Seasons and sky

Horizon Refraction

Direct answer

Horizon Refraction is the especially strong and variable atmospheric bending applied to light from objects near the horizon.

Horizon Refraction raises and distorts low celestial objects.

Seasons & Earth AlmanacThe Great Almanac DictionaryUpdated 2026-09-26

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At a glance

Found in
Seasons & Earth Almanac
Related
Inferior Mirage, Green Flash, Astronomical Season, Equinox
Earth and season · visual guide Horizon Refraction

Horizon Refraction raises and distorts low celestial objects.

A Sun-Earth orientation for seasonal, atmospheric, tidal, and terrestrial terms.

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The story behind Horizon Refraction

Navigators and surveyors learned to distrust low-altitude sights because refraction becomes unstable near the horizon.

Why Horizon Refraction matters

Horizon Refraction is a major reason observed sunrise, sunset, Moonrise, and Moonset differ from simple geometric horizon crossings.

Horizon Refraction in practice: an example

A strong temperature inversion can produce layered or unusually flattened sunset images.

Where readings of Horizon Refraction go wrong

A common error is to use a standard refraction value as a guarantee of exact apparent rise time at a real, uneven horizon.

Sources and editorial method

Research references used for this entry include:

Source
The Great Almanac Dictionary
Category
Seasons & Earth Almanac
Last updated
2026-09-26

Allow for the uncertain horizon

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Inferior MirageAn Inferior Mirage is the apparent image below an object over strongly heated ground or water. Green FlashA Green Flash is a fleeting green solar-edge effect near a clear horizon. Astronomical SeasonAn Astronomical Season runs from one equinox or solstice to the next. EquinoxAn Equinox occurs when the Sun crosses the celestial equator. SolsticeA Solstice marks the Sun's greatest apparent northward or southward position. SunriseSunrise is the calculated first appearance of the Sun's upper edge at the horizon.

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Common questions

What is horizon refraction?

Horizon Refraction is the especially strong and variable atmospheric bending applied to light from objects near the horizon.

What do people get wrong about horizon refraction?

A common error is to use a standard refraction value as a guarantee of exact apparent rise time at a real, uneven horizon.

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