Lunar eclipse

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An eclipse refers to the phenomenon of one body passing into the shadow cast by another body. In astronomy, the best-known type of eclipse occurs whenever the Sun, Earth and Moon line up exactly. If this occurrence is at the time of a Full Moon where the Moon passes through the Earth's shadow, it is called a lunar eclipse. The type and length of a lunar eclipse depends upon the Moon's location relative to its orbital node. If the lining up of the Sun, Moon and Earth occurs at New Moon, the event is usually referred to as a solar eclipse (although the term is a misnomer and can more accurately be referred to as an occultation of the Sun by the Moon).

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Types of lunar eclipses

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A penumbral eclipse occurs when the Moon only passes through the Earth's penumbra, the outer portion of the Earth's shadow. The penumbra does not cause the noticeable darkening of the Moon's surface.

A special type of penumbral eclipse is a total penumbral eclipse. At a total penumbral eclipse the Moon is completely in the penumbra of the Earth, but not in the umbra. At a total penumbral eclipse the parts of the Moon closest to the umbra are a bit darker than the rest of the Moon. Total penumbral eclipses are a rare type of lunar eclipse.

A total lunar eclipse occurs when the Moon travels completely into the Earth's umbra, the dark inner portion of the shadow. The Moon's speed through the shadow is about one kilometer per second, and the totality may last up to nearly 107 minutes. However, the time between the Moon's first contact with the shadow and last contact, when it has completely exited the shadow, may be up to 6 h 14 min or so. If only part of the Moon enters the umbra, it is called a partial lunar eclipse.

Usually, the Moon does not completely disappear as it passes through the umbra because of the refraction of sunlight by the Earth's atmosphere into the shadow cone. The amount of refracted light depends on the amount of clouds or dust in the atmosphere blocking the light. Refracted sunlight causes the Moon to glow with a coppery-red hue that varies from one eclipse to the next. The following scale was devised by André Danjon for rating the overall darkness of lunar eclipses:

0. Very dark eclipse; Moon almost invisible, especially in midtonality
1. Dark eclipse; gray or brownish coloration; details distinguishable only with difficulty
2. Deep red or rust-colored eclipse, with a very dark central part in the umbra and the outer rim of the umbra relatively bright
3. Brick-red eclipse, usually with a bright or yellow rim to the umbra
4. Very bright copper-red or orange eclipse, with a bluish, very bright umbral rim

Because the Moon's orbit around the Earth is inclined 5° with respect to the orbit of the Earth around the Sun, lunar eclipses do not occur at every full moon. For an eclipse to occur, the Moon must be near its orbital node —the intersection of the orbital planes. Passing through the shadow at or very close to the node results in a total or partial eclipse.

The relative distance of the Moon from the Earth at the time of the eclipse can affect the eclipse's intensity. Specifically, a totally-eclipsed Moon being concomitantly at or near apogee will lengthen the duration of totality for two reasons: first, the Moon will appear to move more slowly across the umbra, and second, the Moon will appear smaller as seen from Earth and therefore remain inside the umbra longer.

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Every year there are at least two lunar eclipses. If you know the date and time of an eclipse, you can predict the occurrence of other eclipses using eclipse cycles. Unlike a solar eclipse, which can only be viewed in a certain relatively small area of the world, a lunar eclipse may be viewed from anywhere on the night side of the Earth. If you were on the Moon's surface during a lunar eclipse you would witness a solar eclipse, with the Earth passing in front of the Sun (as is explained above, the term solar "eclipse"—although used frequently—is actually a misnomer; the event is an occultation of the Sun).

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Longest total lunar eclipse between 1900 and 2100

Date Duration of total phase
July 16 2000 1h47m01s
July 6 1982 1h46m20s
July 27 2018 1h43m34s
June 26 2029 1h42m32s
August 4 1906 1h41m48s
July 7 2047 1h41m29s
June 25 1964 1h41m25s
July 26 1953 1h41m22s
June 28 2001 1h41m16s
June 15 2011 1h40m52s
June 16 2076 1h40m49s
July 15 1935 1h40m16s
August 6 1971 1h40m04s

The longest total lunar eclipse between 1000BC and 3000AD took place on May 31 318. Its total phase had a duration of 1h47m14s.

History

Ancient Greek astronomers noticed that during lunar eclipses the edge of the shadow was always circular; they thus concluded that the Earth was spherical. In 499, Indian mathematician Aryabhata gave accurate calculations for both the solar eclipse and lunar eclipse. In 1504, while stranded on Jamaica, Christopher Columbus "predicted" a lunar eclipse (actually, he knew from celestial tables that he had brought with him that a lunar eclipse was to occur on February 29 of that year), thereby intimidating the island's natives into continuing to provision him and his men and thus saving them from death by starvation.

References

  • Alan MacRobert, "October's Ideal Lunar Eclipse", Sky and Telescope (October 2004), p. 74. (Danjon numbers)

See also

External links

Prediction
Animation
Eclipse photos
Fiction

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