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Featured researches published by Bruno Sicardy.


Nature | 2011

A Pluto-like radius and a high albedo for the dwarf planet Eris from an occultation

Bruno Sicardy; Jose Luis Ortiz; M. Assafin; Emmanuel Jehin; A. Maury; E. Lellouch; R. Gil Hutton; F. Braga-Ribas; François Colas; Daniel Hestroffer; J. Lecacheux; F. Roques; P. Santos-Sanz; Thomas Widemann; N. Morales; R. Duffard; A. Thirouin; A. J. Castro-Tirado; Martin Jelinek; Petr Kubánek; A. Sota; R. Sánchez-Ramírez; Alexandre Humberto Andrei; J. I. B. Camargo; D. N. da Silva Neto; A. Ramos Gomes; R. Vieira Martins; Michaël Gillon; Jean Manfroid; G. P. Tozzi

The dwarf planet Eris is a trans-Neptunian object with an orbital eccentricity of 0.44, an inclination of 44 degrees and a surface composition very similar to that of Pluto. It resides at present at 95.7 astronomical units (1 au is the Earth-Sun distance) from Earth, near its aphelion and more than three times farther than Pluto. Owing to this great distance, measuring its size or detecting a putative atmosphere is difficult. Here we report the observation of a multi-chord stellar occultation by Eris on 6 November 2010 ut. The event is consistent with a spherical shape for Eris, with radius 1,163 ± 6 kilometres, density 2.52 ± 0.05 grams per cm3 and a high visible geometric albedo, . No nitrogen, argon or methane atmospheres are detected with surface pressure larger than ∼1 nanobar, about 10,000 times more tenuous than Plutos present atmosphere. As Plutos radius is estimated to be between 1,150 and 1,200 kilometres, Eris appears as a Pluto twin, with a bright surface possibly caused by a collapsed atmosphere, owing to its cold environment. We anticipate that this atmosphere may periodically sublimate as Eris approaches its perihelion, at 37.8 astronomical units from the Sun.


Nature | 2014

A ring system detected around the Centaur (10199) Chariklo

F. Braga-Ribas; Bruno Sicardy; Jose Luis Ortiz; C. Snodgrass; F. Roques; R. Vieira-Martins; J. I. B. Camargo; M. Assafin; R. Duffard; Emmanuel Jehin; J. Pollock; R. Leiva; M. Emilio; D. I. Machado; C. Colazo; E. Lellouch; J. Skottfelt; Michaël Gillon; N. Ligier; L. Maquet; G. Benedetti-Rossi; A. Ramos Gomes; P. Kervella; H. Monteiro; R. Sfair; M. El Moutamid; Gonzalo Tancredi; J. Spagnotto; A. Maury; N. Morales

Hitherto, rings have been found exclusively around the four giant planets in the Solar System. Rings are natural laboratories in which to study dynamical processes analogous to those that take place during the formation of planetary systems and galaxies. Their presence also tells us about the origin and evolution of the body they encircle. Here we report observations of a multichord stellar occultation that revealed the presence of a ring system around (10199) Chariklo, which is a Centaur—that is, one of a class of small objects orbiting primarily between Jupiter and Neptune—with an equivalent radius of 124  9 kilometres (ref. 2). There are two dense rings, with respective widths of about 7 and 3 kilometres, optical depths of 0.4 and 0.06, and orbital radii of 391 and 405 kilometres. The present orientation of the ring is consistent with an edge-on geometry in 2008, which provides a simple explanation for the dimming of the Chariklo system between 1997 and 2008, and for the gradual disappearance of ice and other absorption features in its spectrum over the same period. This implies that the rings are partly composed of water ice. They may be the remnants of a debris disk, possibly confined by embedded, kilometre-sized satellites.


Nature | 2012

Albedo and atmospheric constraints of dwarf planet Makemake from a stellar occultation

J. L. Ortiz; Bruno Sicardy; F. Braga-Ribas; A. Alvarez-Candal; E. Lellouch; R. Duffard; N. Pinilla-Alonso; V. D. Ivanov; S. P. Littlefair; J. I. B. Camargo; M. Assafin; E. Unda-Sanzana; Emmanuel Jehin; N. Morales; Gonzalo Tancredi; R. Gil-Hutton; I. de La Cueva; J. P. Colque; D. N. da Silva Neto; Jean Manfroid; A. Thirouin; Pedro J. Gutierrez; J. Lecacheux; Michaël Gillon; A. Maury; F. Colas; J. Licandro; T. Mueller; C. Jacques; D. Weaver

Pluto and Eris are icy dwarf planets with nearly identical sizes, comparable densities and similar surface compositions as revealed by spectroscopic studies. Pluto possesses an atmosphere whereas Eris does not; the difference probably arises from their differing distances from the Sun, and explains their different albedos. Makemake is another icy dwarf planet with a spectrum similar to Eris and Pluto, and is currently at a distance to the Sun intermediate between the two. Although Makemake’s size (1,420 ± 60 km) and albedo are roughly known, there has been no constraint on its density and there were expectations that it could have a Pluto-like atmosphere. Here we report the results from a stellar occultation by Makemake on 2011 April 23. Our preferred solution that fits the occultation chords corresponds to a body with projected axes of 1,430 ± 9 km (1σ) and 1,502 ± 45 km, implying a V-band geometric albedo pV = 0.77 ± 0.03. This albedo is larger than that of Pluto, but smaller than that of Eris. The disappearances and reappearances of the star were abrupt, showing that Makemake has no global Pluto-like atmosphere at an upper limit of 4–12 nanobar (1σ) for the surface pressure, although a localized atmosphere is possible. A density of 1.7 ± 0.3 g cm−3 is inferred from the data.


The Astrophysical Journal | 2013

THE SIZE, SHAPE, ALBEDO, DENSITY, AND ATMOSPHERIC LIMIT OF TRANSNEPTUNIAN OBJECT (50000) QUAOAR FROM MULTI-CHORD STELLAR OCCULTATIONS

F. Braga-Ribas; Bruno Sicardy; Jose Luis Ortiz; E. Lellouch; Gonzalo Tancredi; J. Lecacheux; R. Vieira-Martins; J. I. B. Camargo; M. Assafin; R. Behrend; Frederic Vachier; F. Colas; N. Morales; A. Maury; M. Emilio; A. Amorim; E. Unda-Sanzana; S. Roland; Sebastian Bruzzone; L. A. Almeida; C. V. Rodrigues; C. Jacques; R. Gil-Hutton; Leonardo Vanzi; A. Milone; W. Schoenell; Rachele Di Salvo; L. Almenares; Emmanuel Jehin; Jean Manfroid

We present results derived from the first multi-chord stellar occultations by the transneptunian object (50000) Quaoar, observed on 2011 May 4 and 2012 February 17, and from a single-chord occultation observed on 2012 October 15. If the timing of the five chords obtained in 2011 were correct, then Quaoar would possess topographic features (crater or mountain) that would be too large for a body of this mass. An alternative model consists in applying time shifts to some chords to account for possible timing errors. Satisfactory elliptical fits to the chords are then possible, yielding an equivalent radius Requiv = 555±2.5 km and geometric visual albedo pV = 0.109±0.007. Assuming that Quaoar is a Maclaurin spheroid with an indeterminate polar aspect angle, we derive a true oblateness of � = 0.087 +0.0268 −0.0175 , an equatorial radius of 569 +2417 km, and a density of 1.99 ± 0.46 g cm −3 . The orientation of our preferred solution in the plane of the sky implies that Quaoar’s satellite Weywot cannot have an equatorial orbit. Finally, we detect no global atmosphere around Quaoar, considering a pressure upper limit of about 20 nbar for a pure methane atmosphere.


Icarus | 1987

Oblateness, radius, and mean stratospheric temperature of Neptune from the 1985 August 20 occultation

William B. Hubbard; Philip D. Nicholson; E. Lellouch; Bruno Sicardy; Andre Brahic; Faith Vilas; P. Bouchet; Robert Alexander McLaren; Robert L. Millis; Lawrence H. Wasserman; J.H. Elias; Keith Y. Matthews; J.D. McGill; C. Perrier

Abstract The occultation of a bright ( K ∼6) infrared star by Neptune revealed a central flash at two stations and provided accurate measurements of the limb position at these and several additional stations. We have fitted this data ensemble with a general model of an oblate atmosphere to deduce the oblateness e and equatorial radius a 0 of Neptune at the 1-μbar pressure level, and the position angle p n of the projected spin axis. The results are e =0.0209±0.0014, a 0 =25269±10 km, p n =20.1°±1°. Parameters derived from fitting to the limb data alone are in excellent agreement with parameters derived from fitting to central flash data alone (E. Lellouch, W.B. Hubbard, B. Sicardy, F. Vilas, and P. Bouchet, 1986, Nature 324, 227–231) , and the principal remaining source of uncertainty appears to be the Neptune-centered declination of the Earth at the time of occultation. As an alternative to the methane absorption model proposed by Lellouch et al ., we explain an observed reduction in the central flash intensity by a decrease in temperature from 150 to 135°K as the pressure rises from 1 to 400 μbar. Implications of the oblateness results for Neptune interior models are briefly discussed.


The Astronomical Journal | 2016

THE OUTER SOLAR SYSTEM ORIGINS SURVEY. I. DESIGN AND FIRST-QUARTER DISCOVERIES

Michele T. Bannister; J. J. Kavelaars; Jean-Marc Petit; Brett James Gladman; Stephen Gwyn; Ying-Tung Chen; Kathryn Volk; Mike Alexandersen; Susan D. Benecchi; A. Delsanti; Wesley C. Fraser; Mikael Granvik; William M. Grundy; A. Guilbert-Lepoutre; Daniel Hestroffer; Wing-Huen Ip; Marian Jakubik; R. Lynne Jones; Nathan A. Kaib; Catherine F. Kavelaars; Pedro Lacerda; S. M. Lawler; M. J. Lehner; Hsing-Wen Lin; Tim Lister; Patryk Sofia Lykawka; Stephanie Monty; Michael Marsset; Ruth A. Murray-Clay; Keith S. Noll

National Research Council of Canada; National Science and Engineering Research Council of Canada; Academia Sinica Postdoctoral Fellowship


Celestial Mechanics and Dynamical Astronomy | 2004

STATIONARY CONFIGURATIONS FOR CO-ORBITAL SATELLITES WITH SMALL ARBITRARY MASSES

Stéfan Renner; Bruno Sicardy

We derive general results on the existence of stationary configurations for N co-orbital satellites with small but otherwise arbitrary masses mi, revolving on circular and planar orbits around a massive primary. The existence of stationary configurations depends on the parity of N. If N is odd, then for any arbitrary angular separation between the satellites, there always exists a set of masses (positive or negative) which achieves stationarity. However, physically acceptable solutions (mi > 0 for all i) restrict this existence to sub-domains of angular separations. If N is even, then for given angular separations of the satellites, there is in general no set of masses which achieves stationarity. The case N=3 is treated completely for small arbitrary satellite masses, giving all the possible solutions and their stability, to within our approximations.


Icarus | 1982

The upper atmosphere of Uranus: A critical test of isotropic turbulence models

Richard G. French; James L. Elliot; Bruno Sicardy; Philip D. Nicholson; Keith Matthews

Abstract Observations of the 15 August 1980 Uranus occultation of KM 12, obtained from Cerro Tololo InterAmerican Observatory, European Southern Observatory, and Cerro Las Campanas Observatory, are used to compare the atmospheric structure at points separated by ∼140 km along the planetary limb. The results reveal striking, but by no means perfect, correlation of the light curves, ruling out isotropic turbulence as the cause of the light curve spikes. The atmosphere is strongly layered, and any acceptable turbulence model must accommodate the axial ratios of ⪆60 which are observed. The mean temperature of the atmosphere is 150 ± 15°K for the region near number density 10 14 cm −3 . Derived temperature variations of vertical scale ∼ 130km and amplitude ±5°K are in agreement for all stations, and correlated spikes correspond to low-amplitude temperature variations with a vertical scale of several kilometers.


The Astrophysical Journal | 2015

PLUTO's ATMOSPHERE FROM STELLAR OCCULTATIONS IN 2012 AND 2013 *

Alex Dias-Oliveira; Bruno Sicardy; E. Lellouch; R. Vieira-Martins; M. Assafin; J. I. B. Camargo; F. Braga-Ribas; A. R. Gomes-Júnior; G. Benedetti-Rossi; F. Colas; A. Decock; A. Doressoundiram; Christophe Dumas; M. Emilio; J. Fabrega Polleri; R. Gil-Hutton; Michaël Gillon; J. H. Girard; George K. T. Hau; V. D. Ivanov; Emmanuel Jehin; J. Lecacheux; R. Leiva; C. Lopez-Sisterna; L. Mancini; Jean Manfroid; A. Maury; Erick Meza; N. Morales; L. Nagy

A. Dias-Oliveira is thankful for the support of the following grants: CAPES (BEX 9110/12-7) FAPERJ/PAPDRJ (E-45/2013). R. Vieira-Martins acknowledges the following grants: CNPq-306885/2013, CAPES/Cofecub-2506/2015, FAPERJ/PAPDRJ-45/2013. TRAPPIST is a project funded by the Belgian Fund for Scientific Research (F.R.S.-FNRS) under grant FRFC 2.5.594.09.F, with the participation of the Swiss National Science Foundation. J. L. Ortiz and N. Morales acknowledge funding from Proyecto de Excelencia de la Junta de Andalucia, J.A. 2012-FQM1776 and from FEDER funds. M. Gillon and E. Jehin are F.R.S.-FNRS Research Associates. C. Opitom acknowledges the support of the F.R.S.-FNRS for her PhD thesis. R. Leiva is supported by the CONICYT PCHA/Doctorado Nacional scholarship. M. Assafin thanks the CNPq (Grants 473002/2013-2 and 308721/2011-0) and FAPERJ (Grant E-26/111.488/2013). J.I.B. Camargo acknowledges CNPq for a PQ2 fellowship (process number 308489/2013-6). A.R. Gomes-Junior thanks CAPES.


Astronomy and Astrophysics | 2015

Orbit determination of trans-Neptunian objects and Centaurs for the prediction of stellar occultations

J. Desmars; J. I. B. Camargo; F. Braga-Ribas; R. Vieira-Martins; M. Assafin; Frederic Vachier; Florent Colas; J. L. Ortiz; R. Duffard; N. Morales; Bruno Sicardy; A. R. Gomes-Júnior; G. Benedetti-Rossi

Context. The prediction of stellar occultations by trans-Neptunian objects (TNOs) and Centaurs is a difficult challenge that requires accuracy both in the occulted star position and in the object ephemeris. Until now, the most used method of prediction, involving dozens of TNOs/Centaurs, has been to consider a constant offset for the right ascension and for the declination with respect to a reference ephemeris, usually the latest public version. This offset is determined as the difference between the most recent observations of the TNO/Centaur and the reference ephemeris. This method can be successfully applied when the offset remains constant with time, i.e. when the orbit is stable enough. In this case, the prediction even holds for occultations that occur several days after the last observations. Aims: This paper presents an alternative method of prediction, based on a new accurate orbit determination procedure, which uses all the available positions of the TNO from the Minor Planet Center database, as well as sets of new astrometric positions from unpublished observations. Methods: Orbits were determined through a numerical integration procedure called NIMA, in which we developed a specific weighting scheme that considers the individual precision of the observation, the number of observations performed during one night by the same observatory, and the presence of systematic errors in the positions. Results: The NIMA method was applied to 51 selected TNOs and Centaurs. For this purpose, we performed about 2900 new observations in several observatories (European South Observatory, Observatorio Pico dos Dias, Pic du Midi, etc.) during the 2007-2014 period. Using NIMA, we succeed in predicting the stellar occultations of 10 TNOs and 3 Centaurs between July 2013 and February 2015. By comparing the NIMA and Jet Propulsion Laboratory (JPL) ephemerides, we highlight the variation in the offset between them with time, by showing that, generally, the constant offset hypothesis is not valid, even for short time scales of a few weeks. Giving examples, we show that the constant offset method cannot accurately predict 6 out of the 13 observed positive occultations that have been successfully predicted by NIMA. The results indicate that NIMA is capable of efficiently refining the orbits of these bodies. Finally, we show that the astrometric positions given by positive occultations can help to refine the orbit of the TNO and, consequently, the future predictions. We also provide unpublished observations of the 51 selected TNOs and their ephemeris in a usable format by the SPICE library. We provide ephemerides of TNO/Centaurs usable with SPICE library and available at http://www.imcce.fr/~desmars/research/tno/The offset observations of the selected TNOs are only available at the CDS via anonymous ftp to http://cdsarc.u-strasbg.fr (ftp://130.79.128.5) or via http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/584/A96

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M. Assafin

Federal University of Rio de Janeiro

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N. Morales

Spanish National Research Council

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J. L. Ortiz

Spanish National Research Council

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R. Duffard

Spanish National Research Council

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R. Vieira-Martins

Federal University of Rio de Janeiro

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