloud amount and underlying surface temperature is presented.

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