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Meteor Showers |
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SETI Team!
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Contents:
Viewing Activity from the 2008 Orionid Meteor Shower
The Orionids are best known as being one of two meteor showers associated with
Halley's Comet. This shower is active throughout most of October and the first
week of November. A plateau of maximum activity is reached for several nights
centered on October 21, when rates usually average 10-15 shower members per hour.
Recently however, the Orionids have been quite strong, rivaling the rates produced
by the Perseids of August. These strong displays have also been accompanied by
fireballs, bright meteors that exceed the brightness of Venus. Unfortunately rates
this year are most likely to be back to normal. This is not caused by a prediction
of lower rates, but rather the fact that the last quarter moon will be in the sky
during this display. The half-illuminated moon will obscure the fainter meteors
and will reduce counts.
The Orionids reach a zenith hourly rate of 1 near October 2. Rates slowly increase
as the date of maximum activity draws near. After October 10, the waxing moon will
begin to interfere and will retard the increase in rates. It will be difficult to
view Orionid activity right up to the 21st. On the 21st, the moon will lie on the
Cancer-Gemini border, not far from the Orionid radiant. Viewing close to the radiant
will be highly discouraged as the moon will ruin your night vision. I would suggest
viewing toward the northern or western portion of the sky. This will keep the moon
out of your field of view. For those south of the equator, view toward the south or
west. With the radiant out of your field of view, seeing Orionids will be easy as
shower members will all be parallel and will also possess similar velocities. It will
be impossible to filter out any members of the Epsilon Geminids but members of the
Taurids will be easy to tell apart due to their much slower velocity. Most sporadic
meteors will appear moving in different directions and have different speeds when
compared to the Orionids.
The Orionids cannot be seen during the early evening hours as the radiant is below
the horizon until 2200 (10pm) local daylight time (LDT). Rates will be low prior to
midnight as the radiant lies too close to the horizon. After midnight activity
increases until the radiant culminates near 0500 LDT. During the short time between
culmination and the beginning of morning twilight rates will slowly decrease as the
radiant loses altitude.
In early October the Orionid radiant lies in northern Orion near the head of the
great hunter. By the 21st the radiant has drifted into the "club" of Orion near the
Orion/Gemini border. After maximum activity the radiant enters southwestern Gemini
where it spend the remainder of its days. Since the radiant lies close to the celestial
equator the Orionids are seen equally well from both hemisphere. Those north of the
equator may have a slight advantage as the radiant lies a bit higher in the sky
(depending on your latitude) and the October nights are longer in the northern
hemisphere.
These meteors strike the Earth's atmosphere from nearly a head-on direction therefore
most of them will appear to move swiftly through the sky. The exceptions will be
Orionids that appear foreshortened near the radiant or those that appear near the
horizon. While produced by particles released by Halley's Comet, the current orbit
of Halley's Comet does not pass close to the Earth. Therefore the Orionids we see
today were released by the comet many hundreds of years ago.
It is also enjoyable and scientifically useful to record the meteor activity you
see. Experts in meteor astronomy can reduce your data and compare it to others
all over the world if you use certain standards in your reporting. First and foremost
is to provide the accurate time of your observing session. It is helpful to time each
meteor but not absolutely necessary as long as the start and finish times are provided.
The observing conditions are very important to properly record, especially if your
field of view is obscured by clouds or trees. These obscurations should be recorded
to the nearest ten percent. Once per session is fine for trees but at least every
15 minutes for changing conditions such as cloudiness. The limiting magnitude of
the sky in your field of view should also be recorded at least once an hour. The
easiest way to do this is to count the number of stars visible in pre-selected areas
of the sky. These star count areas and the resulting equivalent limiting magnitudes are available online
from the IMO web site at:
http://www.imo.net/visual/major/observation/lm
It is also necessary to classify each meteor seen. Near October 21st, a majority of the
meteors seen will be Orionids. There is no way that every meteor is an Orionid that
night. There are on average 10-15 random meteors occurring each hour. These can come
from any direction and be of any velocity, usually slower than the Orionids. Orionids
will always line up with the radiant in Orion and as mentioned before, will usually be swift unless they
occur close to the radiant or close to the horizon. Other parameters that can be
recorded are the magnitudes of each meteor, the color, the velocity (slow, medium,
fast) and whether the meteor produced a persistent train. If you do decide to record
data, be sure to share it with us by emailing them to our operations manager
Robert Lunsford.
This is the last major shower of 2008 that does not coincide with the full moon.
Not until the Quadrantids of January 2009 will a major shower peak under favorable
conditions. Take every opportunity to view this display and to share your observations
with us.
From earliest times, humankind has noticed flurries of meteors that seemed to emanate
from points in the sky at particular times of the year. These flurries,
now called meteor showers, are produced by small fragments of cosmic debris
entering the earth's atmosphere at extremely high speed. Each time a comet swings
by the sun, it produces large amounts of small particles which will eventually spread
out along the entire orbit of the comet to form a meteoroid "stream." If the Earth's
orbit and the comet's orbit intersect at some point, then the Earth will pass through
this stream for a few days at roughly the same time each year, producing a meteor shower.
Because meteor shower particles are all traveling in parallel paths (see the figure
above), and at the same velocity, they will all appear to radiate from a single point
in the sky to an observer below (see the figure at the top of the page). This radiant
point is caused by the effect of perspective, similar to railroad tracks converging at
a single vanishing point on the horizon when viewed from the middle of the tracks.
This effect is illustrated in the photograph shown above. Meteors seen near the radiant
are approaching the observer and will appear as short streaks in the sky. Meteors seen
45 to 135 degrees from the radiant are moving in a more parallel direction to the observer.
These meteors will produce longer streaks in the sky. Those seen in excess of 90 degrees
from the radiant are actually moving away from the observer and their paths will again
shorten the further the are from the radiant.
Meteor showers are usually named for the constellation in which their radiant lies
at the time of shower maximum. Thus, the Perseid meteor shower (peaking
about August 12) will appear to radiate from the constellation of Perseus,
while the Leonid meteor shower (peaking about November 17) will appear to
radiate from the constellation Leo.
Specific suggestions for observing meteor showers may be found on our Visual Observing Program page.
The meteor showers discussed below recur each year; in some cases they have been recognized for
hundreds of years. The name of the shower in most cases indicates the constellation from which
the meteors appear. Also discussed are sporadic rates. Sporadic meteors are those random meteors
not associated with a particular shower; they are the random detritus left over from the creation
of the solar system or are old dispersed debris not recognizable today as shower meteors. Click on
the shower names (when linked) for more detail on any given shower. For meteor observers, those
located in the northern hemisphere have a distinct advantage as shower activity is stronger there than
that seen by observers located south of the equator. The reason for this is that most of the
major showers have meteors that strike the Earth in areas located far above the equator. As seen
from the northern hemisphere these meteors would appear to rain down from high in the sky in all
directions. From those situated in the southern hemisphere only a small percentage of this activity
is visible. Any activity would appear to travel upwards from radiants located low in the sky.
There are a few meteor showers best seen from the southern hemisphere. These would include any
radiant with a declination (celestial latitude) below -20 and those that reach maximum activity
during the southern hemisphere's winter months (July-August-September). These showers would include
the Alpha Centaurids, Gamma Normids, Pi Puppids, Piscis Austrinids, Delta Aquarids, Alpha Capricornids,
Dec Phoenicids, and the Puppid/Velids.
The year begins with the intense but brief Quadrantid maximum (January 3/4). Its brevity combined with typically poor winter weather hampers observation. January overall has good meteor rates restricted to the last third of the night. Rates to 20/hour can be obtained. A large number of radiants spread along the ecliptic from Cancer to Virgo. This activity diminishes somewhat in February with the same areas active.
Late-night rates are fair in the first half of March, but become poor rather suddenly
after mid-March. The very poor rates, seldom reaching 10/hour, continue into early June. However, two major showers appear in this interval. The Lyrids past mid-April (max: April 21/22) raise meteor rates for several nights. The Eta Aquarids (max: May 5/6) enrich late nights of May's first half, sometimes substantially.
February, March, and April evenings have another notable feature. An unusual number of sporadic fireballs come in this interval, possibly one every few nights.
June to mid-July has fair rates. The last half of July has rates increasing steadily as the
Delta Aquarids (July 27/28) and Alpha Capricornids (July 30 - August 1) have maxima at month's end. Even the Perseids are beginning to show a little.
Overall, late July to mid-August is very rich in meteors. The Perseid maximum, just before mid-August (August 12/13), is fairly prolonged and quite rich.
High sporadic activity after midnight continues for the rest of the year, but especially
in September and the first half of December. Sporadic rates over 20/hour are possible for this entire interval. September radiants are numerous in Aries and Taurus.
Mid-October to mid-December is a nearly continuous period of heavy meteor activity.
The Orionids (max: October 21/22) during the second half of October have a prolonged, plateau maximum for several nights, usually rich. The Taurids (max: November 5/6 for S. Taurids, November 11/12 for N. Taurids), active for two months, are most numerous in November's first half, and can be rather variable in strength. This period is the best for a couple of Taurid fireballs each night, if the shower is not too weak. The Leonids of mid-November (max: November 17-19) are quite unpredictable, with rich displays occuring roughly every 33 years. The last Leonid storm period occurred from 1998 through 2002.
The next enhancement for the Leonids is predicted in 2006, when rates may approach
60/hr. for a short time. Studies have shown that no Leonid storms will occur in
either 2033 or 2066. We will have to wait until 2099 for a return of the activity
recently seen during the past few years.
Finally the Geminids of mid-December (max: December 13/14) climax the year with the strongest dependable and observable display. Geminid rates usually pass 60-70/hour at maximum. Concurrent activity from Leo and Canis Minor is also notable during the Geminids. Finally, the oft-overlooked Ursids complete the year's activity, reaching maximum on December 21/22. Nearly half the year's visual meteor activity is crammed into the two-month interval just described.
Activity Period: the dates when the ZHR (Zenith Hourly Rates) are equal to or greater than one.
Maximum: the date on which the maximum activity is expected to occur.
S.L.: the equivalent solar longitude of the date of maximum activity.
Solar longitude is measured in degrees (0-359) with 0 occurring at the exact moment
of the spring equinox, 90 at the summer solstice, 180 at the autumnal equinox, and
270 at the winter solstice.
Radiant: the area in the sky where shower meteors seem to appear from. This position
is given in right ascension (celestial longitude) and declination (celestial latitude).
Velocity: the velocity at which shower meteors strike the Earth's atmosphere.
The velocity depends on the angle meteoroids (meteors in space) intersect the Earth.
Meteoroids orbiting in the opposite direction of the Earth and striking the atmosphere
head-on are much faster than those orbiting in the same direction as the Earth. This
velocity is measured in kilometers per second.
r: The Population Index, An estimate of the ratio of the number of meteors
in subsequent magnitude classes. Simply stated: the lower the "r" value, the resulting
overall mean magnitude of each shower will be brighter. "r" usually ranges from 2.0 (bright)
to 3.5 (faint).
ZHR: Zenith Hourly Rate, the average maximum number of shower meteors visible
per hour if the radiant is located exactly overhead and the limiting magnitude equals +6.5.
Actual counts rarely reach this figure as the zenith angle of the radiant is usually less and
the limiting magnitude is usually lower. ZHR is a useful tool when comparing the actual observed
rates between individual observers as it sets observing conditions for all to the same standards.
Class: A scale developed by Robert Lunsford to group meteor showers by their intensity:
Class I: the strongest annual showers with ZHR's normally ten or better.
Class II: reliable minor showers with ZHR's normally three or better.
Class III: showers with widely variable rates. They may be strong one year and totally
inactive the next.
Class IV: weak minor showers with ZHR's rarely exceeding three. The study of these
showers is best left to experienced observers who use plotting and angular velocity
estimates to determine shower association. Observers with less experience are urged to
limit their shower associations to showers with a rating of I to III. These showers
are also good targets for video and photographic work.
Moon: the age of the moon in days where 0 is new, 7 is first quarter, 14 is full,
and 21 is last quarter. Meteor activity is best seen in the absence of moonlight so
showers reaching maximum activity when the moon is less than 10 days old or more than 25
are much more favorably observed than those situated closer to the full moon.
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