Post by ~*~Kit_The_Kat~*~ on Nov 9, 2003 14:19:16 GMT -5
What is a meteor?
A meteor results when a small particle (typically millimetres in size for a visual meteor) of dust orbiting the Sun collides with the Earth's atmosphere. The speed of collision is determined by whether it is a head on collision or otherwise and also the acceleration due to the Earth's gravity. Velocities of collision are between 11 and 72 km/sec (40,000 - 260,000 km/hr). At these immense speeds, the particles are intensely heated in collision with atoms and molecules in the upper atmosphere causing both the particle and air surrounding it to glow. This phenomenon is known as a meteor. From this explanation it is clear why the phrases "falling star" or "shooting star", whilst descriptive, can be seriously misleading. Meteors typically "burn up" at heights around 90 km but for a typical Leonid meteor having a near head-on collision speed of 71 km/sec, the height is typically over 100 km.
Meteor storms
On an average night, around 5 to 10 meteors can be seen in an hour from a dark country location. The term "storm" is thus most apt for the 1966 Leonids, when a peak rate of over 100,000 meteors/hr was estimated by observers in western North America. For about quarter of an hour either side of maximum, the rates were over half this value. Eyewitness accounts of the 1966 storm, for which only vague predictions existed, were typically expressions of awe and great excitement. It is no wonder therefore that throughout history, many cultures across the world have clearly documented the occurrence of meteor storms.
History of the Leonid shower
One of the first scientific accounts of a Leonid storm was by Alexander von Humboldt, a Prussian aristocrat, explorer and polymath. He witnessed the 1799 storm from South America during his exploration of the Orinoco. His account of meteors pouring from the sky is but one tiny part of the multi-volume report of his expeditions.
It was the 1833 Leonid storm witnessed over North America that resulted in the modern study of meteors. This event led to the recognition of Leonid storms in historical records going back to 902 AD and to the 33 year periodicity in their occurrence. High activity from the Leonids can happen over several years every 33 years or so, but away from these years, the Leonid rates are typically only a few tens of meteors per hour at best.
In 1866 a Leonid storm came on cue, with good activity also in 1867 and 1869. Around this time another major advance in meteor science took place. Comet searchers found two bright comets, one became named Swift-Tuttle and the other Tempel-Tuttle after their discoverers. In both cases, the orbits of the comets around the Sun were shown to be basically identical to known meteor showers, the August Perseids in the case of comet Swift-Tuttle and the Leonids in the case of Tempel-Tuttle. It was clear that shower meteors were directly related to comets.
Showers and radiants
Meteor showers occur at the same time each year because the orbits of the dust and the Earth form a sort of celestial crossroads. Once a year, at the same point (the dates can differ by a day from year to year due to the nature of the calender and the gravitational pull of the planets on the orbiting dust) the Earth goes through the crossroads. The number of meteors seen from that shower will depend on the amount of "traffic" at the time. The number of particles encountered is related to the way the dust comes off the comet and how long ago it was ejected. With all the dust particles from a particular shower having closely similar motions, their paths in the atmosphere are parallel. Parallel lines, like railway lines converging towards the horizon, appear to radiate from a central point. For a meteor shower, this point is called the radiant and the constellation in which the radiant lies gives its name to the shower. The particles from comet Tempel-Tuttle radiate from the constellation Leo and are therefore called the Leonids.
Predicting Leonid activity
The orbital period of comet Tempel-Tuttle is 33.2 years, and with the major Leonid activity being in the years just following the passage of the comet it appeared that the debris formed a cloud that lagged the comet. The stage was then set for the 1899 Leonids and astronomers had enthusiastically predicted a major event. When very little happened in that or subsequent years, astronomy suffered a major blow to its credibility in the eyes of the public. This simple adding of 33 years to the last period of high activity was shown to be rather naive. Irish astronomers Johnstone Stoney and Arthur Downing were amongst a few scientists that pointed out the effect of the gravitational attraction of the planets (particularly Jupiter, Saturn and Uranus) on the orbit of the comet and the dust. By 1899, the orbits had been shifted away from Earth intersection and prospects were no better around 1932. Indeed very little happened from the Leonids in the early 1930's.
When 1966 came around, astronomy was a much more vibrant science with increased amateur participation. Whilst little was specifically predicted for that year, mostly due to no calculations having being made, the huge Leonid storm that took place was very well observed by hundreds of amateur and professional astronomers in North America. This led to new attempts to calculate future storms.
A meteor results when a small particle (typically millimetres in size for a visual meteor) of dust orbiting the Sun collides with the Earth's atmosphere. The speed of collision is determined by whether it is a head on collision or otherwise and also the acceleration due to the Earth's gravity. Velocities of collision are between 11 and 72 km/sec (40,000 - 260,000 km/hr). At these immense speeds, the particles are intensely heated in collision with atoms and molecules in the upper atmosphere causing both the particle and air surrounding it to glow. This phenomenon is known as a meteor. From this explanation it is clear why the phrases "falling star" or "shooting star", whilst descriptive, can be seriously misleading. Meteors typically "burn up" at heights around 90 km but for a typical Leonid meteor having a near head-on collision speed of 71 km/sec, the height is typically over 100 km.
Meteor storms
On an average night, around 5 to 10 meteors can be seen in an hour from a dark country location. The term "storm" is thus most apt for the 1966 Leonids, when a peak rate of over 100,000 meteors/hr was estimated by observers in western North America. For about quarter of an hour either side of maximum, the rates were over half this value. Eyewitness accounts of the 1966 storm, for which only vague predictions existed, were typically expressions of awe and great excitement. It is no wonder therefore that throughout history, many cultures across the world have clearly documented the occurrence of meteor storms.
History of the Leonid shower
One of the first scientific accounts of a Leonid storm was by Alexander von Humboldt, a Prussian aristocrat, explorer and polymath. He witnessed the 1799 storm from South America during his exploration of the Orinoco. His account of meteors pouring from the sky is but one tiny part of the multi-volume report of his expeditions.
It was the 1833 Leonid storm witnessed over North America that resulted in the modern study of meteors. This event led to the recognition of Leonid storms in historical records going back to 902 AD and to the 33 year periodicity in their occurrence. High activity from the Leonids can happen over several years every 33 years or so, but away from these years, the Leonid rates are typically only a few tens of meteors per hour at best.
In 1866 a Leonid storm came on cue, with good activity also in 1867 and 1869. Around this time another major advance in meteor science took place. Comet searchers found two bright comets, one became named Swift-Tuttle and the other Tempel-Tuttle after their discoverers. In both cases, the orbits of the comets around the Sun were shown to be basically identical to known meteor showers, the August Perseids in the case of comet Swift-Tuttle and the Leonids in the case of Tempel-Tuttle. It was clear that shower meteors were directly related to comets.
Showers and radiants
Meteor showers occur at the same time each year because the orbits of the dust and the Earth form a sort of celestial crossroads. Once a year, at the same point (the dates can differ by a day from year to year due to the nature of the calender and the gravitational pull of the planets on the orbiting dust) the Earth goes through the crossroads. The number of meteors seen from that shower will depend on the amount of "traffic" at the time. The number of particles encountered is related to the way the dust comes off the comet and how long ago it was ejected. With all the dust particles from a particular shower having closely similar motions, their paths in the atmosphere are parallel. Parallel lines, like railway lines converging towards the horizon, appear to radiate from a central point. For a meteor shower, this point is called the radiant and the constellation in which the radiant lies gives its name to the shower. The particles from comet Tempel-Tuttle radiate from the constellation Leo and are therefore called the Leonids.
Predicting Leonid activity
The orbital period of comet Tempel-Tuttle is 33.2 years, and with the major Leonid activity being in the years just following the passage of the comet it appeared that the debris formed a cloud that lagged the comet. The stage was then set for the 1899 Leonids and astronomers had enthusiastically predicted a major event. When very little happened in that or subsequent years, astronomy suffered a major blow to its credibility in the eyes of the public. This simple adding of 33 years to the last period of high activity was shown to be rather naive. Irish astronomers Johnstone Stoney and Arthur Downing were amongst a few scientists that pointed out the effect of the gravitational attraction of the planets (particularly Jupiter, Saturn and Uranus) on the orbit of the comet and the dust. By 1899, the orbits had been shifted away from Earth intersection and prospects were no better around 1932. Indeed very little happened from the Leonids in the early 1930's.
When 1966 came around, astronomy was a much more vibrant science with increased amateur participation. Whilst little was specifically predicted for that year, mostly due to no calculations having being made, the huge Leonid storm that took place was very well observed by hundreds of amateur and professional astronomers in North America. This led to new attempts to calculate future storms.
