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Eta Aquariids

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A meteor shower is a celestial event in which a number of meteors are observed to radiate, or originate, from one point in the night sky . These meteors are caused by streams of cosmic debris called meteoroids entering Earth's atmosphere at extremely high speeds on parallel trajectories. Most meteors are smaller than a grain of sand, so almost all of them disintegrate and never hit the Earth's surface. Very intense or unusual meteor showers are known as meteor outbursts and meteor storms , which produce at least 1,000 meteors an hour, most notably from the Leonids . The Meteor Data Centre lists over 900 suspected meteor showers of which about 100 are well established. Several organizations point to viewing opportunities on the Internet. NASA maintains a daily map of active meteor showers.

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39-401: The Eta Aquariids are a meteor shower associated with Halley's Comet . The shower is visible from about April 19 to about May 28 each year with peak activity on or around May 5. Unlike most major annual meteor showers, there is no sharp peak for this shower, but rather a broad maximum with good rates that last approximately one week centered on May 5. The meteors we currently see as members of

78-701: A Greek or Roman letter assigned that is close to the radiant position at the peak of the shower, whereby the grammatical declension of the Latin possessive form is replaced by "id" or "ids." Hence, meteors radiating from near the star Delta Aquarii (declension "-i") are called the Delta Aquariids . The International Astronomical Union's Task Group on Meteor Shower Nomenclature and the IAU's Meteor Data Center keep track of meteor shower nomenclature and which showers are established. A meteor shower results from an interaction between

117-483: A cloud of particles in space. Work continued, yet coming to understand the annual nature of showers though the occurrences of storms perplexed researchers. The actual nature of meteors was still debated during the 19th century. Meteors were conceived as an atmospheric phenomenon by many scientists ( Alexander von Humboldt , Adolphe Quetelet , Julius Schmidt ) until the Italian astronomer Giovanni Schiaparelli ascertained

156-552: A mostly dormant comet. Examples are the Quadrantids and Geminids , which originated from a breakup of asteroid-looking objects, (196256) 2003 EH 1 and 3200 Phaethon , respectively, about 500 and 1000 years ago. The fragments tend to fall apart quickly into dust, sand, and pebbles and spread out along the comet's orbit to form a dense meteoroid stream, which subsequently evolves into Earth's path. Shortly after Whipple predicted that dust particles traveled at low speeds relative to

195-458: A planet, such as Earth, and streams of debris from a comet . Comets can produce debris by water vapor drag, as demonstrated by Fred Whipple in 1951, and by breakup. Whipple envisioned comets as "dirty snowballs," made up of rock embedded in ice, orbiting the Sun . The "ice" may be water , methane , ammonia , or other volatiles , alone or in combination. The "rock" may vary in size from a dust mote to

234-485: A shower component called a filament. A second effect is a close encounter with a planet. When the meteoroids pass by Earth, some are accelerated (making wider orbits around the Sun), others are decelerated (making shorter orbits), resulting in gaps in the dust trail in the next return (like opening a curtain, with grains piling up at the beginning and end of the gap). Also, Jupiter's perturbation can dramatically change sections of

273-491: A small boulder. Dust mote sized solids are orders of magnitude more common than those the size of sand grains, which, in turn, are similarly more common than those the size of pebbles, and so on. When the ice warms and sublimates, the vapor can drag along dust, sand, and pebbles. Each time a comet swings by the Sun in its orbit , some of its ice vaporizes, and a certain number of meteoroids will be shed. The meteoroids spread out along

312-434: Is only above the horizon for the few hours before dawn, and early-rising observers are often rewarded with rates that climb as the radiant rises before sunrise. The shower is best viewed from the equator to 30 degrees south latitude. The activity is fairly constant from one return to the next. However, in 2013, the maximum Zenithal Hourly Rate (ZHR) exceeded the average level significantly for about two days. An explanation

351-459: Is the Perseids , which peak on 12 August of each year at over one meteor per minute. NASA has a tool to calculate how many meteors per hour are visible from one's observing location. The Leonid meteor shower peaks around 17 November of each year. The Leonid shower produces a meteor storm, peaking at rates of thousands of meteors per hour. Leonid storms gave birth to the term meteor shower when it

390-626: The 2nd millennium , the 67th year of the 19th century , and the 8th year of the 1860s decade. As of the start of 1867, the Gregorian calendar was 12 days ahead of the Julian calendar, which remained in localized use until 1923. There were only 354 days this year in the newly purchased territory of Alaska . When the territory transferred from the Russian Empire to the United States ,

429-500: The Institut de Mécanique Céleste et de Calcul des Éphémérides (IMCCE). Because meteor shower particles are all traveling in parallel paths and at the same velocity, they will appear to an observer below to radiate away from a single point in the sky. This radiant point is caused by the effect of perspective , similar to parallel railroad tracks converging at a single vanishing point on the horizon. Meteor showers are normally named after

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468-400: The constellation Aquarius , near one of the constellation's brightest stars, Eta Aquarii . The shower peaks at about a rate of around a meteor per minute, although such rates are rarely seen from northern latitudes due to the low altitude of the radiant. The Eta Aquariids are best viewed in the pre-dawn hours away from the glow of city lights. For northern observers, the radiant of the shower

507-454: The 1995 Alpha Monocerotids outburst from dust trails. In anticipation of the 1999 Leonid storm, Robert H. McNaught , David Asher , and Finland's Esko Lyytinen were the first to apply this method in the West. In 2006 Jenniskens published predictions for future dust trail encounters covering the next 50 years. Jérémie Vaubaillon continues to update predictions based on observations each year for

546-422: The 1995 alpha Monocerotids , and from earlier not widely known identifications of past Earth storms. Over more extended periods, the dust trails can evolve in complicated ways. For example, the orbits of some repeating comets, and meteoroids leaving them, are in resonant orbits with Jupiter or one of the other large planets – so many revolutions of one will equal another number of the other. This creates

585-502: The Eta Aquariid shower separated from Halley's Comet hundreds of years ago. The current orbit of Halley's Comet does not pass close enough to the Earth to be a source of meteoric activity. Eta Aquariid outbursts occurred in 74 BCE, 401, 443, 466, 530, 839, 905, 927, and 934. The Eta Aquariids were the first meteor shower linked to Halley's comet and are usually two to three times stronger than

624-553: The International Astronomical Union's list of meteor showers. Any other Solar System body with a reasonably transparent atmosphere can also have meteor showers. As the Moon is in the neighborhood of Earth it can experience the same showers, but will have its own phenomena due to its lack of an atmosphere per se , such as vastly increasing its sodium tail . NASA now maintains an ongoing database of observed impacts on

663-594: The October Orionids . The Eta Aquariids are the third strongest annual meteor shower observable at Earth and occur at the descending node of Halley's comet. The descending node reached its closest distance to Earth around 500. Currently Earth approaches Halley's orbit at a distance of 0.065  AU (9.7 million  km ; 6.0 million  mi ; 25  LD ) during the Eta Aquariids. The Eta Aquariids get their name because their radiant appears to lie in

702-484: The Sun ;– while more massive objects (responsible for bolides or fireballs ) will tend to be affected less by radiation pressure. This makes some dust trail encounters rich in bright meteors, others rich in faint meteors. Over time, these effects disperse the meteoroids and create a broader stream. The meteors we see from these streams are part of annual showers , because Earth encounters those streams every year at much

741-550: The anticipated Leonid shower return of 1898 and 1899. Meteor storms were expected, but the final calculations showed that most of the dust would be far inside Earth's orbit. The same results were independently arrived at by Adolf Berberich of the Königliches Astronomisches Rechen Institut (Royal Astronomical Computation Institute) in Berlin, Germany. Although the absence of meteor storms that season confirmed

780-644: The calculations, the advance of much better computing tools was needed to arrive at reliable predictions. In 1981, Donald K. Yeomans of the Jet Propulsion Laboratory reviewed the history of meteor showers for the Leonids and the history of the dynamic orbit of Comet Tempel-Tuttle. A graph from it was adapted and re-published in Sky and Telescope . It showed relative positions of the Earth and Tempel-Tuttle and marks where Earth encountered dense dust. This showed that

819-630: The calendric transition from the Julian to the Gregorian Calendar was made with only 11 days instead of 12 during the 19th century . This change was made due to the territorial and geopolitical shift from the Asian to the American side of the International Date Line . Friday, 6 October 1867 (Julian Calendar) was followed by Friday again on 18 October 1867 (instead of Saturday, 19 October 1867 in

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858-561: The comet, Milos Plavec was the first to offer the idea of a dust trail , when he calculated how meteoroids, once freed from the comet, would drift mostly in front of or behind the comet after completing one orbit. The effect is simple celestial mechanics  – the material drifts only a little laterally away from the comet while drifting ahead or behind the comet because some particles make a wider orbit than others. These dust trails are sometimes observed in comet images taken at mid infrared wavelengths (heat radiation), where dust particles from

897-501: The constellation from which the meteors appear to originate. This "fixed point" slowly moves across the sky during the night due to the Earth turning on its axis, the same reason the stars appear to slowly march across the sky. The radiant also moves slightly from night to night against the background stars (radiant drift) due to the Earth moving in its orbit around the Sun. See IMO Meteor Shower Calendar 2017 ( International Meteor Organization ) for maps of drifting "fixed points." When

936-401: The dust trail, especially for a short period comets, when the grains approach the giant planet at their furthest point along the orbit around the Sun, moving most slowly. As a result, the trail has a clumping , a braiding or a tangling of crescents , of each release of material. The third effect is that of radiation pressure which will push less massive particles into orbits further from

975-436: The entire trajectory of the comet to form a meteoroid stream, also known as a "dust trail" (as opposed to a comet's "gas tail" caused by the tiny particles that are quickly blown away by solar radiation pressure). Recently, Peter Jenniskens has argued that most of our short-period meteor showers are not from the normal water vapor drag of active comets, but the product of infrequent disintegrations, when large chunks break off

1014-635: The event most accurately. After spending the last weeks of 1833 collecting information, he presented his findings in January 1834 to the American Journal of Science and Arts , published in January–April 1834, and January 1836. He noted the shower was of short duration and was not seen in Europe , and that the meteors radiated from a point in the constellation of Leo . He speculated the meteors had originated from

1053-427: The meteoroids are mostly behind and outside the path of the comet, but paths of the Earth through the cloud of particles resulting in powerful storms were very near paths of nearly no activity. In 1985, E. D. Kondrat'eva and E. A. Reznikov of Kazan State University first correctly identified the years when dust was released which was responsible for several past Leonid meteor storms. In 1995, Peter Jenniskens predicted

1092-466: The meteoroids due to increased distance from the sun should marginally decrease meteor brightness. This is somewhat balanced because the slower descent means that Martian meteors have more time to ablate. On March 7, 2004, the panoramic camera on Mars Exploration Rover Spirit recorded a streak which is now believed to have been caused by a meteor from a Martian meteor shower associated with comet 114P/Wiseman-Skiff . A strong display from this shower

1131-507: The moon maintained by the Marshall Space Flight Center whether from a shower or not. Many planets and moons have impact craters dating back large spans of time. But new craters, perhaps even related to meteor showers are possible. Mars, and thus its moons, is known to have meteor showers. These have not been observed on other planets as yet but may be presumed to exist. For Mars in particular, although these are different from

1170-444: The moving radiant is at the highest point, it will reach the observer's sky that night. The Sun will be just clearing the eastern horizon. For this reason, the best viewing time for a meteor shower is generally slightly before dawn — a compromise between the maximum number of meteors available for viewing and the brightening sky, which makes them harder to see. Meteor showers are named after the nearest constellation, or bright star with

1209-620: The objects in the Solar System with an atmosphere: Mercury, Venus, Saturn's moon Titan , Neptune's moon Triton , and Pluto . 1867 1867 ( MDCCCLXVII ) was a common year starting on Tuesday of the Gregorian calendar  and a common year starting on Sunday of the Julian calendar , the 1867th year of the Common Era (CE) and Anno Domini (AD) designations, the 867th year of

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1248-401: The ones seen on Earth because of the different orbits of Mars and Earth relative to the orbits of comets. The Martian atmosphere has less than one percent of the density of Earth's at ground level, at their upper edges, where meteoroids strike; the two are more similar. Because of the similar air pressure at altitudes for meteors, the effects are much the same. Only the relatively slower motion of

1287-415: The previous return to the Sun are spread along the orbit of the comet (see figures). The gravitational pull of the planets determines where the dust trail would pass by Earth orbit, much like a gardener directing a hose to water a distant plant. Most years, those trails would miss the Earth altogether, but in some years, the Earth is showered by meteors. This effect was first demonstrated from observations of

1326-412: The relation between meteors and comets in his work "Notes upon the astronomical theory of the falling stars" ( 1867 ). In the 1890s, Irish astronomer George Johnstone Stoney (1826–1911) and British astronomer Arthur Matthew Weld Downing (1850–1917) were the first to attempt to calculate the position of the dust at Earth's orbit. They studied the dust ejected in 1866 by comet 55P/Tempel-Tuttle before

1365-414: The same rate. When the meteoroids collide with other meteoroids in the zodiacal cloud , they lose their stream association and become part of the "sporadic meteors" background. Long since dispersed from any stream or trail, they form isolated meteors, not a part of any shower. These random meteors will not appear to come from the radiant of the leading shower. In most years, the most visible meteor shower

1404-599: Was expected on December 20, 2007. Other showers speculated about are a "Lambda Geminid" shower associated with the Eta Aquariids of Earth ( i.e. , both associated with Comet 1P/Halley ), a "Beta Canis Major" shower associated with Comet 13P/Olbers , and "Draconids" from 5335 Damocles . Isolated massive impacts have been observed at Jupiter: The 1994 Comet Shoemaker–Levy 9 which formed a brief trail as well, and successive events since then (see List of Jupiter events .) Meteors or meteor showers have been discussed for most of

1443-632: Was first realised that, during the November 1833 storm, the meteors radiated from near the star Gamma Leonis. The last Leonid storms were in 1999, 2001 (two), and 2002 (two). Before that, there were storms in 1767, 1799, 1833, 1866, 1867, and 1966. When the Leonid shower is not storming , it is less active than the Perseids. See the Infographics on Meteor Shower Calendar-2021 on the right. Official names are given in

1482-556: Was presented by Mikiya Sato (Sato & Watanabe, 2013), showing that the meteoroids are from a very old ejection from the parent Halley's Comet and are in resonances to Jupiter's orbit (similar to the Orionids observed between 2007 and 2010). The peak ZHR reached 135 ± 16. Updated information on the expected time and rates of the shower is provided through the annual IMO Meteor Shower Calendar. Meteor shower A meteor shower in August 1583

1521-605: Was recorded in the Timbuktu manuscripts . In the modern era, the first great meteor storm was the Leonids of November 1833. One estimate is a peak rate of over one hundred thousand meteors an hour, but another, done as the storm abated, estimated more than two hundred thousand meteors during the 9 hours of the storm, over the entire region of North America east of the Rocky Mountains . American Denison Olmsted (1791–1859) explained

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