The occultation (obscuring) of one celestial body by another. Solar and lunar eclipses take place at syzygies of the Sun, Earth, and Moon, when the three bodies are in a line. At a solar eclipse, the Moon blocks the view of the Sun as seen from the Earth. At a lunar eclipse, the Earth's shadow falls on the Moon, darkening it, and can be seen from wherever on Earth the Moon is above the horizon.
Solar eclipses
A solar eclipse can be understood as an occultation of the Sun by the Moon or, equivalently, the Moon's shadow crossing the Earth's surface. The darkest part of the shadow, from which the Sun is entirely hidden, is the umbra (Fig. 1). The outer part of the shadow, from which part of the Sun can be seen, is the penumbra.

Circumstances of solar and lunar eclipses (not to scale).
Solar eclipses can be central, in which the Moon passes entirely onto the solar disk as seen from Earth, or partial, in which one side of the Sun always remains visible. Central eclipses can be total, in which case the Moon entirely covers the solar photosphere, making the corona visible for the period of totality, or annular, in which case the Moon's angular diameter is smaller than that of the Sun because of the positions of the Earth and Moon in their elliptical orbits. At an annular eclipse, a bright annulus of photospheric sunlight remains visible; it is normally thousands of times brighter than the corona, leaving the sky too blue for the corona to be seen.
The plane of the Moon's orbit is inclined by 5° to the plane of the Earth's orbit (the ecliptic), so the Moon's shadow commonly passes above or below the Earth each month at new moon. But two to five times each year, the Moon's shadow reaches the Earth, and a partial, annular, or total eclipse occurs. The Moon is approximately 400 times smaller than the Sun but is also approximately 400 times closer, so its angular diameter in the sky is about the same as the Sun's. Thus the Moon fits approximately exactly over the photosphere, making the phenomenon of a total eclipse especially beautiful.
The partial phases of a total eclipse visible from the path of totality last over an hour. In the minute or two before totality, shadow bands—low-contrast bands of light and dark caused by irregularities in the Earth's upper atmosphere—may be seen to race across the landscape. As the Moon barely covers the Sun, photospheric light shines through valleys on the edge of the Moon, making dots of light—Baily's beads—that are very bright in contrast to the background. The last Baily's bead gleams so brightly that it appears as a jewel on a ring, with the band made of the corona; this appearance is known as the diamond ring effect. It usually lasts for 5–10 s, and in the clearest skies for as long as 40 s.
During the diamond ring effect, the solar chromosphere becomes visible around the limb of the Moon, glowing pinkish because most of its radiation is in the form of emission lines of hydrogen, mostly the red hydrogen-alpha line. Its emission-line spectrum apparently flashes into view for a few seconds, and is called the flash spectrum. As the advancing limb of the Moon covers the chromosphere, the corona becomes fully visible (Fig. 2). Its shape is governed by the solar magnetic field; common are equatorial streamers and polar tufts. At the maximum of the solar activity cycle, so many streamers exist that the corona appears round when it is seen in projection, as viewed from Earth. At the minimum of the solar activity cycle, only a few streamers exist so that the corona appears more elongated in projection. See also Sun.

Total solar eclipse of February 26, 1998, observed from Aruba, Netherlands Antilles. Image is composited from several exposures in order to show the wide dynamic range of intensity of the corona and to bring out the structures of the streamers. (Jay M. Pasachoff and Wendy Carlos)
Totality lasts from an instant up through somewhat over 7 min. At its end, the phenomena repeat, including chromosphere, diamond ring, Baily's beads, shadow bands, and the partial phases.
The paths of the Sun and Moon in the sky intersect at two points, the ascending node and the descending node. Only when both the Sun and the Moon are near a node can an eclipse occur. Thus eclipse seasons take place each year, whenever the Sun is near enough to the node so that an eclipse is possible. Each eclipse season is 38 days long. Because the Sun's gravity causes the orientation of the Moon's elliptical orbit to change with an 18.6-year cycle, the nodes slide along the ecliptic and a cycle of two eclipse seasons—an eclipse year—has a period of 346.6 days, shorter than a solar year. See also Moon.
There must be at least one solar eclipse each eclipse season, so there are at least two each year. There may be as many as five solar eclipses in a calendar year, though most of these will be partial. Adding lunar eclipses (including penumbral lunar eclipses, which may not be noticeable), there may be seven eclipses in a year.
An important coincidence relates lunar months and eclipse years. A total of 223 lunar months (technically, synodic months, the period of the phases) takes 6585.32 days. A total of 19 eclipse years (passages of the Sun through the same node of the Moon's orbit) takes 6585.78 days, and 242 nodical months (passages of the Moon through the node) take 6585.36 days. Thus eclipses appear with this period of 18 years
days (plus or minus a day, depending on leap years), a period known as the saros. Further, 239 periods of the variation of distance of the Moon from the Earth, the anomalistic month, is 6585.54 days, so the relative angular sizes of the Sun and Moon are about the same at this interval. As a result of the saros, almost identical eclipses recur every 18 years
days. The significance of the
day is that the Earth rotates one-third of the way around, and the eclipse path is shifted on the Earth's surface.
Even with advances in space technology, total solar eclipses are the best way of seeing the lower corona. Related eclipse studies include use of the advancing edge of the Moon to provide high spatial resolution for radio observations of the Sun and, historically, of celestial radio sources. See also Solar corona.
The total phase of an eclipse is completely safe to watch with the naked eye. The total brightness of the corona is only that of the full moon, so is equally safe to watch. For direct observation of the partial phases, a special solar filter must be used. Fogged and exposed black-and-white (not color) film that contains silver and is developed to full density provides suitable diminution of the solar intensity across the entire spectrum. Inexpensive commercial solar filters made of aluminized Mylar can also be used. Gelatin “neutral-density” filters are actually not neutral in the infrared, and so should not be used. Neutral-density filters made by depositing chromium or other metals on glass are safe if they are ND4 or ND5, and are commercially available, as is #14 welder's glass.
Lunar eclipses
A lunar eclipse can occur only when the Moon is full and is near one of the nodes of its orbit. If the Moon enters only the penumbral cone of the Earth (Fig. 1), the eclipse is a penumbral one. If the Moon enters the umbra without being entirely immersed in it, a partial (umbral) eclipse occurs. The eclipse is total if the entire Moon enters the umbra.
The magnitude of an eclipse is the fraction of the diameter of the lunar disk which is eclipsed (in the umbra or in the penumbra) at maximum phase. If the magnitude is larger than 1, the eclipse is total. Penumbral eclipses are not observable unless their magnitude (in the penumbra) is greater than about 0.7.
If penumbral eclipses as well as umbral ones are taken into consideration, the least number of lunar eclipses during a calendar year is two, and the maximum number is five. If only umbral eclipses are considered, the least number of lunar eclipses in one calendar year is zero, and the maximum number is three.
When the Moon passes through the center of the Earth's shadow, the entire eclipse takes
to
, depending on the Moon's position in its orbit at the time of the eclipse. The first hour is spent in the penumbra (Fig. 1). No darkening is noticeable until about a quarter hour before the first contact with the umbra, because in the penumbra all of the Moon's side facing Earth is still receiving some direct sunlight. Then as the Moon enters the umbra, the eclipsed part of the Moon appears nearly black by contrast with the bright side of the disk. Approximately the second hour is required for all of the Moon to get into the umbra.
The diameter of the umbra where the Moon crosses it is about
times the Moon's diameter. The total phase of a lunar eclipse can last up to 107 min.
If the Earth had no atmosphere, the Moon would disappear from view while in the umbra. However, the Earth's atmosphere acts like a lens and bends the sunlight into the umbra. The longer waves of red light penetrate the atmosphere better than the short-wave blue light, which is scattered to form the blue of the sky. An observer on the Moon would see the Earth surrounded by a thin ring of bright sunset colors. This explains the usual reddish color of the totally eclipsed Moon. Extremely dark eclipses are due to major volcanic eruptions, whose dust temporarily increases the atmosphere's opacity. See also Refraction of waves.