IAU Meteor Data Center| the Shower Database: a Status Report
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A&A 598, A40 (2017) Astronomy DOI: 10.1051/0004-6361/201629659 & c ESO 2017 Astrophysics Separation and confirmation of showers? L. Neslušan1 and M. Hajduková, Jr.2 1 Astronomical Institute, Slovak Academy of Sciences, 05960 Tatranska Lomnica, Slovak Republic e-mail: [email protected] 2 Astronomical Institute, Slovak Academy of Sciences, Dubravska cesta 9, 84504 Bratislava, Slovak Republic e-mail: [email protected] Received 6 September 2016 / Accepted 30 October 2016 ABSTRACT Aims. Using IAU MDC photographic, IAU MDC CAMS video, SonotaCo video, and EDMOND video databases, we aim to separate all provable annual meteor showers from each of these databases. We intend to reveal the problems inherent in this procedure and answer the question whether the databases are complete and the methods of separation used are reliable. We aim to evaluate the statistical significance of each separated shower. In this respect, we intend to give a list of reliably separated showers rather than a list of the maximum possible number of showers. Methods. To separate the showers, we simultaneously used two methods. The use of two methods enables us to compare their results, and this can indicate the reliability of the methods. To evaluate the statistical significance, we suggest a new method based on the ideas of the break-point method. Results. We give a compilation of the showers from all four databases using both methods. Using the first (second) method, we separated 107 (133) showers, which are in at least one of the databases used. These relatively low numbers are a consequence of discarding any candidate shower with a poor statistical significance. -
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. -
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. -
„Ordinary“ Showers
„Ordinary“ Showers # MDC Show Shower Name MDC Number Solar Longitude Right Declination Vgeo Comment Num Code Status of Ascension ber Meteors Mean/ Max Interval Mean Drift Mean Drift Mean Drift [°] [°] [°] [°] [°] [°] [km/s] [km/s] 1 40 ZCY zeta Cygnids W 500 16 13-20 302 +0.3 +40 +0.2 40 - NM; SS: α,δ,v geo ; DM: δ 2 131 DAL delta Aquilids W 200 20 17-23 308 +1.0 +12 +0.3 63 - DM: δ 3 136 SLE sigma Leonids W 1,000 26 18-35 201 +0.6 +3 +0.0 19 -0.16 NM; DM: α,v geo 348 ARC April rho Cygnids E 4 1,700 33 13-44 314 +0.8 +44.5 +0.3 42 +0.00 ARC and NCY are identical 409 NCY nu Cygnids W 5 346 XHE x Herculids W 300 352 350-355 256 +0.8 +48.5 -0.0 35 - NM 6 6 LYR April Lyrids E 4,000 32.5 28-35 272.6 +0.65 +33.2 -0.3 45.5 +0.25 7 343 HVI H Virginids W 200 41 39-43 205 +0.7 -11 -0.5 17 - NM; SD; NAD 8 31 ETA eta Aquariids E 3,800 47 38-59 339.1 +0.64 -0.5 +0.33 66.5 +0.1 9 531 GAQ gamma Aquilids W 320 48 45-52 307 -0.1 +14.5 -0.1 66 - NM; SS: α; Part of N Apex? 10 145 ELY eta Lyrids E 800 50 45-52 291.3 +0.15 +43.4 +0.0 42.6 - Maybe active longer; DM: δ 11 520 MBC May beta Capricornids W 150 59 56-61 305 +0.7 -15 +0.3 68 - NM; WS; similar to 7CCA 12 362 JMC June mu Cassiopeiids W 150 71 69-74 11 +2.8 +53 +0.5 42 - WS; SS: α,δ,v geo 13 171 ARI Daytime Arietids E 70 77 74-79 44 +1.0 +23.5 +0.1 42 NM; Daytime shower; DM: v geo 14 164 NZC Northern June Aquilids E 200 82 79-84 293 +1.0 -12 -0.4 42 - DM: v geo 510 JRC NM; SD; NAD; short & strong; 15 June rho Cygnids W 190 84 83-85 320.4 +0.8 44.7 -0.8 48 - 521 JRP JRP is identical to JRC 16 410 DPI -
Meteor Activity Outlook for January 2-8, 2021
Meteor Activity Outlook for January 2-8, 2021 Daniel Bush captured this impressive fireball at 04:11 UT (23:11 CDT on Sept. 5) on 6 Septmeber 2020, from Albany, Missouri, USA. For more details on this particular event visit: https://fireball.amsmeteors.org/members/imo_view/event/2020/5020. Credit Daniel Bush January is best known for the Quadrantids, which have the potential of being the best shower of the year. Unfortunately, this shower is short lived and occurs during some of the worst weather in the northern hemisphere. Due to the high northern declination (celestial latitude) and short summer nights, little of this activity can be seen south of the equator. There are many very minor showers active throughout the month. Unfortunately, most of these produce less than 1 shower member per hour and do not add much to the overall activity total. Activity gets interesting as seen from the southern hemisphere as ill-defined radiants in Vela, Carina, and Crux become active this month. This activity occurs during the entire first quarter of the year and moves eastward into Centaurus in February and ends in March with activity in Norma and Lupus. Sporadic rates are generally similar in both hemispheres this month. Sporadic rates are falling though for observers in the northern hemisphere and rising as seen from the southern hemisphere. During this period, the moon reaches its last quarter phase on Wednesday January 6th. At this time, the moon is located 90 degrees west of the sun in the sky and will rise near midnight standard time. -
Aa501 Graphicx Document an Artificial Meteors Database As a Test for The
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by CERN Document Server aa501 graphicx document An artificial meteors database as a test for the presence of weak showers Arkadiusz Olech 1 and Mariusz Wi´sniewski 2 A.Olech Nicolaus Copernicus Astronomical Center, ul. Bartycka 18, 00-716 Warszawa, Poland Received .................., 2001; accepted ................ 2002 We have constructed an artificial meteor database resembling in all details the real sample collected by the observers of the Comets and Meteors Workshop in the years 1996-1999. The artificial database includes the sporadic meteors and also events from the following showers: Perseids, Aquarid complex, α- Capricornids, July Pegasids and Sagittarids. This database was searched for the presence of the radiants of two weak showers: α-Cygnids and Delphinids. The lack of these radiants in the artificial database and their existence in the real observations suggests that α-Cygnids and Delphinids are the real showers and their radiants could not be formed as an effect of intersections of back prolongated paths of meteors belonging to other showers. Solar System – meteors – α-Cygnids, Delphinids An artificial meteors database as a test ... Introduction Recently, Polish observers taking part in the Comets and Meteors Workshop (CMW) have reported the rediscovery of two July meteor showers - α-Cygnids and Delphinids (Olech et al. 1999a, 1999b, Stelmach & Olech 2000, Wi´sniewski & Olech 2000, 2001). Both of these showers are weak with maximum Zenithal Hourly Rates (ZHRs) slightly exceeding or laying beneath the sporadic background. The α-Cygnids are active from the end of June until the end of July. -
The Status of the NASA All Sky Fireball Network
https://ntrs.nasa.gov/search.jsp?R=20120004179 2019-08-30T19:42:51+00:00Z The Status of the NASA All Sky Fireball Network William J. Cooke Meteoroid Environment Office, NASA Marshall Space Flight Center, Huntsville, AL 35812 USA. [email protected] Danielle E. Moser MITS/Dynetics, NASA Marshall Space Flight Center, Huntsville, AL 35812 USA. [email protected] Abstract Established by the NASA Meteoroid Environment Office, the NASA All Sky Fireball Network consists of 6 meteor video cameras in the southern United States, with plans to expand to 15 cameras by 2013. As of mid-2011, the network had detected 1796 multi-station meteors, including meteors from 43 different meteor showers. The current status of the NASA All Sky Fireball Network is described, alongside preliminary results. 1 Introduction The NASA Meteoroid Environment Office (MEO), located at the Marshall Space Flight Center in Huntsville, Alabama, USA, is the NASA organization responsible for meteoroid environments as they pertain to spacecraft engineering and operations. Understanding the meteoroid environment can help spacecraft designers to better protect critical components on spacecraft or avoid critical operations such as extravehicular activities during periods of higher flux such as meteor showers. In mid-2008, the MEO established the NASA All Sky Fireball Network, a network of meteor cameras in the southern United States. The objectives of this video network are to 1) establish the speed distribution of cm-sized meteoroids, 2) determine which sporadic sources produce large particles, 3) determine (low precision) orbits for bright meteors, 4) attempt to discover the size at which showers begin to dominate the meteoroid flux, 5) monitor the activity of major meteor showers, and 6) assist in the location of meteorite falls. -
Investigating the Radiant Sources of Meteors Anamol Mittal, Dr
International Journal of Scientific & Engineering Research Volume 8, Issue 10, October-2017 1369 ISSN 2229-5518 Investigating the radiant sources of meteors Anamol Mittal, Dr. K. Kishore Kumar Abstract— The results obtained in the present study, which are related to basic meteor phenomenon such as meteor velocity distribution, height distribution and annual variability of meteors are discussed. An attempt is also made to identify the peak radiant sources of the observed meteors. The results are found to be consistent with the present understanding of the meteor phenomenon. Further studies are required to estimate the orbits of the meteors using single station observations. The important outcome of the present study is the algorithm for estimating the radiant sources using azimuth, zenith angle observations of meteor radar. Index Terms— Astronomy, earth sciences, entrance velocity distribution, meteor wind radar, meteors, radiant sources, Thumba —————————— —————————— 1 INTRODUCTION eople have always wondered about the worlds that lie 3. Epoch: In astronomy, an epoch is a moment in time P beyond the boundaries of sky, the purpose of our exis- used as a reference point for some time-varying as- tence, whether the existence of earth is a result of some tronomical quantity, such as the celestial coordinates higher purpose or just a lucky coincidence? Well, answers to or elliptical orbital elements of a celestial body, be- these questions are not known and beyond the reach of present technology. One such question asks: Where do the cause these are subject to perturbations and vary with meteoroids (most commonly known as falling stars) come time.[2] from and how is their distribution in solar system related to the formation of planets and other solar system bodies? You may find answers to these questions as you proceed through the report. -
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. -
Craters and Airbursts
Craters and Airbursts • Most asteroids and comets fragments explode in the air as fireballs or airbursts; only the largest ones make craters. • Evidence indicates that the YDB impact into the Canadian ice sheet made ice-walled craters that melted away long ago. • The YDB impact also possibly created rocky craters, most likely along the edge of the ice sheet in Canada or underwater in the oceans. • Our group is planning expeditions to search for impact evidence and hidden craters, for example to North Dakota, Montana, Quebec, and Nova Scotia. The following pages show what could happen during an impact NOTE: this website is a brief, non-technical introduction to the YDB impact hypothesis. For in-depth information, go to “Publications” to find links to detailed scientific papers. NAME OF SHOWER NAME OF SHOWER Alpha Aurigids Leo Minorids Meteor Showers Alpha Bootids Leonids Alpha Capricornids Librids Alpha Carinids Lyrids Comet impacts are common, Alpha Centaurids Monocerotids Alpha Crucids Mu Virginids but usually, they are harmless Alpha Cygnids Northern Delta Aquariids Alpha Hydrids Northern Iota Aquariids Alpha Monocerotids Northern Taurids Alpha Scorpiids October Arietids • Earth is hit by 109 meteor Aries-triangulids Omega Capricornids Arietids Omega Scorpiids showers every year (listed at Beta Corona Austrinids Omicron Centaurids right), averaging 2 collisions Chi Orionids Orionids Coma Berenicids Perseids with streams each week Delta Aurigids Phoenicids Delta Cancrids Pi Eridanids Delta Eridanids Pi Puppids • Oddly, most “meteor showers”