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The Diurnal Variation of the O33) Source Functions and Limb Radiances in the Mesosphere and Lower Thermosphere

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Abstract

In order to determine ozone concentration profiles from the measurement of infrared limb emission in the 900 cm-1 to 1200 cm-1 spectral interval, an accurate knowledge of the terms composing the radiative transfer equation is required.

© 1990 Optical Society of America

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