On accounting for temperature and pressure in determining the Rayleigh scattering in the earth's atmosphere

Details On accounting for temperature and pressure in determining the Rayleigh scattering in the earth's atmosphere On accounting for temperature and pressure in determining the Rayleigh scattering in the earth's atmosphere

Jun 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010bcrao.106...87k&link_type=abstract

Bulletin of the Crimean Astrophysical Observatory, Volume 106, Issue 1, pp.87-91

Mathematics

Logic

Rayleigh Optical Depth, Atmospheric Pressure, Temperature

Scientific paper

We calculated the variations of Rayleigh optical depth with changes of pressure and temperature for three observation sites: Simferopol (φ = 44°57'N, λ = 34°8'E, h = 265 m above sea level), Nauchny (φ = 44°43'N, λ = 34°3'E, h = 583 m), and Ai-Petry meteorological station (φ = 44°24'N, λ = 34°6'E, h = 1180 m).

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