J/AJ/152/70   Outer Solar System Origins Survey (OSSOS). I.   (Bannister+, 2016)

The outer solar system origins survey. I. Design and first-quarter discoveries. Bannister M.T., Kavelaars J.J., Petit J.-M., Gladman B.J., Gwyn S.D.J., Chen Y.-T., Volk K., Alexandersen M., Benecchi S.D., Delsanti A., Fraser W.C., Granvik M., Grundy W.M., Guilbert-Lepoutre A., Hestroffer D., Ip W.-H., Jakubik M., Jones R.L., Kaib N., Kavelaars C.F., Lacerda P., Lawler S., Lehner M.J., Lin H.W., Lister T., Lykawka P.S., Monty S., Marsset M., Murray-Clay R., Noll K.S., Parker A., Pike R.E., Rousselot P., Rusk D., Schwamb M.E., Shankman C., Sicardy B., Vernazza P., Wang S.-Y. <Astron. J., 152, 70 (2016)> =2016AJ....152...70B 2016AJ....152...70B (SIMBAD/NED BibCode)
ADC_Keywords: Solar system ; Minor planets ; Magnitudes ; Surveys Keywords: Kuiper Belt: general - surveys Abstract: We report the discovery, tracking, and detection circumstances for 85 trans-Neptunian objects (TNOs) from the first 42deg2 of the Outer Solar System Origins Survey. This ongoing r-band solar system survey uses the 0.9deg2 field of view MegaPrime camera on the 3.6m Canada-France-Hawaii Telescope. Our orbital elements for these TNOs are precise to a fractional semimajor axis uncertainty <0.1%. We achieve this precision in just two oppositions, as compared to the normal three to five oppositions, via a dense observing cadence and innovative astrometric technique. These discoveries are free of ephemeris bias, a first for large trans-Neptunian surveys. We also provide the necessary information to enable models of TNO orbital distributions to be tested against our TNO sample. We confirm the existence of a cold "kernel" of objects within the main cold classical Kuiper Belt and infer the existence of an extension of the "stirred" cold classical Kuiper Belt to at least several au beyond the 2:1 mean motion resonance with Neptune. We find that the population model of Petit et al. remains a plausible representation of the Kuiper Belt. The full survey, to be completed in 2017, will provide an exquisitely characterized sample of important resonant TNO populations, ideal for testing models of giant planet migration during the early history of the solar system. Description: The Outer Solar System Origins Survey (OSSOS) observations are acquired in blocks: contiguous patches of sky formed by a layout of adjoining multiple 0.90deg2 MegaCam fields. The OSSOS discovery and tracking program uses the Canada-France-Hawaii Telescope (CFHT) MegaPrime/MegaCam. In 2013 and 2014, the MegaPrime/MegaCam focal plane was populated by thirty-six 4612*2048 pixel CCDs in a 4 by 9 arrangement, with a 0.96°*0.94° unvignetted Field Of View (FOV) (0.90deg2) and 0.05'' Full Width at Half Maximum (FWHM) Image Quality (IQ) variation between center and edge. The plate scale is 0.184'' per pixel, which is well suited for sampling the 0.7'' median seeing at Maunakea. We observed our 2013 discovery fields in MegaCam's r.MP9601 filter (564-685nm at 50% transmission; 81.4% mean transmission) which is similar to the Sloan Digital Sky Survey (SDSS) r' filter. Our integration length was set at 287s. This exposure length achieves a target depth of mr=24.5 in a single frame in 0.7'' median CFHT seeing. MegaPrime/MegaCam operates exclusively as a dark-time queue-mode instrument for CFHT. The OSSOS project thus has between 10 and 14 potentially observable nights each month, weather considerations aside. Through CFHT's flexible queue-schedule system we requested our observations be made in possibly non-photometric conditions (discussed in Section 3.5) with 0.6''-0.8'' seeing and <0.1mag extinction for discovery, and requested image quality of 0.8''-1.0'' seeing for follow-up observations. Images were taken entirely with sidereal guiding and above airmass 1.5. This aided the quality of the astrometric solution and the point-spread function, and retained image depth: median extinction on Maunakea is 0.10mag per airmass in this passband. This paper covers OSSOS blocks that had their discovery observations in 2013A (2013 is the year that the discovery observations were successfully made, and A indicates the half-year semester of discovery opposition; A for Northern spring). Forthcoming papers will cover the subsequent discovery observations. The 2013A blocks were 13AE, centered at R.A. 14h20m, decl. -12°52' at discovery, spanning ecliptic latitude range b=0°-3°, and 13AO, centered at R.A. 15h57m, decl. -12°30' at discovery, spanning ecliptic latitude range b=6°-9°. The sky locations of the 13A blocks are at 44° and 30° galactic latitude. The 13AE discovery triplets were taken under some minor (<0.04mag) extinction and with IQ that ranged from 0.65'' to 0.84''. The 13AO discovery triplets exhibited no extinction and IQ that ranged from 0.49'' to 0.74''. Subsequent imaging to track the discoveries was acquired through 2013 August. Not all discoveries were observed in every lunation due to objects falling in chip gaps or on background sources on some dates, faint magnitudes, or variable seeing in the recovery observations. In much of 2013, poor weather conditions prevented observations in sufficient IQ for us to recover the faintest objects. To compensate, from 2013 November onward we used alternative 387s exposures in 0.8±0.1'' seeing for single-image passes on the block. For the seven February-August lunations that the blocks were visible in 2014, the 13AE and 13AO discoveries brighter than the characterization limit (Section 5) were observed with pointed recoveries; this was possible because the high-frequency cadence in the discovery year shrank the ephemeris uncertainty to a tiny fraction of the MegaPrime FOV. A handful of fainter objects not immediately recovered in the first pointed recovery images were targeted with spaced triplets of observations in subsequent lunations until recovery was successful on all of them (Section 6.1). Generally, two observations per object per lunation were made. File Summary: -------------------------------------------------------------------------------- FileName Lrecl Records Explanations -------------------------------------------------------------------------------- ReadMe 80 . This file table4.dat 244 85 Orbit and discovery properties of the characterized Outer Solar System Origins Survey (OSSOS) objects table5.dat 244 19 Orbit and discovery properties of the uncharacterized Outer Solar System Origins Survey (OSSOS) objects -------------------------------------------------------------------------------- See also: B/astorb : Orbits of Minor Planets (Bowell+ 2014) J/A+A/546/A115 : Colors of minor bodies in outer solar system (Hainaut+, 2012) http://www.minorplanetcenter.net/iau/MPCORB.html : Public catalog at the MPC http://www.ossos-survey.org/ : OSSOS website Byte-by-byte Description of file: table[45].dat -------------------------------------------------------------------------------- Bytes Format Units Label Explanations -------------------------------------------------------------------------------- 1- 3 A3 --- Pop Orbital population (xxx, cen, sca, cla, res, or det) (1) 5 A1 --- n_Pop [Nimox] Population subgroup (N, i, m, o, x) (2) 7- 8 I2 --- j [2/18]?=-1 Object is in the j:k resonance 10- 11 I2 --- k [1/11]?=-1 Object is in the j:k resonance 13- 15 A3 --- sh Orbit classification status (I, H, S, or x) (3) 17- 24 A8 --- Object Object identifier (4) 26- 30 F5.2 mag [21.15/24.8] Cleaned mean magnitude during discovery (mr) 32- 36 F5.3 mag e_ [0.02/0.364] Uncertainty in 38 A1 --- Flt [r] Filter used in observation (r) (5) 40- 44 F5.2 mag HMag [5.27/12.9] Absolute magnitude H in Flt (Hr) 46- 51 F6.3 AU Dist [13.7/57.4] Object distance at discovery (6) 53- 57 F5.3 AU e_Dist [0/8.5] Uncertainty in Dist 59- 60 I2 --- Nobs [3/56] Number of observations 62- 68 F7.4 yr Time [0.0002/13.85] Length of measured orbital arc 70- 74 F5.3 arcsec [0.006/0.185] Mean orbit-fit residual, RA 76- 80 F5.3 arcsec [0/0.202] Mean orbit-fit residual, Dec 82- 86 F5.3 arcsec max-x [0.009/0.669] Maximum orbit-fit residual, RA 88- 92 F5.3 arcsec max-y [0.001/1.169] Maximum orbit-fit residual, Dec 94-103 F10.6 AU a [15.5/149.9] Semimajor axis (6) 105-111 F7.4 AU e_a [0.002/25.5] Uncertainty in a (7) 113-120 F8.6 --- e [0.012/0.76] Orbital eccentricity (6) 122-129 F8.6 --- e_e [0/0.94] Uncertainty in e (7) 131-136 F6.3 deg i [0.5/50.4] Inclination to the ecliptic (6) 138-143 F6.3 deg e_i [0/49.5] Uncertainty in i (7) 145-151 F7.3 deg Omega [25.2/229] Longitude of ascending node Ω 153-159 F7.3 deg e_Omega [0/166.5] Uncertainty in Omega 161-167 F7.3 deg omega [11.9/358.6] Argument of perihelion ω 169-176 F8.3 deg e_omega [0.003/1716.8] Uncertainty in omega 178-187 F10.3 d T0 [7912/107982] Modified Julian Date of perihelion passage 189-198 F10.3 d e_T0 [2/576875] Uncertainty in T0 200-205 F6.3 h RAh Hour of Right Ascension at mean equinox of discovery (J2000) 207-213 F7.3 deg DEdeg Declination in decimal degrees at mean equinox of discovery (J2000) 215-227 F13.5 d Mean Julian Date of discovery 229-232 F4.2 arcsec/h Motion [2.2/8.3] Angular rate of sky motion at discovery 234-238 F5.3 --- Deff [0.01/0.9] Value of the detection efficiency function for the motion rate and magnitude of the object at its discovery 240-244 F5.2 mag mlim [23.9/24.5] Limiting magnitude of discovery block -------------------------------------------------------------------------------- Note (1): Orbital population is defined as follows: xxx = Unclassified due to uncharacterized status; cen = Centaur; sca = Scattering disk object; cla = Classical belt; res = In mean-motion resonance; det = Detached object. Note (2): Population subgroup for resonant (resonance status is checked for outer planets) and classical objects is defined as follows: U = Uranus; N = Neptune; i = Inner main belt; m = Main belt; o = Outer main belt; x = No applicable population subgroup; X = Not checked due to uncharacterized status. Note (3): Orbit classification status is defined as follows: I = The orbit classification is currently insecure; H = The human operator intervened to declare the orbit security status; S = The orbit classification is secure; x = Unclassifiable due to uncharacterized status. Note (4): Survey designation here based on their OSSOS discovery, with a format: * u=uncharacterized, and o=Outer Solar System Origins Survey (OSSOS); * Last digit of the year in which the object was discovered by OSSOS (3-6); * The block ID letter: e=Centered at R.A. 14h20m, decl. -12°52' at discovery, spanning ecliptic latitude range b=0°-3°; o=Centered at R.A. 15h57m, decl. -12°30' at discovery, spanning ecliptic latitude range b=6°-9°; * And the sequential number 01-xx to give unique identifiers; * PD suffix = Previous Discovery. Some of the Trans-Neptunian Objects (TNOs) in the OSSOS discovery sample were previously discovered in other surveys: seven 13AE and one 13AO object link either to one-night observations from the Canada-France Ecliptic Plane Survey (CFEPS) survey (Jones et al. 2006Icar..185..508J 2006Icar..185..508J; Kavelaars et al. 2009AJ....137.4917K 2009AJ....137.4917K; Petit et al. 2011AJ....142..131P 2011AJ....142..131P), or to objects of varying arc length in the public catalog at the Minor Planet Center (MPC; http://www.minorplanetcenter.net/iau/MPCORB.html), providing arcs to objects first observed 9-13 years ago; * nt suffix = Not observed on more than two nights in the discovery lunation. The on-plane 13AE block contains more discoveries (49 Trans-Neptunian Objects) than in the higher-latitude 13AO block (36 TNOs), due to the cold classical Kuiper Belt's concentration in the plane. Note (5): We observed our 2013 discovery fields in MegaCam's r.MP9601 filter (564-685nm at 50% transmission; 81.4% mean transmission) which is similar to the Sloan Digital Sky Survey (SDSS) r' filter (see Section 3.5). Note (6): J2000 ecliptic barycentric coordinates. Full barycentric elements are available at http://www.ossos-survey.org/. The full heliocentric orbital elements are available in electronic form from the Minor Planet Center. Note (7): Uncertainties from the covariant matrix fit of Bernstein & Khushalani 2000AJ....120.3323B 2000AJ....120.3323B. -------------------------------------------------------------------------------- History: From electronic version of the journal
(End) Prepared by [AAS]; Sylvain Guehenneux [CDS] 26-Sep-2016
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