Evaluation of Earth's atmospheric brightness temperature at decimetric wavelengths

Details Evaluation of Earth's atmospheric brightness temperature at decimetric wavelengths Evaluation of Earth's atmospheric brightness temperature at decimetric wavelengths

Feb 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995apjs...96..643a&link_type=abstract

The Astrophysical Journal Supplement Series (ISSN 0067-0049), vol. 96, no. 2, p. 643-650

Mathematics

Logic

9

Atmospheric Physics, Brightness Temperature, Decimeter Waves, Earth Atmosphere, Evaluation, Humidity Measurement, Meteorological Balloons, Meteorological Instruments, Pressure Measurement, Temperature Measurement

Scientific paper

Atmospheric profiles of pressure, temperature, and relative humidity, measured with stratospheric balloons, are used to calculate the radiofrequency brightness temperature, Tatm, of the atmospheric signal seen by a ground observer. Below 1 GHz the calculated values are definitely more precise (few percent accuracy), than directly measured values (10% accuracy or worse).

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