Generating Variable Lightcurves of Asteroid 135 Hertha Using Differential Photometry
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The Minor Planet Bulletin
THE MINOR PLANET BULLETIN OF THE MINOR PLANETS SECTION OF THE BULLETIN ASSOCIATION OF LUNAR AND PLANETARY OBSERVERS VOLUME 36, NUMBER 3, A.D. 2009 JULY-SEPTEMBER 77. PHOTOMETRIC MEASUREMENTS OF 343 OSTARA Our data can be obtained from http://www.uwec.edu/physics/ AND OTHER ASTEROIDS AT HOBBS OBSERVATORY asteroid/. Lyle Ford, George Stecher, Kayla Lorenzen, and Cole Cook Acknowledgements Department of Physics and Astronomy University of Wisconsin-Eau Claire We thank the Theodore Dunham Fund for Astrophysics, the Eau Claire, WI 54702-4004 National Science Foundation (award number 0519006), the [email protected] University of Wisconsin-Eau Claire Office of Research and Sponsored Programs, and the University of Wisconsin-Eau Claire (Received: 2009 Feb 11) Blugold Fellow and McNair programs for financial support. References We observed 343 Ostara on 2008 October 4 and obtained R and V standard magnitudes. The period was Binzel, R.P. (1987). “A Photoelectric Survey of 130 Asteroids”, found to be significantly greater than the previously Icarus 72, 135-208. reported value of 6.42 hours. Measurements of 2660 Wasserman and (17010) 1999 CQ72 made on 2008 Stecher, G.J., Ford, L.A., and Elbert, J.D. (1999). “Equipping a March 25 are also reported. 0.6 Meter Alt-Azimuth Telescope for Photometry”, IAPPP Comm, 76, 68-74. We made R band and V band photometric measurements of 343 Warner, B.D. (2006). A Practical Guide to Lightcurve Photometry Ostara on 2008 October 4 using the 0.6 m “Air Force” Telescope and Analysis. Springer, New York, NY. located at Hobbs Observatory (MPC code 750) near Fall Creek, Wisconsin. -
Asteroids, Comets, Meteors 1991, Pp. 641-643 Lunar and Planetary Institute, Houston, 1992 W/Eg- 641
Asteroids, Comets, Meteors 1991, pp. 641-643 Lunar and Planetary Institute, Houston, 1992 w/eg- 641 THE MASS OF (1) CERES FROM PERTURBATIONS ON (348) MAY Gareth V. Williams Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, U.S.A. ABSTRACT The most promising ground-based technique for determining the mass of s minor planet is the observation of the perturbations it induces in the motion of another minor planet. This method requires cv.reful observation of both minor planets over extended periods of time. The mass of (1) Ceres has been determined from the perturbations on (348) May, which made three close approaches to Ceres at intervals of 46 years between 1891 and 1984. The motion of May is clearly influenced by Ceres, and by Using different test masses for Ceres, a search has been made to determine the mass of Ceres that minimizes the residuals in the observations of May. Introduction The masses of the largest minor planets are rather poorly known. Traditionally, the masses of the major planets were obtained by observing their mutual perturbations or by observing their satellite systems. These methods are not easily applicable to minor planets: no minor planets are known to have satellites; the minor-planet perturbations on any of the major planets are negligible (from a ground-based viewpoint, except by tracking spacecraft); and the mutual minor-planet perturbations generally are small. However, the mutual-perturbation method, when applied to suitable objects, is the best ground-based method currently available for determimng minor-planet masses. The best circumstances for using this method occur when one of the minor planets is large compared to the other, when the two objects make close, periodic approaches to each other, and when both have long observational histories. -
Ice& Stone 2020
Ice & Stone 2020 WEEK 51: DECEMBER 13-19 Presented by The Earthrise Institute # 51 Authored by Alan Hale COMET OF THE WEEK: The Great Comet of 1680 Perihelion: 1680 December 18.49, q = 0.006 AU The Great Comet of 1680 over Rotterdam in The Netherlands, during late December 1680 as painted by the Dutch artist Lieve Verschuier. This particular comet was undoubtedly one of the brightest comets of the 17th Century, but it is also one of the most important comets in history from a scientific perspective, and perhaps even from the perspective of overall human history. While there were certainly plenty of superstitions attached to the comet’s appearance, the scientific investigations made of it were among the beginnings of the era in European history we now call The Enlightenment, and indeed, in a sense the Great Comet of 1680 can perhaps be considered as one of the sparks of that era. The significance began with the comet’s discovery, which was made on the morning of November 14, 1680, by a German astronomer residing in Coburg, Gottfried Kirch – the first comet ever to be discovered by means of a telescope. It was already around 4th magnitude at that time, and located near the star Regulus in the constellation Leo; from that point it traveled eastward and brightened rapidly, being closest to Earth (0.42 AU) on November 30. By that time it was a conspicuous naked-eye object with a tail 20 to 30 degrees long, and it remained visible for another week before disappearing into morning twilight. -
Hydrated Minerals on Asteroids: the Astronomical Record
Hydrated Minerals on Asteroids: The Astronomical Record A. S. Rivkin, E. S. Howell, F. Vilas, and L. A. Lebofsky March 28, 2002 Corresponding Author: Andrew Rivkin MIT 54-418 77 Massachusetts Ave. Cambridge MA, 02139 [email protected] 1 1 Abstract Knowledge of the hydrated mineral inventory on the asteroids is important for deducing the origin of Earth’s water, interpreting the meteorite record, and unraveling the processes occurring during the earliest times in solar system history. Reflectance spectroscopy shows absorption features in both the 0.6-0.8 and 2.5-3.5 pm regions, which are diagnostic of or associated with hydrated minerals. Observations in those regions show that hydrated minerals are common in the mid-asteroid belt, and can be found in unex- pected spectral groupings, as well. Asteroid groups formerly associated with mineralogies assumed to have high temperature formation, such as MAand E-class asteroids, have been observed to have hydration features in their reflectance spectra. Some asteroids have apparently been heated to several hundred degrees Celsius, enough to destroy some fraction of their phyllosili- cates. Others have rotational variation suggesting that heating was uneven. We summarize this work, and present the astronomical evidence for water- and hydroxyl-bearing minerals on asteroids. 2 Introduction Extraterrestrial water and water-bearing minerals are of great importance both for understanding the formation and evolution of the solar system and for supporting future human activities in space. The presence of water is thought to be one of the necessary conditions for the formation of life as 2 we know it. -
M-Type Asteroids: Primitive, Metallic, Or Both?
Artist’s concept of mission to (16) Psyche NASA/JPL-Caltech M-Type asteroids: primitive, metallic, or both? Zoe A. Landsman1 2 1 Collaborators: J. Emery , H. Campins 1 University of Central Florida, Orlando, FL, USA 2 University of Tennessee, Knoxville, TN, USA 15th Meeting of the NASA Small Bodies Assessment Group JHU APL, Laurel, MD | June 28-30, 2016 SBAG | June 28 – 30, 2016 Background The M-Type Asteroids o M-types are the moderate-albedo group of the spectrally degenerate X taxon o Many have a 3-μm hydration feature (e.g., Rivkin et al. 2000, Landsman et al. 2015) o Most have weak silicate features at 0.9 μm ±1.9 μm (e.g., Fornasier et al. 2010, Hardersen et al. 2011) o Many have elevated radar albedos, suggesting high surface density (e.g., Neeley et al. 2014, Shepard et al. 2015) Bottom figure: Tholen 1984 SBAG | June 28 – 30, 2016 Previous Work (Landsman et al. 2015) Studied 6 M-types in the 2 – 4 μm region using the IRTF o (69) Hesperia, (136) Austria, (216) Kleopatra, (261) Prymno, (337) “Rounded” feature Devosa, (418) Alemannia Ice? Evidence for a 3-μm hydration feature on all 6, with band depths from ~4 – 8% Diversity in the shape of feature among the asteroids “Sharp” feature Phyllosilicates SBAG | June 28 – 30, 2016 M-types in the Mid-Infrared Thermal modeling allows insight into surface properties of asteroids o Albedo, thermal inertia, surface roughness, etc. Emissivity spectra contain information about mineralogy and grain size This project: Spitzer Space Telescope o Perform thermophysical modeling on 5 – 40 μm Spitzer InfraRed Spectrograph (IRS) spectra of M-type spectra o Also look at emissivity spectra o Focus on asteroids well-characterized at other wavelengths Emissivity Spectra SBAG | June 28 – 30, 2016 Preliminary TPM Results Our TPM Previous TPM work Asteroid R (km) Γ (SI units) R (km) Γ (SI units) Ref . -
Absolute Magnitudes of Asteroids and a Revision of Asteroid Albedo Estimates from WISE Thermal Observations ⇑ Petr Pravec A, , Alan W
Icarus 221 (2012) 365–387 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Absolute magnitudes of asteroids and a revision of asteroid albedo estimates from WISE thermal observations ⇑ Petr Pravec a, , Alan W. Harris b, Peter Kušnirák a, Adrián Galád a,c, Kamil Hornoch a a Astronomical Institute, Academy of Sciences of the Czech Republic, Fricˇova 1, CZ-25165 Ondrˇejov, Czech Republic b 4603 Orange Knoll Avenue, La Cañada, CA 91011, USA c Modra Observatory, Department of Astronomy, Physics of the Earth, and Meteorology, FMFI UK, Bratislava SK-84248, Slovakia article info abstract Article history: We obtained estimates of the Johnson V absolute magnitudes (H) and slope parameters (G) for 583 main- Received 27 February 2012 belt and near-Earth asteroids observed at Ondrˇejov and Table Mountain Observatory from 1978 to 2011. Revised 27 July 2012 Uncertainties of the absolute magnitudes in our sample are <0.21 mag, with a median value of 0.10 mag. Accepted 28 July 2012 We compared the H data with absolute magnitude values given in the MPCORB, Pisa AstDyS and JPL Hori- Available online 13 August 2012 zons orbit catalogs. We found that while the catalog absolute magnitudes for large asteroids are relatively good on average, showing only little biases smaller than 0.1 mag, there is a systematic offset of the cat- Keywords: alog values for smaller asteroids that becomes prominent in a range of H greater than 10 and is partic- Asteroids ularly big above H 12. The mean (H H) value is negative, i.e., the catalog H values are Photometry catalog À Infrared observations systematically too bright. -
(50278) 2000Cz12
A&A 455, L29–L31 (2006) Astronomy DOI: 10.1051/0004-6361:20065760 & c ESO 2006 Astrophysics Letter to the Editor New mass determination of (15) Eunomia based on a very close encounter with (50278) 2000CZ12 A. Vitagliano1 andR.M.Stoss2,3 1 Dipartimento di Chimica, Università di Napoli Federico II, Complesso Universitario di Monte S. Angelo, via Cintia, 80126 Napoli, Italy e-mail: [email protected] 2 Observatorio Astronómico de Mallorca, Camí de l’Observatori, 07144 Costitx, Mallorca, Spain 3 Astronomisches Rechen-Institut, Mönchhofstr. 12-14, 69120 Heidelberg, Germany Received 5 June 2006 / Accepted 22 June 2006 ABSTRACT Aims. The possibility of determining the mass of large asteroids (other than Ceres, Pallas, and Vesta) from recent close encounters with smaller bodies has been investigated, and a new and more accurate determination of the mass of the asteroid (15) Eunomia is presented. Methods. The circumstances of the close approaches between large asteroids and the ca. 129 000 numbered ones were found by a numerical integration over the past 20 years. The cases for which an appreciable perturbation could be expected were investigated by fitting the mass of the perturbing body to the available observations. Results. A very close approach took place on March 4, 2002, between Eunomia and (50278) 2000CZ12, at a nominal distance of 55 200 km. The resulting perturbation in the mean motion of the smaller body was substantially larger than for the other detected events, amounting to ca. 0.9 arcsecs/y. The orbital elements of (50278) 2000CZ12 were fitted together with the mass of Eunomia 19 −11 on 106 of 110 observations spanning 1950 to 2006, resulting in a mass of 3.25 × 10 kg (1.64 × 10 MSun) with a formal 1σ relative uncertainty of 3.7%. -
Hydrated Minerals on Asteroids 235
Rivkin et al.: Hydrated Minerals on Asteroids 235 Hydrated Minerals on Asteroids: The Astronomical Record A. S. Rivkin Massachusetts Institute of Technology E. S. Howell Arecibo Observatory F. Vilas NASA Johnson Space Center L. A. Lebofsky University of Arizona Knowledge of the hydrated mineral inventory on the asteroids is important for deducing the origin of Earth’s water, interpreting the meteorite record, and unraveling the processes occurring during the earliest times in solar system history. Reflectance spectroscopy shows absorption features in both the 0.6–0.8 and 2.5–3.5-µm regions, which are diagnostic of or associated with hydrated minerals. Observations in those regions show that hydrated minerals are common in the mid-asteroid belt, and can be found in unexpected spectral groupings as well. Asteroid groups formerly associated with mineralogies assumed to have high-temperature formation, such as M- and E-class asteroids, have been observed to have hydration features in their reflectance spectra. Some asteroids have apparently been heated to several hundred degrees Celsius, enough to destroy some fraction of their phyllosilicates. Others have rotational variation suggesting that heating was uneven. We summarize this work, and present the astronomical evidence for water- and hydroxyl-bearing minerals on asteroids. 1. INTRODUCTION to be common. Indeed, water is found throughout the outer solar system on satellites (Clark and McCord, 1980; Clark Extraterrestrial water and water-bearing minerals are of et al., 1984), Kuiper Belt Objects (KBOs) (Brown et al., great importance both for understanding the formation and 1997), and comets (Bregman et al., 1988; Brooke et al., 1989) evolution of the solar system and for supporting future as ice, and on the planets as vapor (Larson et al., 1975; human activities in space. -
Main-Belt Asteroids with Wise/Neowise: Near-Infrared Albedos
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Caltech Authors The Astrophysical Journal, 791:121 (11pp), 2014 August 20 doi:10.1088/0004-637X/791/2/121 C 2014. The American Astronomical Society. All rights reserved. Printed in the U.S.A. MAIN-BELT ASTEROIDS WITH WISE/NEOWISE: NEAR-INFRARED ALBEDOS Joseph R. Masiero1, T. Grav2, A. K. Mainzer1,C.R.Nugent1,J.M.Bauer1,3, R. Stevenson1, and S. Sonnett1 1 Jet Propulsion Laboratory/Caltech, 4800 Oak Grove Drive, MS 183-601, Pasadena, CA 91109, USA; [email protected], [email protected], [email protected], [email protected], [email protected], [email protected] 2 Planetary Science Institute, Tucson, AZ, USA; [email protected] 3 Infrared Processing and Analysis Center, Caltech, Pasadena, CA, USA Received 2014 May 14; accepted 2014 June 25; published 2014 August 6 ABSTRACT We present revised near-infrared albedo fits of 2835 main-belt asteroids observed by WISE/NEOWISE over the course of its fully cryogenic survey in 2010. These fits are derived from reflected-light near-infrared images taken simultaneously with thermal emission measurements, allowing for more accurate measurements of the near- infrared albedos than is possible for visible albedo measurements. Because our sample requires reflected light measurements, it undersamples small, low-albedo asteroids, as well as those with blue spectral slopes across the wavelengths investigated. We find that the main belt separates into three distinct groups of 6%, 16%, and 40% reflectance at 3.4 μm. -
The Planetary and Lunar Ephemeris DE 421
IPN Progress Report 42-178 • August 15, 2009 The Planetary and Lunar Ephemeris DE 421 William M. Folkner,* James G. Williams,† and Dale H. Boggs† The planetary and lunar ephemeris DE 421 represents updated estimates of the orbits of the Moon and planets. The lunar orbit is known to submeter accuracy through fitting lunar laser ranging data. The orbits of Venus, Earth, and Mars are known to subkilometer accu- racy. Because of perturbations of the orbit of Mars by asteroids, frequent updates are needed to maintain the current accuracy into the future decade. Mercury’s orbit is determined to an accuracy of several kilometers by radar ranging. The orbits of Jupiter and Saturn are determined to accuracies of tens of kilometers as a result of spacecraft tracking and modern ground-based astrometry. The orbits of Uranus, Neptune, and Pluto are not as well deter- mined. Reprocessing of historical observations is expected to lead to improvements in their orbits in the next several years. I. Introduction The planetary and lunar ephemeris DE 421 is a significant advance over earlier ephemeri- des. Compared with DE 418, released in July 2007,1 the DE 421 ephemeris includes addi- tional data, especially range and very long baseline interferometry (VLBI) measurements of Mars spacecraft; range measurements to the European Space Agency’s Venus Express space- craft; and use of current best estimates of planetary masses in the integration process. The lunar orbit is more robust due to an expanded set of lunar geophysical solution parameters, seven additional months of laser ranging data, and complete convergence. -
Models from Sparse Photometry Inversion
Asteroid models from sparse photometry Josef Durechˇ 1 1Astronomical Institute, Charles University in Prague Workshop on the Physical Properties of Asteroids Paris, 22-23 March 2010 Outline 1 Introduction Sparse photometry Period search Hipparcos data example 2 Questions How many data do you need? Number of points, spread over how many years? How much data do you expect (Pan-STARRS, Gaia, LSST, VO)? Photometric precision you need to do any work Sensibility to phase angle, sub-Earth point latitude Advantage of adding one single dense LC Advantage of adding one single occultation or image DAMIT 3 Current and future work sparse photometry data sparse in time with respect to the rotation period one or a few points per night tens to hundreds points from more apparitions all-sky surveys like Pan-STARRS, Gaia (Hipparcos), LSST sparse data from astrometry { noisy but sometimes useful Two types of photometric data standard lightcurves one lightcurve per night, 10{100 points we need tens of lightcurves from three or more apparitions to derive a model it takes time to collect enough lightcurves ∼ 3800 asteroids have at least one LC { period determination ∼ 100 asteroids with enough lightcurves to make a full model Two types of photometric data standard lightcurves one lightcurve per night, 10{100 points we need tens of lightcurves from three or more apparitions to derive a model it takes time to collect enough lightcurves ∼ 3800 asteroids have at least one LC { period determination ∼ 100 asteroids with enough lightcurves to make a full model sparse photometry data sparse in time with respect to the rotation period one or a few points per night tens to hundreds points from more apparitions all-sky surveys like Pan-STARRS, Gaia (Hipparcos), LSST sparse data from astrometry { noisy but sometimes useful Dense vs. -
Astrometric Asteroid Masses: a Simultaneous Determination
A&A 565, A56 (2014) Astronomy DOI: 10.1051/0004-6361/201322766 & c ESO 2014 Astrophysics Astrometric asteroid masses: a simultaneous determination Edwin Goffin Aartselaarstraat 14, 2660 Hoboken, Belgium e-mail: [email protected] Received 27 September 2013 / Accepted 18 March 2014 ABSTRACT Using over 89 million astrometric observations of 349 737 numbered minor planets, an attempt was made to determine the masses of 230 of them by simultaneously solving for corrections to all orbital elements and the masses. For 132 minor planets an acceptable result was obtained, 49 of which appear to be new. Key words. astrometry – celestial mechanics – minor planets, asteroids: general 1. Introduction substantial number of test asteroids (349 737). Section 2 explains the basic principles and problems of simultaneous asteroid mass The astrometric determination of asteroid masses is the tech- determination and in Sect. 3 the details of the actual calculations nique of calculating the mass of asteroids (hereafter called “per- are given. Section 4 briefly deals with the observations used and turbing asteroids” or “perturbers”) from the gravitational pertur- explains the statistical analysis of the residuals that was used to bations they exert on the motion of other asteroids (called “test assign weights to, or reject observations. In Sect. 5 the results asteroids”). are presented and Sect. 6 discusses them. The usual procedure to calculate the mass of one aster- Throughout this paper, asteroid masses are expressed in units oid is, first, to identify potential test asteroids by searching −10 of 10 solar masses (M) and generally given to 3 decimal for close approaches with the perturbing asteroids and then places.