Analysis of Meteoritic Activity in the Vth-Xvth Centuries Using an Extended Survey of European Medieval Sources
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Teachers' Guide to Meteor Showers Leonids Meteor Shower
Education and Public Outreach Look Up! Event Guides Teachers’ Guide to Meteor Showers Leonids Meteor Shower - November 17/18, 2015 What is a meteor shower? A meteor shower is a predictable celestial event in which a relatively large number of meteors streak across the sky on a given night or series of nights. Meteor showers appear to originate from one point (called the radiant) in the night sky, often a constellation. Meteor showers get their name from the constellation from which they appear to originate. Meteor showers are caused by debris called meteoroids entering Earth’s atmosphere at extremely high speeds. This debris usually comes from comets that intersect Earth’s orbit. As Earth orbits the Sun, it collides with the debris left by passing comets and the result are meteors streaking through Earth’s atmosphere. Most meteors are smaller than a grain of sand, so almost all of them disintegrate before having a chance to hit the ground. In 2015, the annual Leonid meteor shower will peak the night of November 17/18. The Leonids are so named because they appear to originate from the constellation of Leo (the lion). The debris responsible for the Leonids comes from the comet Tempel- Tuttle. It is possible to view about 20 meteors in one hour at the peak of the Leonids meteor shower. Upcoming Events Find information and resources about upcoming celestial events and NASA mission milestones to share with your students at http://www.lpi.usra.edu/education/look_up. Meteor Showers/Comets in Your Classroom! Use the resources below to enable your students to explore meteor showers. -
Meteor Showers' Activity and Forecasting
Meteoroids 2007 – Barcelona, June 11-15 About the cover: The recent fall of the Villalbeto de la Peña meteorite on January 4, 2004 (Spain) is one of the best documented in history for which atmospheric and orbital trajectory, strewn field area, and recovery circumstances have been described in detail. Photometric and seismic measurements together with radioisotopic analysis of several recovered specimens suggest an original mass of about 760 kg. About fifty specimens were recovered from a strewn field of nearly 100 km2. Villalbeto de la Peña is a moderately shocked (S4) equilibrated ordinary chondrite (L6) with a cosmic-ray-exposure age of 48±5 Ma. The chemistry and mineralogy of this genuine meteorite has been characterized in detail by bulk chemical analysis, electron microprobe, electron microscopy, magnetism, porosimetry, X-ray diffraction, infrared, Raman, and 57Mössbauer spectroscopies. The picture of the fireball was taken by M.M. Ruiz and was awarded by the contest organized by the Spanish Fireball Network (SPMN) for the best photograph of the event. The Moon is also visible for comparison. The picture of the meteorite was taken as it was found by the SPMN recovery team few days after the fall. 2 Meteoroids 2007 – Barcelona, June 11-15 FINAL PROGRAM Monday, June 11 Auditorium conference room 9h00-9h50 Reception 9h50-10h00 Opening event Session 1: Observational Techniques and Meteor Detection Programs Morning session Session chairs: J. Borovicka and W. Edwards 10h00-10h30 Pavel Spurny (Ondrejov Observatory, Czech Republic) et al. “Fireball observations in Central Europe and Western Australia – instruments, methods and results” (invited) 10h30-10h45 Josep M. -
The Leonid Meteor Shower: Historical Visual Observations
Icarus 138, 287–308 (1999) Article ID icar.1998.6074, available online at http://www.idealibrary.com on The Leonid Meteor Shower: Historical Visual Observations P. Brown Department of Physics and Astronomy, University of Western Ontario, London, Ontario, N6A 3K7, Canada E-mail: [email protected] Received July 20, 1998; revised December 10, 1998 of past showers, independent of the many secondary accounts The original visual accounts of the Leonids from 1799 to 1997 which appear in the literature, in an effort to better understand are examined and the times and magnitude of peak activity are the stream’s past activity, its formation, and as a way to predict established for 32 Leonid returns during this two-century interval. what may happen in the years from 1999 onwards. In addition, Previous secondary accounts of many of these returns are shown this revised set of historical Leonid data provides a set of obser- to differ from the information contained in the original accounts vations reduced in a common manner, which any model of the due to misinterpretations, typographical errors, and unsupported stream must be able to explain and to which others can easily assumptions. The strongest Leonid storms are shown to follow a examine and apply their own corrections. Gaussian activity profile and to occur after the perihelion passage In this work, we examine in detail available original records and nodal longitude of 55P/Tempel–Tuttle. The relationship be- tween the Gaussian width of the strongest returns and their peak of the Leonids for modern returns of the shower (here defined activity is established, and the particle density/stream width rela- to be post-1799). -
Meteor Shower Detection with Density-Based Clustering
Meteor Shower Detection with Density-Based Clustering Glenn Sugar1*, Althea Moorhead2, Peter Brown3, and William Cooke2 1Department of Aeronautics and Astronautics, Stanford University, Stanford, CA 94305 2NASA Meteoroid Environment Office, Marshall Space Flight Center, Huntsville, AL, 35812 3Department of Physics and Astronomy, The University of Western Ontario, London N6A3K7, Canada *Corresponding author, E-mail: [email protected] Abstract We present a new method to detect meteor showers using the Density-Based Spatial Clustering of Applications with Noise algorithm (DBSCAN; Ester et al. 1996). DBSCAN is a modern cluster detection algorithm that is well suited to the problem of extracting meteor showers from all-sky camera data because of its ability to efficiently extract clusters of different shapes and sizes from large datasets. We apply this shower detection algorithm on a dataset that contains 25,885 meteor trajectories and orbits obtained from the NASA All-Sky Fireball Network and the Southern Ontario Meteor Network (SOMN). Using a distance metric based on solar longitude, geocentric velocity, and Sun-centered ecliptic radiant, we find 25 strong cluster detections and 6 weak detections in the data, all of which are good matches to known showers. We include measurement errors in our analysis to quantify the reliability of cluster occurrence and the probability that each meteor belongs to a given cluster. We validate our method through false positive/negative analysis and with a comparison to an established shower detection algorithm. 1. Introduction A meteor shower and its stream is implicitly defined to be a group of meteoroids moving in similar orbits sharing a common parentage. -
Meteor Showers # 11.Pptx
20-05-31 Meteor Showers Adolf Vollmy Sources of Meteors • Comets • Asteroids • Reentering debris C/2019 Y4 Atlas Brett Hardy 1 20-05-31 Terminology • Meteoroid • Meteor • Meteorite • Fireball • Bolide • Sporadic • Meteor Shower • Meteor Storm Meteors in Our Atmosphere • Mesosphere • Atmospheric heating • Radiant • Zenithal Hourly Rate (ZHR) 2 20-05-31 Equipment Lounge chair Blanket or sleeping bag Hot beverage Bug repellant - ThermaCELL Camera & tripod Tracking Viewing Considerations • Preparation ! Locate constellation ! Take a nap and set alarm ! Practice photography • Location: dark & unobstructed • Time: midnight to dawn https://earthsky.org/astronomy- essentials/earthskys-meteor-shower- guide https://www.amsmeteors.org/meteor- showers/meteor-shower-calendar/ • Where to look: 50° up & 45-60° from radiant • Challenges: fatigue, cold, insects, Moon • Recording observations ! Sky map, pen, red light & clipboard ! Time, position & location ! Recording device & time piece • Binoculars Getty 3 20-05-31 Meteor Showers • 112 confirmed meteor showers • 695 awaiting confirmation • Naming Convention ! C/2019 Y4 (Atlas) ! (3200) Phaethon June Tau Herculids (m) Parent body: 73P/Schwassmann-Wachmann Peak: June 2 – ZHR = 3 Slow moving – 15 km/s Moon: Waning Gibbous June Bootids (m) Parent body: 7p/Pons-Winnecke Peak: June 27– ZHR = variable Slow moving – 14 km/s Moon: Waxing Crescent Perseid by Brian Colville 4 20-05-31 July Delta Aquarids Parent body: 96P/Machholz Peak: July 28 – ZHR = 20 Intermediate moving – 41 km/s Moon: Waxing Gibbous Alpha -
3D/Biela and the Andromedids: Fragmenting Versus Sublimating Comets P
The Astronomical Journal, 134:1037 Y 1045, 2007 September # 2007. The American Astronomical Society. All rights reserved. Printed in U.S.A. 3D/BIELA AND THE ANDROMEDIDS: FRAGMENTING VERSUS SUBLIMATING COMETS P. Jenniskens1 and J. Vaubaillon2 Received 2007 January 3; accepted 2007 April 22 ABSTRACT Comet 3D/Biela broke up in 1842/1843 and continued to disintegrate in the returns of 1846 and 1852. When meteor storms were observed in November of 1872 and 1885, it was surmised that those showers were the debris from that breakup. This could have come from one of two sources: (1) the initial separation of fragments near aphelion or (2) the continued disintegration of the fragments afterward. Alternatively, the meteoroids could simply have come from water vapor drag when the fragments approached perihelion (option 3). We investigated the source of the Andromedid storms by calculating the dynamical evolution of dust ejected in a normal manner by water vapor drag in the returns from 1703 to 1866, assuming that the comet would have remained similarly active over each return. In addition, we simulated the isotropic ejection of dust during the initial fragmentation event at aphelion in December of 1842. We conclude that option 2 is the most likely source of meteoroids encountered during the 1872 and 1885 storms, but this accounts for only a relatively small amount of mass lost in a typical comet breakup. Key words: comets: individual (3D/Biela) — meteors, meteoroids — minor planets, asteroids 1. INTRODUCTION 2. THE COMET AND ITS SHOWER Ever since Whipple (1951) showed that water vapor can ac- 2.1. -
Five Wild Years Reminiscences of the Leonids Experience 1998 – 2002
Proceedings IMC Bollmannsruh 2003 29 Five wild years Reminiscences of the Leonids experience 1998 – 2002 Daniel Fischer K¨onigswinter, Germany Abstract This is not a scientific review of the surprises, discoveries and sensations the Leonids brought from 1998 to 2002, but a look back by one observer (and science writer) who often witnessed first-hand what went on in the sky — and also how science finally got its grip on the elusive and striking phenomenon of meteor storms. It was a truly an experience with a deep impact (no pun intended) that is not likely to be repeated... I admit it: before about ten years ago I had considered meteor observing, especially with your own eye, as one of the most useless branches of (amateur) astronomy, with no serious data reduction possible and dubious results. This was not true, at least at that time, of course (see Roggemans, 2004), but the progress made by the IMO had not been widely known to the outside world. Not in- terested at all in systematic meteor watching, I was struck by the idea of meteor storms nonetheless: I had read a lot about the fabulous Leonids storm of 1966 and eagerly devoured two big reviews of meteor storms in British journals. Beech et al (1995) had described these rare phenomena as both spectacular and little understood, while Mason (1995) predicted — using a crude model — storms of the Leonids with ZHRs around 5000 in 1998 and 1999. Would it be worth chasing after those possible storms? I was already travelling a lot for astronomy’s sake, both in the quest for eclipses (1983, 1988, 1990, 1991, 1992, 1994, 1995 and so on) and comets (Halley in 1986), but for meteors? Then again, Brad Schaefer, the American astronomer famous for his professional work on astronomy with the naked eye, had told me in 1988 that for him one meteor storm would be “worth ten eclipses”. -
Leonid Meteor Shower Peaks Wednesday 12 November 2010
Leonid Meteor Shower Peaks Wednesday 12 November 2010 clumps this year, viewers could see hundreds of meteors per hour at the shower's peak. If Earth simply passes through the normal part of the comet's debris trail, the number of meteors visible will be much lower. For your best view, get away from city lights. Look for state or city parks or other safe, dark sites. Lie on a blanket or reclining chair to get a full-sky view. If you can see all of the stars in the Little Dipper, you have good dark-adapted vision. More information: stardate.org/magazine The Leonid meteor shower best viewing this year will be in the two to three hours before dawn on Provided by University of Texas at Austin Nov. 17 and 18, according to the editors of StarDate magazine. There is always some uncertainty in the number of meteors the Leonid shower will produce, but viewers should expect to see at least 20 meteors per hour if they have clear skies. The nearly full moon will set several hours before dawn, and therefore not wash out any meteors in the hours immediately before dawn. High-resolution images and high-definition video animation of the Leonid meteor shower are available online at StarDate's Media Center. There, you can also sign up to receive advance e-mail notices of future skywatching events. Leonid meteors appear to fall from the constellation Leo, the lion, but they are not associated with it. They are leftover debris from comet Tempel-Tuttle. As the comet orbits the sun, it leaves a trail of debris. -
Librarians' Guide to Meteor Showers Leonids Meteor Shower
Education and Public Outreach Look Up! Event Guides Librarians’ Guide to Meteor Showers Leonids Meteor Shower - November 17/18, 2015 What is a meteor shower? A meteor shower is a predictable celestial event in which a relatively large number of meteors streak across the sky on a given night or series of nights. Meteor showers appear to originate from one point (called the radiant) in the night sky, often a constellation. Meteor showers get their name from the constellation from which they appear to originate. Meteor showers are caused by debris called meteoroids entering Earth’s atmosphere at extremely high speeds. This debris usually comes from comets that intersect Earth’s orbit. As Earth orbits the Sun, it collides with the debris left by passing comets and the result are meteors streaking through Earth’s atmosphere. Most meteors are smaller than a grain of sand, so almost all of them disintegrate before having a chance to hit the ground. In 2015, the annual Leonid meteor shower will peak the night of November 17/18. The Leonids are so named because they appear to originate from the constellation of Leo (the lion). The debris responsible for the Leonids comes from the comet Tempel- Tuttle. It is possible to view about 20 meteors in one hour at the peak of the Leonids meteor shower. Upcoming Events Find information and resources about upcoming celestial events and NASA mission milestones to share with your child at http://www.lpi.usra.edu/education/look_up. night sky http://www.lpi.usra.edu/education/look_up @earthskyscience Meteor Showers/Comets in Your Library! Use the resources below to create a program for your patrons to explore meteor showers. -
2020 Meteor Shower Calendar Edited by J¨Urgen Rendtel 1
IMO INFO(2-19) 1 International Meteor Organization 2020 Meteor Shower Calendar edited by J¨urgen Rendtel 1 1 Introduction This is the thirtieth edition of the International Meteor Organization (IMO) Meteor Shower Calendar, a series which was started by Alastair McBeath. Over all the years, we want to draw the attention of observers to both regularly returning meteor showers and to events which may be possible according to model calculations. We may experience additional peaks and/or enhanced rates but also the observational evidence of no rate or density enhancement. The position of peaks constitutes further important information. All data may help to improve our knowledge about the numerous effects occurring between the meteoroid release from their parent object and the currently observable structure of the related streams. Hopefully, the Calendar continues to be a useful tool to plan your meteor observing activities during periods of high rates or periods of specific interest for projects or open issues which need good coverage and attention. Video meteor camera networks are collecting data throughout the year. Nevertheless, visual observations comprise an important data sample for many showers. Because visual observers are more affected by moonlit skies than video cameras, we consider the moonlight circumstances when describing the visibility of meteor showers. For the three strongest annual shower peaks in 2020 we find the first quarter Moon for the Quadrantids, a waning crescent Moon for the Perseids and new Moon for the Geminids. Conditions for the maxima of other well-known showers are good: the Lyrids are centred around new Moon, the Draconids occur close to the last quarter Moon and the Orionids as well as the Leonids see a crescent only in the evenings. -
Asteroid-Meteoroid Complexes Backwards in Time, in of What Produces the Meteoroid Streams? Suggested Alter- Order to Learn How They Form
LIST OF CONTRIBUTORS toshihiro kasuga Public Relations Center National Astronomical Observatory of Japan 2-21-1 Osawa Mitaka Tokyo 181-8588 Japan Department of Physics Kyoto Sangyo University Motoyama, Kamigamo Kita-ku Kyoto 603-8555 Japan david jewitt Earth, Planetary and Space Sciences / Physics and Astron- omy University of California at Los Angeles 595 Charles Young Drive East Los Angeles CA 90095-1567 USA arXiv:2010.16079v1 [astro-ph.EP] 30 Oct 2020 1 8 Asteroid–Meteoroid Complexes TOSHIHIRO KASUGA AND DAVID JEWITT 8.1 Introduction are comets is comparatively old, having been suggested by Whipple (1939a,b, 1940) (see also Olivier, 1925; Hoffmeis- Physical disintegration of asteroids and comets leads to the ter, 1937). The Geminid meteoroid stream (GEM/4, from production of orbit-hugging debris streams. In many cases, Jopek and Jenniskens, 2011)1 and asteroid 3200 Phaethon the mechanisms underlying disintegration are uncharacter- are probably the best-known examples (Whipple, 1983). In ized, or even unknown. Therefore, considerable scientific in- such cases, it appears unlikely that ice sublimation drives terest lies in tracing the physical and dynamical properties the expulsion of solid matter, raising the general question of the asteroid-meteoroid complexes backwards in time, in of what produces the meteoroid streams? Suggested alter- order to learn how they form. native triggers include thermal stress, rotational instability Small solar system bodies offer the opportunity to under- and collisions (impacts) by secondary bodies (Jewitt, 2012; stand the origin and evolution of the planetary system. They Jewitt et al., 2015). Any of the above, if sufficiently vio- include the comets and asteroids, as well as the mostly un- lent or prolonged, could lead to the production of a debris seen objects in the much more distant Kuiper belt and Oort trail that would, if it crossed Earth’s orbit, be classified as cloud reservoirs. -
Lunar Meteor Schedule and Observing Plan for 2021
Lunar Meteor Schedule and Observing Plan for 2021 This form outlines the plan to monitor the moon on a regular basis both inside and outside normal annual showers. Each month, for a total of up to 14 days per month, we are coordinating observations of the Earthshine portion of the moon for background (including the minor showers when they fall during this time) meteor impact flux. A typical run of observations starts three days after New Moon and continues until two days past First Quarter. The run resumes two days before Last Quarter and continues until three days prior to New Moon. The actual interval will depend on the lunar elevation and elongation as well as the ability of the observer to control stray light in one’s system. Shower Activity Maximum Radiant V∞ r ZHR Date λ⊙ α δ km/s Antihelion Source Mar-Apr, late Dec 10 – Sep 10 Varies Varies 30 3.0 4 (ANT) May, late June Quadrantids (010 QUA) Dec 28 - Jan 12 Jan 03 283.15° 230° +49° 41 2.1 110 γ-Ursae Minorids (404 Jan 10 - Jan 22 Jan 19 298° 228° +67° 31 3.0 3 GUM) α-Centaurids (102 ACE) Jan 31 - Feb 20 Feb 08 319.2° 210° -59° 58 2.0 6 γ-Normids (118 GNO) Feb 25 - Mar 28 Mar 14 354° 239° -50° 56 2.4 6 Lyrids (006 LYR) Apr 14 - Apr 30 Apr 22 32.32° 271° +34° 49 2.1 18 π-Puppids (137 PPU) Apr 15 – Apr 28 Apr 23 33.5° 110° -45° 18 2.0 Var η-Aquariids (031 ETA) Apr 19 - May 28 May 05 45.5° 338° -01° 66 2.4 50 η-Lyrids (145 ELY) May 03 - May 14 May 08 48.0° 287° +44° 43 3.0 3 June Bootids (170 JBO) Jun 22 - Jul 02 Jun 27 95.7° 224° +48° 18 2.2 Var Piscis Austr.