Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

The Number of Particles in the Path of a Ray of Light Traversing the Earth's Atmosphere


     

   Subscribe/Renew Journal


It is useful in several astronomical problems to have some knowledge of the number of particles of a gas in the earth's atmosphere, that are encountered by a ray of light proceeding from a stellar source and reaching the observer. For instance, in stellar photometry, it is necessary to know the diminution in the intensity of light from a star due to absorption by the earth's atmosphere; this is easily found, if the number of particles of the absorbing gas and its coefficient of absorption are known. Or again, to deduce the laws of intensity-distribution of the telluric lines in a spectrum such as that of the sun, the number of particles of the gas producing those lines needs to be ascertained. The following is an attempt to arrive at an approximate formula for the number of such particles; which, while taking account of atmospheric refraction, is simple enough for ready calculation.
Subscription Login to verify subscription
User
Notifications
Font Size


Abstract Views: 206

PDF Views: 0




  • The Number of Particles in the Path of a Ray of Light Traversing the Earth's Atmosphere

Abstract Views: 206  |  PDF Views: 0

Authors

Abstract


It is useful in several astronomical problems to have some knowledge of the number of particles of a gas in the earth's atmosphere, that are encountered by a ray of light proceeding from a stellar source and reaching the observer. For instance, in stellar photometry, it is necessary to know the diminution in the intensity of light from a star due to absorption by the earth's atmosphere; this is easily found, if the number of particles of the absorbing gas and its coefficient of absorption are known. Or again, to deduce the laws of intensity-distribution of the telluric lines in a spectrum such as that of the sun, the number of particles of the gas producing those lines needs to be ascertained. The following is an attempt to arrive at an approximate formula for the number of such particles; which, while taking account of atmospheric refraction, is simple enough for ready calculation.