Determination of Design Meteoroid Mass for a Sporadic and Stream Meteoroid Environment
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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. -
17. a Working List of Meteor Streams
PRECEDING PAGE BLANK NOT FILMED. 17. A Working List of Meteor Streams ALLAN F. COOK Smithsonian Astrophysical Observatory Cambridge, Massachusetts HIS WORKING LIST which starts on the next is convinced do exist. It is perhaps still too corn- page has been compiled from the following prehensive in that there arc six streams with sources: activity near the threshold of detection by pho- tography not related to any known comet and (1) A selection by myself (Cook, 1973) from not sho_m to be active for as long as a decade. a list by Lindblad (1971a), which he found Unless activity can be confirmed in earlier or from a computer search among 2401 orbits of later years or unless an associated comet ap- meteors photographed by the Harvard Super- pears, these streams should probably be dropped Sehmidt cameras in New Mexico (McCrosky and from a later version of this list. The author will Posen, 1961) be much more receptive to suggestions for dele- (2) Five additional radiants found by tions from this list than he will be to suggestions McCrosky and Posen (1959) by a visual search for additions I;o it. Clear evidence that the thresh- among the radiants and velocities of the same old for visual detection of a stream has been 2401 meteors passed (as in the case of the June Lyrids) should (3) A further visual search among these qualify it for permanent inclusion. radiants and velocities by Cook, Lindblad, A comment on the matching sets of orbits is Marsden, McCrosky, and Posen (1973) in order. It is the directions of perihelion that (4) A computer search -
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. -
Long Grazing and Slow Trail Fireball Over Portugal Spectra of Slow
e-Zine for meteor observers meteornews.org Vol. 4 / January 2017 A bright fireball photographed by four stations of the Danish Meteor network on December 25 at 2:11 UT. Long grazing and slow trail OCT outburst model comparisons fireball over Portugal in the years 2005, 2016, 2017 Spectra of slow bolides Worldwide radio results The PRO-AM Lunar Impact autumn 2016 project Exoss Fireball events 2016 – 4 eMeteorNews Contents Spectra of slow bolides Jakub Koukal ........................................................................................................................................... 117 Visual observing reports Paul Jones ............................................................................................................................................... 123 Fireball events Compiled by Paul Roggemans ................................................................................................................ 130 CAMS BeNeLux September results Carl Johannink ........................................................................................................................................ 134 October Camelopardalis outburst model comparisons in the years 2005, 2016, 2017 Esko Lyytinen .......................................................................................................................................... 135 CAMS Benelux contributed 4 OCT orbits Carl Johannink ....................................................................................................................................... -
Smithsonian Contributions Astrophysics
SMITHSONIAN CONTRIBUTIONS to ASTROPHYSICS Number 14 Discrete Levels off Beginning Height off Meteors in Streams By A. F. Cook Number 15 Yet Another Stream Search Among 2401 Photographic Meteors By A. F. Cook, B.-A. Lindblad, B. G. Marsden, R. E. McCrosky, and A. Posen Smithsonian Institution Astrophysical Observatory Smithsonian Institution Press SMITHSONIAN CONTRIBUTIONS TO ASTROPHYSICS NUMBER 14 A. F. cook Discrete Levels of Beginning Height of Meteors in Streams SMITHSONIAN INSTITUTION PRESS CITY OF WASHINGTON 1973 Publications of the Smithsonian Institution Astrophysical Observatory This series, Smithsonian Contributions to Astrophysics, was inaugurated in 1956 to provide a proper communication for the results of research conducted at the Astrophysical Observatory of the Smithsonian Institution. Its purpose is the "increase and diffusion of knowledge" in the field of astrophysics, with particular emphasis on problems of the sun, the earth, and the solar system. Its pages are open to a limited number of papers by other investigators with whom we have common interests. Another series, Annals of the Astrophysical Observatory, was started in 1900 by the Observa- tory's first director, Samuel P. Langley, and was published about every ten years. These quarto volumes, some of which are still available, record the history of the Observatory's researches and activities. The last volume (vol. 7) appeared in 1954. Many technical papers and volumes emanating from the Astrophysical Observatory have appeared in the Smithsonian Miscellaneous Collections. Among these are Smithsonian Physical Tables, Smithsonian Meteorological Tables, and World Weather Records. Additional information concerning these publications can be obtained from the Smithsonian Institution Press, Smithsonian Institution, Washington, D.C. -
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. -
Radio Echo Observations of Meteors in the Southern Hemisphere
RADIO ECHO OBSERVATIONS OF METEORS IN THE SOUTHERN HEMISPHERE By A. A. WEISS* [Manuscript received September 20, 1954] Summary The results of a radio survey of meteor activity at Adelaide are presented. The radiants and activities of six major meteor showers (Geminids, day-time Arietids, ~-Perseids, a-Aquarids, Corona Australids, Orionids) have been measured by methods which are described, and the mass distributions in three of these showers are discussed. Seasonal and diurnal variations in the background activity of sporadic meteors are examined in relation to the radiation patterns of the aerial systems_ Height distribut.ions for meteors of three showers (Geminids, day-time Arietids, ~-Perseids) are given. Diurnal variations in the height distribution of sporadic meteors do not conform to those expected from the motion of the apex of the Earth's way. I. INTRODUCTION The successful application, at the Jodrell Bank Experimental Station of the University of Manchester, of radio echo techniques to the continuous monitoring of meteor activity in the northern hemisphere, prompted the initiation ()f a complementary survey in the southern hemisphere. Up to the time of (lommencement of this survey lists of southern hemisphere visual observations had been published by McIntosh and by Hoffmeister, and McIntosh (1935) had compiled" An Index to Southern Meteor Showers" which lists 320 radiants visible at mid-southern latitudes. These visual observations have since been supplemented by radio echo observations on the a-Aquarid shower by Hawkins and Almond (1952) and by Lindblad (1952). Although it is certain that all major southern night-time showers have been detected by the visual workers, the cover in the months September to March is not altogether satisfactory (McIntosh 1935). -
Analysis of Historical Meteor and Meteor Shower Records: Korea, China and Japan
Highlights of Astronomy, Volume 16 XXVIIIth IAU General Assembly, August 2012 c International Astronomical Union 2015 T. Montmerle, ed. doi:10.1017/S1743921314005079 Analysis of Historical Meteor and Meteor shower Records: Korea, China and Japan Hong-Jin Yang1, Changbom Park2 and Myeong-Gu Park3 1 Korea Astronomy and Space Science Institute, Korea email: [email protected] 2 Korea Institute for Advanced Study, Korea 3 Kyungpook National University, Korea Abstract. We have compiled and analyzed historical meter and meteor shower records in Ko- rean, Chinese, and Japanese chronicles. We have confirmed the peaks of Perseids and an excess due to the mixture of Orionids, north-Taurids, or Leonids through the Monte-Carlo test from the Korean records. The peaks persist for almostonethousandyears.Wehavealsoanalyzed seasonal variation of sporadic meteors from Korean records. Major features in Chinese meteor shower records are quite consistent with those of Korean records, particularly for the last millen- nium. Japanese records also show Perseids feature and Orionids/north-Taurids/Leonids feature, although they are less prominent compared to those of Korean or Chinese records. Keywords. meteors, meteor showers, historical records We have compiled and analyzed the meteor and meteor shower records in official Korean history books (Kim et al. 1145; Kim et al. 1451; Chunchugwan 1392-1863) dating from 57 B.C. to A.D. 1910, covering the Three Kingdoms period (from 57 B.C. to A.D. 918), Goryeo dynasty (from A.D. 918 to A.D. 1392), and Joseon dynasty (from A.D. 1392 to A.D. 1910). The books contain only a small number of meteor shower records in contrast to abundant meteor records. -
Spectra and Physical Properties of Taurid Meteoroids
Spectra and physical properties of Taurid meteoroids Pavol Matloviˇca, Juraj T´otha, Regina Rudawskab, Leonard Kornoˇsa aFaculty of Mathematics, Physics and Informatics, Comenius University, Bratislava, Slovakia bESA European Space Research and Technology Centre, Noordwijk, Netherlands Abstract Taurids are an extensive stream of particles produced by comet 2P/Encke, which can be observed mainly in October and November as a series of me- teor showers rich in bright fireballs. Several near-Earth asteroids have also been linked with the meteoroid complex, and recently the orbits of two car- bonaceous meteorites were proposed to be related to the stream, raising interesting questions about the origin of the complex and the composition of 2P/Encke. Our aim is to investigate the nature and diversity of Taurid mete- oroids by studying their spectral, orbital, and physical properties determined from video meteor observations. Here we analyze 33 Taurid meteor spectra captured during the predicted outburst in November 2015 by stations in Slo- vakia and Chile, including 14 multi-station observations for which the orbital elements, material strength parameters, dynamic pressures, and mineralog- ical densities were determined. It was found that while orbits of the 2015 Taurids show similarities with several associated asteroids, the obtained spec- tral and physical characteristics point towards cometary origin with highly heterogeneous content. Observed spectra exhibited large dispersion of iron content and significant Na intensity in all cases. The determined material strengths are typically cometary in the KB classification, while PE criterion is on average close to values characteristic for carbonaceous bodies. The studied meteoroids were found to break up under low dynamic pressures of 0.02 - 0.10 MPa, and were characterized by low mineralogical densities of 1.3 arXiv:1704.06482v1 [astro-ph.EP] 21 Apr 2017 - 2.5 g cm-3. -
The Student Voice October 29, 2013
Six Mile Post Vol. 43, #2 www.sixmilepost.com The Student Voice October 29, 2013 Lucy Njuguna embraces the outdoors while studying on the Cartersville campus. See more fall photos on page 8. Photo by Tatiana Smithson Student balances Charger Café Men’s and Women’s family and class not up to par Basketball Preview See page 5. See page 12. See page 16. Georgia Highlands College - Rome, Georgia Page 2, SMP, Oct. 29, 2013 News November to bring excitement to the night sky By Thomas Dobson Earth well into January Staff Writer 2014, no telescope required. The Floyd campus obser- This coming November vatory has in its inventory will be an eventful month a 16-inch Meade telescope for stargazers. and a 12-inch Newtonian This promises to bring telescope, along with many people from the Rome area smaller telescopes, perfect to Georgia Highlands Floyd for viewing distant objects campus, the home of the at night even on a full moon. Bishop Observatory, one of According to Mark Per- only two observatories in grem, assistant professor Rome area, the other being of astronomy, the Bishop Berry College’s Pew Obser- Observatory is not open vatory. to the public, but appoint- Three separate meteor ments can be made for other showers are predicted to groups not affiliated with peak in November, but the Georgia Highlands to use star everyone is expecting the facility, weather permit- to steal the show is Comet ting. Two separate groups ISON. have already signed up to The meteor showers will use the observatory in the be the South Taurids and the coming months. -
The Geologists' Frontier
Vol. 30, No. 8 AufJlIt 1968 STATE OF OREGON DEPARTMENT Of GEOLOGY AND MINERAL INDUSTRIES State of Oregon Department of Geology The ORE BI N and Mineral Industries Volume30, No.8 1069 State Office Bldg. August 1968 Portland Oregon 97201 FIREBALLS. METEORITES. AND METEOR SHOWERS By EnNin F. Lange Professor of General Science, Portland State College About once each year a bri lIiant and newsworthy fireball* passes across the Northwest skies. The phenomenon is visible evidence that a meteorite is reach i ng the earth from outer space. More than 40 percent of the earth's known meteorites have been recovered at the terminus of the fireball's flight. Such meteorites are known as "falls" as distinguished from "finds," which are old meteorites recovered from the earth's crust and not seen falling. To date only two falls have been noted in the entire Pacific North west. The more recent occurred on Sunday morning, July 2, 1939, when a spectacular fireball or meteor passed over Portland just before 8:00 a.m. Somewhat to the east of Portland the meteor exploded, causing many people to awaken from their Sunday morning slumbers as buildings shook, and dishes and windows rattled. No damage was reported. Several climbers on Mount Hood and Mount Adams reported seei ng the unusual event. The fireball immediately became known as the Portland meteor and stories about it appeared in newspapers from coast to coast. For two days th e pre-Fourth of July fireworks made front-page news in the local newspapers. J. Hugh Pruett, astronomer at the University of Oregon and Pacific director of the American Meteor Society, in an attempt to find the meteor ite which had caused such excitement, appealed to all witnesses of the event to report to him their observations. -
Occurrence and Altitude of the Non-Specular Long-Lived Meteor Trails During Meteor Showers at High Latitudes
EGU2020-1543 https://doi.org/10.5194/egusphere-egu2020-1543 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Occurrence and altitude of the non-specular long-lived meteor trails during meteor showers at high latitudes Alexander Kozlovsky1, Renata Lukianova2, and Mark Lester3 1University of Oulu, Sodankyla Geophysical Observatory, Sodankyla, Finland ([email protected]) 2Space Research Institute, Moscow, Russia 3Department of Physics and Astronomy, University of Leicester, Leicester, UK Meteoroids entering the Earth’s atmosphere produce ionized trails, which are detectable by radio sounding. Majority of such radar detections are the echoes from cylindrical ionized trails, which occur if the radar beam is perpendicular to the trail, i.e., the reflection is specular. Typically such echoes detected by VHF radars last less than one second. However, sometimes meteor radars (MR) observe unusually long-lived meteor echoes and these echoes are non-specular (LLNS echoes). The LLNS echoes last up to several tens of seconds and show highly variable amplitude of the radar return. The LLNS echoes are received from the non-field-aligned irregularities of ionization generated along trails of bright meteors and it is believed that key role in their generation belongs to the aerosol particles arising due to fragmentation and burning of large meteoroids. The occurrence and height distributions of LLNS are studied using MR observations at Sodankylä Geophysical Observatory (SGO, 67° 22' N, 26° 38' E, Finland) during 2008-2019. Two parameters are analyzed: the percentage and height distribution of LLNS echoes. These LLNS echoes constitute about 2% of all MR detections.