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meteor

 
Dictionary: me·te·or   ('tē-ər, -ôr') pronunciation
n.
A bright trail or streak that appears in the sky when a meteoroid is heated to incandescence by friction with the earth's atmosphere. Also called falling star, meteor burst, Also called shooting star.

[Middle English metheour, atmospheric phenomenon, from Old French meteore, from Medieval Latin meteōrum, from Greek meteōron, astronomical phenomenon, from neuter of meteōros, high in the air : meta-, meta- + -āoros, lifted, akin to āeirein, to lift up.]


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Streak of light in the sky that results when a particle or small chunk of stony or metallic matter from space enters Earth's atmosphere and is vapourized by friction. The term is sometimes applied to the falling object itself, properly called a meteoroid. Most meteoroids, traveling at five times the speed of sound or more, burn up in the upper atmosphere, but a large one may survive its fiery plunge and reach the surface as a solid body (meteorite). See also meteor shower.

For more information on meteor, visit Britannica.com.

The luminous streak lasting seconds or fractions of a second and seen at night when a solid, natural body plunges into the Earth's (or another planet's) atmosphere. The entering object is called a meteoroid and, if any of it survives atmospheric passage, the remainder is called a meteorite. Cosmic dust particles (with masses of micrograms) entering the atmosphere and leaving very brief, faint trails are called micrometeors, with the surviving pieces known as micrometeorites. If the apparent brightness of a meteor exceeds that of the planet Venus as seen from Earth, it is called a fireball, and when a bright meteor is seen to explode, it is called a bolide. See also Meteorite; Micrometeorite.

Under normal, clear atmospheric conditions and dark skies (no moonlight or artificial lights), an observer will see an average of five meteors per hour. The spatial distribution of meteoroid orbits relative to the Sun and the circumstances of their intersections with the moving Earth are responsible for pronounced variations in meteor rates.

The average meteor seen by the unaided eye starts with a meteoroid velocity of 18 mi/s (30 km/s) and leaves a luminous trail from 67 to 50 mi (110 to 80 km) high. The meteor trails are rapidly expanding columns of atoms, ions, and electrons dislodged from the meteoroid by collisions with air molecules, and can be excited to temperatures of several thousand degrees Celsius. For a time after trail formation, the free electrons are dense enough to reflect radio waves in the very high frequency range, and therefore can be used to transmit radio messages. See also Radio-wave propagation.

Under the right circumstances, particularly with high-power ultrahigh-frequency (UHF) radars, the ionization right around and moving with the meteoroid itself is seen. This is known as the head echo, and a determination of its velocity is the most accurate way to determine radar meteor speeds. See also Radar; Radar astronomy.

The Earth moves around the Sun with an average speed of 18 mi/s (30 km/s). According to thelaws of celestial mechanics, if a meteoroid comes from beyond the solar system, its velocity at the Earth's distance from the Sun must be greater than 26 mi/s (42 km/s). If such a meteoroid hits the Earth head-on, indications of preatmospheric speeds in excess of 45 mi/s (72 km/s) would be observed. The fact that the vast majority of observed meteoroids have orbits with Earth-approaching velocities of less than 45 mi/s indicates that most of these are comet and asteroid fragments, and are therefore long-term members of the solar system. However, in the 1980s and 1990s, a combination of spacecraft and high-power radar observations indicated that hypervelocity micrometeoids do indeed exist with seeming interstellar dust connections. See also Interstellar matter.

A combination of the meteoroid's and Earth's velocities of travel around the Sun make the meteor itself seem to originate from a specific direction in the sky called the radiant. If there are numerous meteoroids in nearly the same orbit (sometimes incorrectly called meteor streams), the Earth sweeps them up at specific times of the year and a so-called meteor shower is observed. Meteor showers are named after the constellation or single star in the sky from which they appear to radiate. While shower meteoroids are really moving nearly parallel through space and result in nearly parallel meteor trails, the effects of perspective make the meteors appear to diverge from the radiant. Meteors that cannot be shown to be associated with a known shower are termed sporadic meteors.

A number of meteor showers have been observed to be in orbits that are similar to those traveled by known comets. Thus an association between shower meteors and comets has gradually become a firmly entrenched concept. There are numerous theoretical scenarios where vaporization of the more volatile cometary ices ejects small solid particles from the surface of the nucleus. A fair proportion of these fragments, particularly the smaller dust-sized ones, escape and take up their own orbits as meteoroids. Cometary nuclei have been known to split into two or more pieces and, when this occurs, it is likely that particles larger than dust size are released as well.

The strategy of photographic or electronic measurements is to place at least two cameras 10–52 mi (15–85 km) apart over a known baseline, but arranged to examine the same volume of space at a height of about 56 mi (90 km). Each camera has a rotating shutter so that the meteor trail consists of a line of bright dashes. Meteor imaging is one of the most difficult areas of astronomical detection, even with ultrafast cameras. Meteor spectroscopy is even more difficult since the light is spread out over areas hundreds of times larger than the meteor trail itself. See also Astronomical photography; Astronomical spectroscopy.

Radio and radar observations depend on the fact that the initial ion-electron densities in a meteor trail are considerably higher than the average for the ionosphere at an altitude of 56 mi (90 km). For a very high frequency (VHF) or somewhat lower-frequency radar system, the maximum reflected signal occurs when the meteor trail is at right angles to the outgoing wave, with head echoes rarely seen. At ultrahigh frequencies (UHF), radar reflections from the head-echo predominate. From these, high-accuracy radial velocities are determined directly, using the Doppler effect. See also Doppler effect; Radio astronomy.

The parent comet of the Leonid stream, 1866 I, made another of its periodic (33-year intervals) approaches to the Sun in 1999. With the appearance of the comet, it was expected that the strong meteor storm that happened last in 1966 would again make a brief but spectacular appearance. However, perturbations by the outer planets (particularly by Neptune) once again played a significant role in this shower's behavior. The perturbations moved a number of thin meteoroid streams produced by the comet many orbit periods in the past into intersection range of the Earth. This produced a unique succession of strong peaks covering a span of seven years (1996–2003). The scientific yield of this extended display was much more than anyone had hoped. While meteor trails had been previously recorded from the space shuttle and other spacecraft, in 1997 the first above-atmosphere, far-ultraviolet spectrum of a bright meteor was recorded during the Leonid shower. Spectra obtained from the ground also yielded new information. The large number of fireballs in the Leonid streams enabled many details of the ablation processes at higher than average meteoroid incoming velocities to be recorded with high-speed cameras.


 
meteor, appearance of a small particle flying through space that interacts with the earth's upper atmosphere. While still outside the atmosphere, the particle is known as a meteoroid. Countless meteoroids of varying sizes are moving about the solar system at any time. Perhaps a billion meteoroids a day enter the atmosphere, their speeds ranging from 10 to 45 mi (16-72 km) per sec. They experience friction due to collisions with the atmosphere; by the time they reach 50 to 75 mi (80-120 km) from the earth's surface, they have been heated to incandescence through friction and are visible as "shooting stars," or "falling stars." Most disintegrate completely before they reach the earth; those large enough to reach the ground are called meteorites. A meteor of considerable duration and brightness is known as a fireball; a fireball that breaks apart with an explosion is a bolide. The brightest fireball ever recorded fell in the Tunguska Basin, Siberia, in 1908, causing the destruction of forest over an area of about 770 sq mi (2,000 sq km). Meteoroids are composed of stone, iron, or a mixture of stone and iron, with other metals present in very small proportions. Other meteoroids, the carbonaceous chondrites, are stony with a large amount of carbon. Although most meteoroids are quite small, and even though only a very small fraction of them reach the earth's surface, their large quantity accounts for several tons of matter falling on the earth each day. A single observer under a dark sky can see an average of 5 to 10 meteors per hour; more during a meteor shower. More meteors are visible after midnight because the earth's rotation has then positioned the observer's part of the earth in the direction of the earth's motion about the sun. The frequency of meteors also increases when the earth passes through certain swarms of particles that intersect the earth's orbit. Such meteor showers are named for the constellation from which they appear to originate.


Science Dictionary: meteor
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A streak of light in the sky, often called a “shooting star,” that occurs when a bit of extraterrestrial matter falls into the atmosphere of the Earth and burns up.

  • Meteor showers occur at regular times during the year.
  • Word Tutor: meteor
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    pronunciation

    IN BRIEF: n. - (astronomy) any of the small solid extraterrestrial bodies that hits the earth's atmosphere;

    Tutor's tip: Note: If something is "meatier" it contains more meat or substance, not to be confused with "meteor" which is a bright, moving heavenly body.

    Dream Symbol: Meteor
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    Ancient peoples believed that witnessing a meteor streaking across the sky or possessing a piece of a meteor meant that the gods had bestowed a gift from the heavens, which is where the custom of wishing upon a falling star derived. Seeing a meteor in a dream may symbolize a strong desire of the dreamer's or suggest that the dreamer is merely engaging in wishful thinking with regard to some aspect of his or her life.


    Translations: Meteor
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    Dansk (Danish)
    n. - meteor

    idioms:

    • meteor shower    meteorregn

    Nederlands (Dutch)
    meteoor, elk verschijnsel in de atmosfeer

    Français (French)
    n. - météore, étoile filante

    idioms:

    • meteor shower    pluie de météores

    Deutsch (German)
    n. - Meteor

    idioms:

    • meteor shower    Meteorschauer

    Ελληνική (Greek)
    n. - (αστρον., μτφ.) μετέωρο, διάττων

    idioms:

    • meteor shower    βροχή μετεωριτών

    Italiano (Italian)
    meteora

    idioms:

    • meteor shower    pioggia di meteoriti

    Português (Portuguese)
    n. - meteoro (m), estrela cadente (f)

    idioms:

    • meteor shower    chuva de meteoros (f) (Astr.)

    Русский (Russian)
    метеор

    idioms:

    • meteor shower    метеорный поток

    Español (Spanish)
    n. - meteoro, estrella fugaz, meteorito

    idioms:

    • meteor shower    lluvia de meteoritos, lluvia de estrellas

    Svenska (Swedish)
    n. - meteor

    中文(简体)(Chinese (Simplified))
    流星, 大气现象

    idioms:

    • meteor shower    流星雨

    中文(繁體)(Chinese (Traditional))
    n. - 流星, 大氣現象

    idioms:

    • meteor shower    流星雨

    한국어 (Korean)
    n. - 운석, 잠시 나타났다가 사라지는 것

    日本語 (Japanese)
    n. - 流星, 流星体, 隕石, 大気現象

    idioms:

    • meteor shower    流星雨

    العربيه (Arabic)
    ‏(الاسم) نيزك, شهاب‏

    עברית (Hebrew)
    n. - ‮כוכב נופל, מטאור‬


    Best of the Web: meteor
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    Some good "meteor" pages on the web:


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    Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2009. Published by Houghton Mifflin Company. All rights reserved.  Read more
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    Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/ Read more
    Science Dictionary. The New Dictionary of Cultural Literacy, Third Edition Edited by E.D. Hirsch, Jr., Joseph F. Kett, and James Trefil. Copyright © 2002 by Houghton Mifflin Company. Published by Houghton Mifflin. All rights reserved.  Read more
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