2001
DOI: 10.1007/978-3-642-56428-4_5
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Discoveries from Observations and Modeling of the 1998/99 Leonids

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Cited by 10 publications
(12 citation statements)
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“…The recent Leonid meteor storm of 1999 November 18 and a second outburst half a day later were caused by ejecta from Comet 55P/Tempel-Tuttle released at the returns of 1899 and 1866, respectively (Kondrat'eva and Reznikov 1985, Lyytinen 1999, McNaught and Asher 1999. And three calculated encounters with dust from the 1932, 1733, and 1866 returns were observed much as predicted (Jenniskens 2001a). Similar identifications for short-period comets have been made for outbursts of the June Bootids, Beilids, and Draconids (Reznikov 1983).…”
Section: Introductionsupporting
confidence: 78%
“…The recent Leonid meteor storm of 1999 November 18 and a second outburst half a day later were caused by ejecta from Comet 55P/Tempel-Tuttle released at the returns of 1899 and 1866, respectively (Kondrat'eva and Reznikov 1985, Lyytinen 1999, McNaught and Asher 1999. And three calculated encounters with dust from the 1932, 1733, and 1866 returns were observed much as predicted (Jenniskens 2001a). Similar identifications for short-period comets have been made for outbursts of the June Bootids, Beilids, and Draconids (Reznikov 1983).…”
Section: Introductionsupporting
confidence: 78%
“…To make the resulting trajectory solution averages per shower have realistic weighted geometries given the station locations, activity profiles for each shower are required. The activity profile of simulated meteor showers is defined by the solar longitude of the peak λ max and the slope of the activity profile B, where the activity is approximated as Z HR = Z HR max 10 −B |λ −λ ma x | following Jenniskens (1994).…”
Section: Simulating Radiants and Activitymentioning
confidence: 99%
“…These were modified from the original so that they are centered around the peak solar longitude while the radiant spread was computed directly from data provided in Spurnỳ et al (2017). λ ma x is the solar longitude of the peak (degrees), B is the solar longitude slope of the rising portion of the activity profile following the procedure of Jenniskens (1994), α is the mean geocentric right ascension, ∆α is the radiant drift (degree on the sky per degree of solar longitude), α σ is the standard deviation in R.A., δ is the mean geocentric declination, ∆δ is the declination radiant drift, δ σ is the standard deviation of the declination, V g is the mean geocentric velocity in km s −1 , ∆V g is the change in geocentric velocity per degree of solar longitude, and V gσ is the standard deviation of the geocentric velocity.…”
Section: Resultsmentioning
confidence: 99%
“…As both the Geminids and Perseids are older showers, we do not expect the physical radiant dispersion to be as compact as the Draconids, thus for simulation purposes we have used observed values for these quantities provided in Jenniskens et al (2016) and Jenniskens (1994). We summarize the modeling parameters adopted of the simulated meteors showers in table 2 and the physical properties of shower meteoroids used in the ablation modeling in table 3.…”
Section: Dynamical Modelling Of the 2011 Draconid Outburstmentioning
confidence: 99%