Meteoroids 2013, Proceedings of the Astronomical Conference, Held at A.M
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Meteor Activity Outlook for June 20-26, 2020
Meteor Activity Outlook for June 20-26, 2020 AMS Event #2360-2020, Fireball over Thuringia state, Germany on May 15th, 2020 © M.Tebeck During this period the moon reaches its new phase on Monday June 22nd. At this time, the moon is located near the sun and it invisible at night. As the week progresses the waxing crescent moon will enter the evening sky but will not interfere with meteor observing. The estimated total hourly meteor rates for evening observers this week is near 3 for those viewing from the northern hemisphere and 4 for those located south of the equator. For morning observers, the estimated total hourly rates should be near 11 as seen from mid-northern latitudes (45N) and 15 as seen from tropical southern locations (25S). The actual rates will also depend on factors such as personal light and motion perception, local weather conditions, alertness, and experience in watching meteor activity. Note that the hourly rates listed below are estimates as viewed from dark sky sites away from urban light sources. Observers viewing from urban areas will see less activity as only the brighter meteors will be visible from such locations. The radiant (the area of the sky where meteors appear to shoot from) positions and rates listed below are exact for Saturday night/Sunday morning June 20/21. These positions do not change greatly day to day so the listed coordinates may be used during this entire period. Most star atlases (available at science stores and planetariums) will provide maps with grid lines of the celestial coordinates so that you may find out exactly where these positions are located in the sky. -
Metal Species and Meteor Activity 5 Discussion J
Atmos. Chem. Phys. Discuss., 9, 18705–18726, 2009 Atmospheric www.atmos-chem-phys-discuss.net/9/18705/2009/ Chemistry ACPD © Author(s) 2009. This work is distributed under and Physics 9, 18705–18726, 2009 the Creative Commons Attribution 3.0 License. Discussions This discussion paper is/has been under review for the journal Atmospheric Chemistry Metal species and and Physics (ACP). Please refer to the corresponding final paper in ACP if available. meteor activity J. Correira et al. Title Page Metal concentrations in the upper Abstract Introduction atmosphere during meteor showers Conclusions References J. Correira1,*, A. C. Aikin1, J. M. Grebowsky2, and J. P. Burrows3 Tables Figures 1 The Catholic University of America, Institute for Astrophysics and Computational Sciences J I Department of Physics, Washington, DC 20064, USA 2 NASA Goddard Space Flight Center, Code 695, Greenbelt, MD 20771, USA J I 3Institute of Environmental Physics (IUP), University of Bremen, Bremen, Germany Back Close *now at: Computational Physics, Inc., Springfield, Virginia, USA Full Screen / Esc Received: 30 June 2009 – Accepted: 10 August 2009 – Published: 10 September 2009 Correspondence to: J. Correira ([email protected]) Printer-friendly Version Published by Copernicus Publications on behalf of the European Geosciences Union. Interactive Discussion 18705 Abstract ACPD Using the nadir-viewing Global Ozone Measuring Experiment (GOME) UV/VIS spec- trometer on the ERS-2 satellite, we investigate short term variations in the vertical mag- 9, 18705–18726, 2009 nesium column densities in the atmosphere and any connection to possible enhanced 5 mass deposition during a meteor shower. Time-dependent mass influx rates are de- Metal species and rived for all the major meteor showers using published estimates of mass density and meteor activity temporal profiles of meteor showers. -
Download This Article in PDF Format
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. -
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 -
7 X 11 Long.P65
Cambridge University Press 978-0-521-85349-1 - Meteor Showers and their Parent Comets Peter Jenniskens Index More information Index a – semimajor axis 58 twin shower 440 A – albedo 111, 586 fragmentation index 444 A1 – radial nongravitational force 15 meteoroid density 444 A2 – transverse, in plane, nongravitational force 15 potential parent bodies 448–453 A3 – transverse, out of plane, nongravitational a-Centaurids 347–348 force 15 1980 outburst 348 A2 – effect 239 a-Circinids (1977) 198 ablation 595 predictions 617 ablation coefficient 595 a-Lyncids (1971) 198 carbonaceous chondrite 521 predictions 617 cometary matter 521 a-Monocerotids 183 ordinary chondrite 521 1925 outburst 183 absolute magnitude 592 1935 outburst 183 accretion 86 1985 outburst 183 hierarchical 86 1995 peak rate 188 activity comets, decrease with distance from Sun 1995 activity profile 188 Halley-type comets 100 activity 186 Jupiter-family comets 100 w 186 activity curve meteor shower 236, 567 dust trail width 188 air density at meteor layer 43 lack of sodium 190 airborne astronomy 161 meteoroid density 190 1899 Leonids 161 orbital period 188 1933 Leonids 162 predictions 617 1946 Draconids 165 upper mass cut-off 188 1972 Draconids 167 a-Pyxidids (1979) 199 1976 Quadrantids 167 predictions 617 1998 Leonids 221–227 a-Scorpiids 511 1999 Leonids 233–236 a-Virginids 503 2000 Leonids 240 particle density 503 2001 Leonids 244 amorphous water ice 22 2002 Leonids 248 Andromedids 153–155, 380–384 airglow 45 1872 storm 380–384 albedo (A) 16, 586 1885 storm 380–384 comet 16 1899 -
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. -
Proceedings of the International Meteor Conference La Palma, Canary Islands, Spain 20–23 September, 2012
ISBN 978-2-87355-024-4 Proceedings of the International Meteor Conference La Palma, Canary Islands, Spain 20–23 September, 2012 Published by the International Meteor Organization 2013 Edited by Marc Gyssens and Paul Roggemans Proceedings of the International Meteor Conference La Palma, Canary Islands, Spain, 20–23 September, 2012 International Meteor Organization ISBN 978-2-87355-024-4 Copyright notices c 2013 The International Meteor Organization The copyright of papers in this publication remains with the authors. It is the aim of the IMO to increase the spread of scientific information, not to restrict it. When material is submitted to the IMO for publication, this is taken as indicating that the author(s) grant(s) permission for the IMO to publish this material any number of times, in any format(s), without payment. This permission is taken as covering rights to reproduce both the content of the material and its form and appearance, including images and typesetting. Formats may include paper and electronically readable storage media. Other than these conditions, all rights remain with the author(s). When material is submitted for publication, this is also taken as indicating that the author(s) claim(s) the right to grant the permissions described above. The reader is granted permission to make unaltered copies of any part of the document for personal use, as well as for non-commercial and unpaid sharing of the information with third parties, provided the source and publisher are mentioned. For any other type of copying or distribution, prior written permission from the publisher is mandatory. -
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. -
Fireballs and Meteor Showers As Seen by the NASA All Sky Fireball Network
Fireballs and meteor showers as seen by the NASA All Sky Fireball Network Althea Moorhead NASA Meteoroid Environment Office, MSFC Outline I Overview of all-sky network and data I Discussion of shower and sporadic meteors I Past and current projects that use all-sky data I Potential student projects 2 / 54 All-sky meteor camera and sample image 3 / 54 Map 4 / 54 Meteor detection 5 / 54 Meteor detection 6 / 54 Meteor detection 7 / 54 False positives: satellites (ISS) 8 / 54 False positives: satellites (Iridium Flare) 9 / 54 False positives: airplanes 10 / 54 False positives: vehicle headlights 11 / 54 False positives: lightning 12 / 54 False positives: birds 13 / 54 False positives: insects and spiders 14 / 54 False positives I Satellites: too high I Airplanes: too low I Headlights: only one camera I Lightning: too low, track is erratic I Birds and bugs: only one camera, track is erratic 15 / 54 Meteor detection: false negatives I We get false negatives as well (meteors that are rejected) I We review these rejects near-daily and override as needed I These show up in the log more than a day later 16 / 54 Event data 17 / 54 Event data 18 / 54 Camera stations 19 / 54 Position relative to cameras 20 / 54 Brightness 21 / 54 Orbit 22 / 54 Orbit time 20180108 4.7600 hours lat 33 22 29.208 = 33.3748 deg lon 250 53 24.216 = 250.8901 deg ht 54.610 b -14.07390 7.06982 -5.75963 19.87105 alp 84.870 +/- 19.112 deg del 22.386 +/- 10.702 deg v_inf 21.555 +/- 2.256 km/s v_avg 21.555 +/- 2.256 km/s a 7.214 +/- 22.675 AU e 0.888 +/- 0.338 incl 0.863 +/- 5.700 deg omega 51.721 +/- 23.497 deg asc_node 107.747 +/- 0.979 deg v_g 18.350 +/- 2.643 km/s v_h 41.004 +/- 4.713 km/s alp_geo 84.476 +/- 20.584 deg del_geo 21.582 +/- 11.588 deg q_per 0.806 +/- 0.118 AU q_aph 13.622 +/- 45.252 AU lambda 85.120 +/- 19.140 deg beta -1.757 +/- 11.604 deg true anom 308.131 +/- 11.604 deg T_j 1.8 23 / 54 Shower vs.