The calculation of the optical surfaces tilts having the constant index of the refraction coefficient in the free atmosphere when treating the observations by the equal altitudes method.

Details The calculation of the optical surfaces tilts having the constant index of the refraction coefficient in the free atmosphere when treating the observations by the equal altitudes method. The calculation of the optical surfaces tilts having the constant index of the refraction coefficient in the free atmosphere when treating the observations by the equal altitudes method.

Dec 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996kfnt...12...80z&link_type=abstract

Kinematika Fiz. Nebesn. Tel, Tom 12, No. 6, p. 80 - 85

Computer Science

Earth Atmosphere: Refraction, Earth Atmosphere: Methods Of Reduction

Scientific paper

The author presents the common way of calculating the anomalous
refraction vertical component when treating the observations by the
equal-altitudes method, considering the very part of the component which
is caused by the slope of equal density layers in the atmosphere to the
level surface of the gravity.

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