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Refraction from the Effect of the Atmosphere. The apparent

Altitude is always greater than the true. Refraction great-
est in the Horizon; at 45° in its mean quantity = 574".
Quantity of Refraction changed by the Weight and Tem-
perature of the Atmosphere. Change ascertained by the
Heights of the Barometer and Thermometer. Methods of
Observing Quantity of Refraction. Twilight occasioned
by Reflection of Sun's Rays by Atmosphere.-Lasts till the
Sun is 18° below Horizon. Duration of Twilight. Oval

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