11 results on '"Jenniskens P"'
Search Results
2. Meteor outbursts from long-period comet dust trails
- Author
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Lyytinen, E. and Jenniskens, P.
- Subjects
Mechanics, Celestial -- Research ,Comets -- Models ,Comets -- Observations ,Mathematical models -- Usage ,Meteors -- Models ,Meteors -- Observations ,Orbits -- Models ,Orbits -- Analysis ,Astronomy ,Earth sciences - Abstract
Long-period comets have narrow one-revolution old dust trails that can cause meteor outbursts when encountered by Earth. To facilitate observing campaigns that will characterize and perhaps help find Earth-threatening, long-period comets from their trace of meteoric debris, we use past accounts of outbursts from 14 different showers to calculate the future dust trail positions near Earth's orbit. We also examine known near-Earth, long-period comets and identify five potential new showers, which can be utilized to learn more about these objects. We demonstrate that it is the one-revolution trail that is responsible for meteor outbursts. A method that calculates in what year these showers are likely to return and at what hour is presented. The calculations improve on earlier approximate methods that used the Sun' s reflex motion to gauge the trail motion relative to Earth's orbit. Keywords: Meteors; Comets-dynamics; Interplanetary dust; Orbits; (Meteor showers)
- Published
- 2003
3. Dust trails of 8P/Tuttle and the unusual outbursts of the Ursid shower
- Author
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Jenniskens, P., Lyytinen, E., de Lignie, M.C., Johannink, C., Jobse, K., Schievink, R., Langbroek, M., Koop, M., Gural, P., Wilson, M.A., Yrjola, I., Suzuki, K, Ogawa, H., and de Groote, P.
- Subjects
Meteoroids -- Research ,Earth -- Orbit ,Astronomy ,Earth sciences - Abstract
We calculate the position of dust trails from comet 8P/Tuttle, in an effort to explain unusual Ursid meteor shower outbursts that were seen when the comet was near aphelion. Comet 8P/Tuttle is a Halley-type comet in a 13.6-year orbit, passing just outside of Earth's orbit. We find that the meteoroids tend to be trapped in the 12:14 mean motion resonance with Jupiter, while the comet librates in a slightly shorter period orbit around the 13:15 resonance. It takes 6 centuries to decrease the perihelion of the meteoroid orbits enough to intersect Earth's orbit, during which time the meteoroids and comet separate in mean anomaly by 6 years, thus explaining the 6-year lag between the comet's return and Ursid outbursts. The resonances also prevent dispersion along the comet orbit and limit viewing to only one year in each return. We identified past dust trail encounters with dust trails from 1392 (Dec. 1945) and 1378 (Dec. 1986) and predicted another outburst on 2000 December 22 at around 7:29 and 8:35 UT, respectively, from dust trails dating to the 1405 and 1392 returns. This event was observed from California using video and photographic techniques. At the same time, five Global-MS-Net stations in Finland, Japan, and Belgium counted meteors using forward meteor scatter. The outburst peaked at 8:06 [+ or -] 07 UT, December 22, at zenith hourly rate ~90 per hour, and the Ursid rates were above half peak intensity during 4.2 h. We find that most Ursid orbits do scatter around the anticipated positions, confirming the link with comet 8P/Tuttle and the epoch of ejection. The 1405 and 1392 dust trails appear to have contributed similar amounts to the activity profile. Some orbits, provide a hint of much older debris being present as well. This work is the strongest evidence yet for the relevance of mean motion resonances in Halley-type comet dust trail evolution.
- Published
- 2002
4. Oxygen Isotope Composition of Almahata Sitta
- Author
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Rumble, D, Zolensky, M. E, Friedrich, J. M, Jenniskens, P, and Shaddad, M. H
- Subjects
Astronomy - Abstract
The name Almahata Sitta is applied collectively to some hundreds of stones that were found in a linear strewn field in the Nubian Desert coincident with the projected Earth-impacting orbit of the Asteroid 2008 TC3. Fragments of the meteorite were collected in December 2008 and March 2009, 2 to 5 months after the asteroid exploded in Earths atmosphere on 7 October 2008.
- Published
- 2010
5. Mission goals of a 1998/1999 Leonid storm Multi-instrument Aircraft Campaign (MAC)
- Author
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Jenniskens, P and Butow, S
- Subjects
Astronomy - Abstract
In November of 1998 (or in 1999 with about equal probability) will be our one chance in a lifetime to anticipate with some certainty the occurrence of a meteor storm. For a period of up to 2 hours, rates are expected to increase above 1 meteor per second for a naked eye observer. At that time, Earth passes through the outer regimes of the dust trail of comet 55P/Tempel-Tuttle. The high meteor flux offers unprecedented precision in characterizing the dust trail in terms of spatial and particle size distributions of dust grains and allows the measurement of composition, morphology and orbits of individual cometary grains relatively soon after ejection from the comet. By using the Earth's atmosphere as a detector for the dust trains, grains are sampled over a wide mass range, from the typical grain size of zodiacal dust (40 - 200 micron) up until the rare boulders that can still be lifted off the comet nucleus.
- Published
- 1998
6. Meteor stream activity. 2: Meteor outbursts
- Author
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Jenniskens, P
- Subjects
Astronomy - Abstract
In the past two centuries, alert amateur and professional meteor astronomers have documented 35 outbursts of 17 individual meteor streams well enough to allow the construction of a homogeneous set of activity curves. These curves add to similar profiles of the annual streams in a previous paper (Paper 1). This paper attempts to define the type and range of phenomena that classify as meteor outbursts from which the following is concluded: Outbursts are associated with the return of the comet to perihelion (near-comet type outbursts), but occur also when the parent comet is far from perihelion and far from the Earth (far-comet type). All outbursts of a given type only, depending on encounter geometry. The activity curves, expressed in terms of Zenith Hourly Rates (ZHR), have a shape that is generally well described by: ZHR = ZHR(sub max) 10(sup(-B (the absolute value of lambda (sub dot in a circle) - lambda (sup max) (sub dot in a circle))). The steepness of the slopes varies from an exponent of B = 7 to B = 220 per degree of solar longitude, with a typical value of B = 30. In addition, most near-comet type outbursts have a broader component underlying the main peak with B approximately 1 - 7.The duration Delta t is approximately 1/B of the main peak is almost independent of location near the comet, while the background component varies considerably in duration and relative intensity from one return to another. The two components in the activity curve are due to two distinct structures in the dust distribution near the parent comet, where the main component can be due to a sheet of dust that emanates from the IRAS dust trail. This brings the total number of distinct structures in meteor streams to four, including the two structures from the annual stream activity in Paper 1.
- Published
- 1995
7. Mostly Dormant Comets and their Disintegration into Meteoroid Streams: A Review.
- Author
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Trigo-Rodríguez, J. M., Rietmeijer, F. J. M., Llorca, J., Janches, D., and Jenniskens, Peter
- Abstract
The history of associating meteor showers with asteroidal-looking objects is long, dating to before the 1983 discovery that 3200 Phaethon moves among the Geminids. Only since the more recent recognition that 2003 EH1 moves among the Quadrantids are we certain that dormant comets are associated with meteoroid streams. Since that time, many orphan streams have found parent bodies among the newly discovered Near Earth Objects. The seven established associations pertain mostly to showers in eccentric or highly inclined orbits. At least 35 other objects are tentatively linked to streams in less inclined orbits that are more difficult to distinguish from those of asteroids. There is mounting evidence that the streams originated from discrete breakup events, rather than long episodes of gradual water vapor outgassing. If all these associations can be confirmed, they represent a significant fraction of all dormant comets that are in near-Earth orbits, suggesting that dormant comets break at least as frequently as the lifetime of the streams. I find that most pertain to NEOs that have not yet fully decoupled from Jupiter. The picture that is emerging is one of rapid disintegration of comets after being captured by Jupiter, and consequently, that objects such as 3200 Phaethon most likely originated from among the most primitive asteroids in the main belt, instead. They too decay mostly by disintegration into comet fragments and meteoroid streams. The disintegration of dormant comets is likely the main source of our meteor showers and the main supply of dust to the zodiacal cloud. [ABSTRACT FROM AUTHOR]
- Published
- 2008
- Full Text
- View/download PDF
8. Characterization of the Meteoroid Spatial Flux Density during the 1999 Leonid Storm.
- Author
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Trigo-Rodríguez, J. M., Rietmeijer, F. J. M., Llorca, J., Janches, D., Gural, Peter S., and Jenniskens, Peter
- Abstract
The November 18, 1999 Leonid storm was rich in meteors and well observed by airborne intensified video cameras aimed low in the sky which enabled enhanced meteor counts over ground-based observations. The two- and three-dimensional distribution of meteoroids was investigated for signs of clustering that could provide evidence of meteoroid fragmentation shortly after lift-off from the parent comet 55P/Tempel-Tuttle, or much later due to space weathering. Analysis of the video tapes yields a refined estimation of the mass ratio during the peak of s = 1.65 and spatial flux density of 0.5 particles/km2 greater than those causing visual magnitude +6.5 during the 5 min centered around the peak of the storm. Furthermore, the projection of the individual trails into three-dimensional Heliocentric coordinates, shows non-homogeneity of the stream on spatial scales from hundreds to thousands of kilometers. [ABSTRACT FROM AUTHOR]
- Published
- 2008
- Full Text
- View/download PDF
9. Predictions for the Aurigid Outburst of 2007 September 1.
- Author
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Trigo-Rodríguez, J. M., Rietmeijer, F. J. M., Llorca, J., Janches, D., Jenniskens, Peter, and Vaubaillon, Jérémie
- Abstract
The September 2007 encounter of Earth with the 1-revolution dust trail of comet C/1911 N1 (Kiess) is the most highly anticipated dust trail crossing of a known long period comet in the next 50 years. The encounter was modeled to predict the expected peak time, duration, and peak rate of the resulting outburst of Aurigid shower meteors. The Aurigids will radiate with a speed of 67 km/s from a radiant at R.A. = 92°, Decl. = +39° (J2000) in the constellation Auriga. The expected peak time is 11:36 ± 20 min UT, 2007 September 1, and the shower is expected to peak at Zenith Hourly Rate = 200/h during a 10-min interval, being above half this value during 25 min. The meteor outburst will be visible by the naked eye from locations in Mexico, the Western provinces of Canada, and the Western United States, including Hawaii and Alaska. A concerted observing campaign is being organized. Added in proof: first impression of the shower. [ABSTRACT FROM AUTHOR]
- Published
- 2008
- Full Text
- View/download PDF
10. The IAU Meteor Shower Nomenclature Rules.
- Author
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Trigo-Rodríguez, J. M., Rietmeijer, F. J. M., Llorca, J., Janches, D., and Jenniskens, Peter
- Abstract
The International Astronomical Union at its 2006 General Assembly in Prague has adopted a set of rules for meteor shower nomenclature, a working list with designated names (with IAU numbers and three-letter codes), and established a Task Group for Meteor Shower Nomenclature in Commission 22 (Meteors and Interplanetary Dust) to help define which meteor showers exist from well defined groups of meteoroids from a single parent body. [ABSTRACT FROM AUTHOR]
- Published
- 2008
- Full Text
- View/download PDF
11. Meteor induced chemistry, ablation products, and dust in the middle and upper atmosphere from optical spectroscopy of meteors
- Author
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Jenniskens, P.
- Subjects
- *
METEORS , *ASTRONOMY , *NATURAL disasters , *ATMOSPHERE - Abstract
The recent intense Leonid meteor storms have seen a rejuvenation of optical meteor studies, including the first application of cooled CCD technologies and the first large-scale use of intensified slit-less video spectrographs. The Leonid Multi-Instrument Aircraft Campaign has provided a wealth of diverse new data. This paper is an initial attempt to ask what the myriad of Leonid observations have taught us, by bringing the observations and early modeling efforts together, and by presenting a `grand vision'' of the interaction of fast meteoroids with the atmosphere. An overview is given of the physical conditions in meteors, their products, and their influence on the Earth''s atmosphere. [Copyright &y& Elsevier]
- Published
- 2004
- Full Text
- View/download PDF
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