MNRAS000,1–9(2016) Preprint26January2017 CompiledusingMNRASLATEXstylefilev3.0 Precise CCD positions of Himalia using Gaia DR1 in 2015-2016 H. W. Peng,1,2,3,4 Q. Y. Peng1,4⋆ and N. Wang1,4 1Department of Computer Science, Jinan University,Guangzhou 510632, China 2Yunnan Observatories, Chinese Academy of Sciences, Kunming 650216, China 3Universityof Chinese Academy of Sciences,Beijing 100049, China 7 4Sino-French Joint Laboratory for Astrometry, Dynamicsand Space Science, Jinan University,Guangzhou 510632, China 1 0 2 Accepted2017January24.Received2017January19;inoriginalform2016October17 n a J ABSTRACT 5 Inorderto obtainhighprecisionCCD positions ofHimalia,the sixthJoviansatellite, 2 a total of 598 CCD observations have been obtained during the years 2015-2016.The observationsweremadebyusingthe2.4mand1mtelescopesadministeredbyYunnan ] P Observatories over 27 nights. Several factors which would influence the positional E precision of Himalia were analyzed, including the reference star catalogue used, the . geometric distortion and the phase effect. By taking advantage of its unprecedented h positional precision, the recently released catalogue Gaia DR1 was chosen to match p reference stars in the CCD frames of both Himalia and open clusters which were - o observed for deriving the geometric distortion. The latest version of SOFA library r was used to calculate the positions of reference stars. The theoretical positions of t s Himalia were retrieved from the Jet Propulsion Laboratory Horizons System which a includes the satellite ephemeris JUP300, while the positions of Jupiter were based [ on the planetary ephemeris DE431. Our results showed that the means of observed 1 minus computed (O-C) residuals are 0.071 and -0.001 arcsec in right ascension and v declination,respectively.Theirstandarddeviationsareestimatedatabout0.03arcsec 2 in each direction. 4 Key words: astrometry – planets and satellites: individual: Himalia – methods: 1 observational– techniques: image processing 7 0 . 1 0 7 1 INTRODUCTION servationsofirregularsatellitescanalsobeusedforimprov- 1 ingthe ephemeridesof their host planets. The irregular satellites in our solar system have been stud- : v ied for many years. Parts of them may be formed follow- Himaliaisthelargest memberofJovianirregularsatel- i X ing with their host giant planets. However, some of these lites (Grav et al. 2015). It has been discovered by Perrine objects are widely believed to have been heliocentric as- at Lick Observatory in 1904 (Perrine 1905). The astromet- r a teroids before being captured by a giant planet’s gravity ricobservationsofHimaliawereobtainedcontinuouslysince (Colombo & Franklin 1971; Heppenheimer & Porco 1977; then.TheprecisionofpositionsofHimaliawasalsoimproved Pollacketal.1979;Sheppard&Jewitt2003;Agnor&Hamil- steadily with the time after larger diameter telescopes and ton2006;Nesvorny´etal.2007,2014).Thismeanstheirreg- newastrometricdataprocessingtechniqueswereused.Thus ular satellites may have close relationship with the forma- two medium size telescopes which are the 2.4 m telescope tionofearlysolarsystem.Theyaresmallerandfarther,and (Fan et al. 2015) and 1 m telescope (Zhou et al. 2001) ad- havinghighly eccentricand inclined orbitsthan theregular ministeredbyYunnanObservatorieswereusedforobtaining satellites (Nicholson 2008; Grav et al. 2015).The astromet- our CCD observations. For the data processing, in order to ric observationsof irregular satellites are also more difficult obtainhighprecisionresults,severalfactorsweretakeninto tobeobtainedwithhighprecision.Untilnow,thoughmany account. Specifically, the reference star catalogue used, the space missions have had close flyby, observations made by geometricdistortion(calledGDhereafter)andthephaseef- ground-based telescopes could still be the primary way to fect, etc. The latest version of software routines from the studyirregularsatellites.Thehighprecisionastrometricob- IAU-SOFA(InternationalAstronomicalUnion-Standardsof FundamentalAstronomy)collection(Hohenkerk2015)were used for calculating the topocentric apparent positions of ⋆ E-mail:[email protected] referencestars.OurpreviouslyproposedGDsolution(Peng (cid:13)c 2016TheAuthors 2 H. W. Peng et al. etal.2012)wasusedforderivingtheGDpatterns.TheGD Table 1.Specifications of the 2.4 m and 1 m telescopes admin- effects of the 2.4 m and 1 m telescopes have been proved istered by Yunnan Observatories and the corresponding CCD in our previous works (Peng et al. 2012, 2015; Zhang et detectors. Column 1 shows the parameters and the following al. 2012; Wang et al. 2015; Peng et al. 2016). In consid- columnslisttheirvaluesforthetwotelescopes. eration of the fewer numberof reference stars in each CCD frame of Himalia, the high-order plate model can’t be ap- Parameters 2.4m 1m plied. In some cases, there are only several reference stars Approximatefocallength 1920cm 1330cm available in the CCD field of view, and a plate model with F-Ratio 8 13 four constants becomes the most reasonable choice. Under Diameterofprimarymirror 240cm 100cm this circumstance, the GD effects should be corrected ac- CCDfieldofview(effective) 9′×9′ 7′×7′ curately. Furthermore, the phase effect of Himalia was also SizeofCCDarray(effective) 1900×1900 2048×2048 analyzed (Lindegren 1977). Sizeofpixel 13.5m ×13.5m 13.5m ×13.5m Asiswell known,theprecision ofareferencestarcata- Approximatescalefactor 0.286′′/pixel 0.209′′/pixel logueisessentialtothemeasurementsofirregularsatellites. Furthermore, the zonal errors of a star catalogue also have direct influence on the positional precision. The astrome- try satellite Gaia (Gaia Collaboration et al. 2016a) which Table 2.CCD observations of Himaliaand calibrationfields by is fully funded by the European Space Agency (ESA) has using the 2.4 m and 1 m telescopes administered by Yunnan been launched on December 19, 2013. After less than three Observatories. Column 1 lists the observational dates. Column years, the first catalogue Gaia Data Release 1 (Gaia DR1) 2showstheopenclustersobserved.Column3andColumn4list (GaiaCollaboration etal.2016b)waspublishedonSeptem- thenumberofobservationsforopenclustersandHimalia,respec- ber14,2016. TheprecisestarpositionsderivedbytheGaia tively.TheJohnson-I filterwasusedinallobservations.Column could render better predictions with the primary source of 5showswhichtelescopewasused. errorbeingtheephemerides(deBruijne2012;Gomes-Ju´nior et al. 2015). Though the final mission products are waiting Obsdates Calibrationfields Himalia Tel to be released in the future, the results of Gaia DR1 still openclusters No. No. represent a huge improvementin theavailable fundamental 2015-01-31 NGC1664 44 21 2.4m stellar data and practical definition of the optical reference 2015-02-07 NGC2324 44 25 2.4m frame (Lindegren et al. 2016). We believe that the higher 2015-02-08 NGC2324 44 14 2.4m positional precision of targets will be achieved. 2015-02-09 NGC2324 44 18 2.4m The contents of this paper are arranged as follows. 2015-02-10 NGC1664 44 18 2.4m In Section 2, the CCD observations are described. Section 2015-02-11 19 2.4m 3 presents the reduction details. In Section 4, results are 2015-02-12 17 2.4m showed. In Section 5, discussions are made. Finally, in Sec- 2015-02-13 19 2.4m tion 6, conclusions are drawn. 2015-02-12 M35 60 14 1m 2015-02-14 20 1m 2016-03-01 M35 49 36 1m 2016-03-02 M35 49 30 1m 2 CCD OBSERVATIONS 2016-03-03 M35 49 41 1m 2016-03-04 M35 49 51 1m Atotalof27nightsofCCDobservationsofHimaliawereob- 2016-03-06 20 2.4m tained from two telescopes administered by YunnanObser- 2016-03-08 18 2.4m vatoriesduringtheyears2015-2016.Theobservationaldates 2016-03-09 20 2.4m werechosenaccordingtotheepochswhenJupiterisnearits 2016-03-10 3 2.4m 2016-03-11 NGC6633 44 23 2.4m opposition.Specifically,19nightsofCCDobservationswere 2016-03-12 21 2.4m made by the YunnanFaint Object Spectrograph and Cam- 2016-03-13 21 2.4m era (YFOSC) instrument attached to the 2.4 m telescope 2016-03-14 24 2.4m (longitude E 100◦1′51′′, latitude N 26◦42′32′′, height 3193 2016-03-15 23 2.4m m above sea level), and 9 nights of CCD observations were 2016-03-16 22 2.4m madebythe1mtelescope(longitudeE102◦47′18′′,latitude 2016-03-17 20 2.4m N 25◦1′46′′,height 2000 m abovesealevel). It isnoted that 2016-04-07 14 1m observations were obtained from both the 2.4 m and 1 m 2016-04-09 M67 35 11 1m telescopes on February 12, 2015. The specifications of the 2016-04-10 M67 44 15 1m two telescopes and corresponding CCD detectors are listed Total 599 598 in Table 1. A total of 598 CCD observations of Himalia have been obtained, as well as 599 CCD frames of calibration fields which are open clusters. Distributions of the observations withrespecttotheobservationaldatesarelistedinTable2. 120secondsdependingonthetelescopesandmeteorological It can be seen that 366 CCD observations of Himalia were conditions. Calibration fields were observed following with obtained from the 2.4 m telescope, and 232 CCD observa- Himalia,exceptforthosenightsthatobservationsweresub- tionsofHimalia wereobtainedfrom the1mtelescope. The jected to rapidly changing weather conditions and limited exposure time for each CCD frame is ranged from 20 to telescope time. MNRAS000,1–9(2016) Precise CCD positions of Himalia using Gaia DR1 3 2015-01-31 Med =0.29 Max=2.08 2015-02-10 Med =0.31 Max=2.06 2016-03-11 Med =0.33 Max=2.23 2000 2000 2000 1500 1500 1500 el el el x1000 x1000 x1000 pi pi pi Y/ Y/ Y/ 500 500 500 0 0 0 0 500 1000 1500 2000 0 500 1000 1500 2000 0 500 1000 1500 2000 X/pixel X/pixel X/pixel 2015-02-12 Med =0.21 Max=0.45 2016-03-01 Med =0.20 Max=0.46 2016-04-10 Med =0.21 Max=0.51 2000 2000 2000 1500 1500 1500 el el el x x x pi1000 pi1000 pi1000 Y/ Y/ Y/ 500 500 500 0 0 0 0 500 1000 1500 2000 0 500 1000 1500 2000 0 500 1000 1500 2000 X/pixel X/pixel X/pixel Figure 1. GD patterns for the 2.4 m and 1 m telescopes administered by Yunnan Observatories using catalogue Gaia DR1. Only six typicalGDpatternsareshowed.TheupperthreepanelsshowtheGDpatternsderivedfromtheCCDobservationsofthe2.4mtelescope. Thelower threepanels show the GD patterns derivedfromthe CCDobservations of the1m telescope. Allobservations wereobtained with the Johnson-I filter. In each panel, the observational date, the median and maximum GD values are listed on the top in units of pixels.Afactorof200isusedtoexaggeratethemagnitudeofeachGDvector. 3 ASTROMETRIC REDUCTION cataloguewaschosentomatchreferencestarsinalltheCCD frames. Thereductionprocedureswerecarried outaccordingtoour InordertoobtaintheobservationalpositionsofHimalia previouswork(Pengetal.2012).Firstly,alltheCCDframes andalsotoderivetheGDpatterns,thetopocentricapparent wereprocessedtoobtainthepixelpositionsofbothHimalia positionsofreferencestarsinalltheCCDframesneedtobe andreferencestars.Secondly,theGDpatternswerederived calculated. In this work, the latest version of software rou- fromtheCCDframesofopenclusters.Thirdly,theGDcor- tinesfromtheIAU-SOFAcollection (Hohenkerk2015)were rections were applied for both Himalia and reference stars. used to compute the topocentric apparent positions. How- Atlast,thetopocentricapparentpositionsofHimaliacould ever, the catalogue Gaia DR1 does provide parallaxes only be obtained with respect to the reference stars in the same forTychostars.Thusonlythesereferencestarswereapplied CCD field of view. More description follows. withbothparallaxesandaberration correctionsintopocen- tric correction. The other reference stars were applied with Before the data reduction, there are several preprocess aberration correction, only. steps need to be accomplished. As showed in Section 2, several open clusters were observed for the purpose of de- After the positional computations of reference stars in riving GD patterns. These CCD frames together with the theCCDframesofopenclusterswerefinished,theGDpat- CCDframesofHimaliawerefirstlyprocessedwithbiasand terns could be derived according to the solution presented flat-field corrections. Then the CCD frames obtained from in our previous work (Peng et al. 2012). For the purpose the 2.4 m telescope were clipped into 1900×1900 square of derivingGD patternsaccurately, theatmospheric refrac- pixels because they have ineffective boundaries which have tion effect should be added to the positional computations non-exposure pixels. Next, the pixel positions of both Hi- ofreferencestars. Astandardatmosphericrefraction model malia and reference stars were obtained by using the two- should be precise enough (Peng et al. 2012). According to dimensional Gaussian fit algorithm. Lastly, a reference star thestudypresentedinStone(2002),thefiltersusedandob- MNRAS000,1–9(2016) 4 H. W. Peng et al. servationalzenithdistanceareimportantforcomputingthe Table 3. Statistics on the (O-C) residuals of positions of Hi- differentialcolor refraction (DCR).In ourobservations, the malia.ThecatalogueGaiaDR1wasused.Column1andcolumn Johnson-I filter was used, and the average of observational 2 show the observational dates and GD corrections. The follow- zenithdistancesisabout25degrees.Undersuchconditions, ingcolumnslistthemeansof(O-C)residualsandtheirstandard theDCRisinsomedegreenegligibleaccordingtothestudy deviations (SDs)inrightascensionanddeclination, respectively. presented in Stone (2002). Thus the DCR for our observa- Allunitsareinarcseconds. tions was not taken into account in the refraction model. Fig. 1 shows six typical GD patterns derived by using the Obsdates GDC hO-Ci SD hO-Ci SD andTel RA DEC star catalogue Gaia DR1. It can be seen that the GD ef- fects of the 1 m telescope are much smaller than the 2.4 m 2015-01-31 Before 0.064 0.065 -0.032 0.059 telescope. (2.4m) After 0.061 0.021 0.003 0.019 TheGDcorrectionswereappliedforthepixelpositions 2015-02-07 Before 0.044 0.037 -0.003 0.055 ofbothHimaliaandreferencestarsinthesameCCDfieldof (2.4m) After 0.036 0.011 0.020 0.016 view.Inpractice,GDcorrectionswereappliedoneachnight 2015-02-08 Before -0.012 0.076 -0.032 0.028 (2.4m) After 0.054 0.020 0.021 0.030 if the GD pattern is available, otherwise the GD pattern of 2015-02-09 Before -0.002 0.050 -0.042 0.058 nearest night is used(Penget al. 2016).More details about (2.4m) After 0.057 0.013 0.012 0.014 the different GD correction schemes are presented in our 2015-02-10 Before 0.050 0.078 -0.016 0.033 previouswork(Wangetal.2015).AftertheGDcorrections (2.4m) After 0.041 0.014 0.024 0.021 werefinished,thetopocentricapparentpositionsofreference 2015-02-11 Before 0.000 0.064 -0.014 0.036 starswerecalculated.TheobservationalpositionsofHimalia (2.4m) After 0.050 0.016 0.024 0.021 were computed relative to these reference stars in the same 2015-02-12 Before 0.014 0.071 0.009 0.075 CCD field of view. A plate model with four constants was (2.4m) After 0.061 0.012 0.020 0.023 used for the computations. However, this is accurate only 2015-02-13 Before 0.022 0.081 -0.047 0.063 after all the astrometric effects, including the GD effects, (2.4m) After 0.068 0.012 0.012 0.017 2015-02-12 Before 0.040 0.046 -0.029 0.012 are taken intoaccount (Penget al. 2012). (1m) After 0.063 0.045 -0.003 0.011 According to the illustration presented in Linde- 2015-02-14 Before 0.054 0.027 0.014 0.035 gren (1977), the phase effect has a direct influence on posi- (1m) After 0.075 0.028 0.013 0.034 tionalmeasurementsofplanetsandnaturalsatellites in our 2016-03-01 Before 0.051 0.053 -0.092 0.045 solar system. Phase corrections should be considered and (1m) After 0.054 0.026 -0.024 0.043 applied for these objects. Though our observational dates 2016-03-02 Before 0.071 0.014 0.023 0.011 were selected near Jupiter’s opposition, the phase effect of (1m) After 0.067 0.014 -0.013 0.010 Himalia isstill calculated. Asan irregular satellite, Himalia 2016-03-03 Before 0.082 0.034 0.030 0.026 maybefarfrom beingasphere,whilethisisan implicitas- (1m) After 0.074 0.031 0.002 0.026 sumption in Lindegren (1977). Under the assumption that 2016-03-04 Before 0.070 0.017 -0.038 0.013 (1m) After 0.077 0.012 -0.014 0.011 Himalia is a sphere, the phase effect of Himalia was calcu- 2016-03-06 Before 0.000 0.010 0.056 0.019 lated byusingequation(14) presentedinLindegren(1977). (2.4m) After 0.074 0.010 -0.006 0.019 Severaltypicalobservationaltimewereselected tocompute 2016-03-08 Before 0.064 0.019 -0.116 0.039 thephaseeffects.Ourresultsshowthatthemaximumvalue (2.4m) After 0.066 0.018 0.006 0.039 of phase effects according to the observational time is as 2016-03-09 Before 0.155 0.049 -0.058 0.042 smallas∼0.002′′,andmostofthephaseeffectsarelessthan (2.4m) After 0.061 0.051 0.007 0.044 0.001′′. These values are beyond our measurable precision 2016-03-10 Before 0.129 0.023 -0.154 0.061 limitation. It means the phase effect of Himalia for our ob- (2.4m) After 0.095 0.003 -0.021 0.058 servations is negligible. 2015-03-11 Before -0.036 0.038 0.036 0.019 (2.4m) After 0.089 0.038 -0.015 0.016 2016-03-12 Before 0.090 0.012 -0.097 0.018 (2.4m) After 0.072 0.010 -0.003 0.018 4 RESULTS 2016-03-13 Before -0.006 0.033 -0.078 0.035 (2.4m) After 0.078 0.037 0.000 0.034 In this work, the reference star catalogue Gaia DR1 (Gaia 2016-03-14 Before 0.128 0.042 -0.041 0.038 Collaboration et al. 2016b) was used in the astrometric (2.4m) After 0.085 0.037 -0.024 0.043 data reduction. The observed positions of Himalia were 2016-03-15 Before 0.204 0.040 -0.042 0.042 compared to the ephemeris retrieved from Jet Propulsion (2.4m) After 0.100 0.040 -0.014 0.039 Laboratory (JPL) Horizons ephemeris service (Giorgini et 2016-03-16 Before 0.056 0.015 -0.010 0.021 (2.4m) After 0.091 0.015 0.013 0.021 al.1996)whichincludesthesatelliteephemerisJUP300(Ja- 2016-03-17 Before 0.092 0.009 -0.072 0.009 cobson 2013) and planetary ephemeris DE431 (Folkner et (2.4m) After 0.054 0.008 0.000 0.010 al. 2014). Fig. 2 shows the (O-C) residuals of positions of 2016-04-07 Before 0.106 0.037 0.004 0.032 Himalia with respect to the Julian Dates. Table 3 lists the (1m) After 0.111 0.029 -0.009 0.034 statisticsonthe(O-C)residualsforHimaliabeforeandafter 2016-04-09 Before 0.078 0.006 -0.055 0.012 GD corrections. It can be seen that the internal agreement (1m) After 0.083 0.006 -0.030 0.012 orprecisionforanindividualnighthasbeensignificantlyim- 2016-04-10 Before 0.072 0.008 -0.022 0.011 provedafterGDcorrectionsforthe2.4mtelescope,butthe (1m) After 0.084 0.008 -0.018 0.010 results slightly improved for the 1 m telescope. This is due Total Before 0.060 0.066 -0.028 0.056 to the GD effects associated with the 1 m telescope being After 0.071 0.029 -0.001 0.030 MNRAS000,1–9(2016) Precise CCD positions of Himalia using Gaia DR1 5 0.3 0.3 0.2 0.2 A A R 0.1 R 0.1 n n c) i c) i se 0.0 se 0.0 c c ar ar C ( C ( O- -0.1 O- -0.1 Before GDC (2.4 m) Before GDC (2.4 m) After GDC (2.4 m) After GDC (2.4 m) -0.2 -0.2 Before GDC (1 m) Before GDC (1 m) After GDC (1 m) After GDC (1 m) -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-24 57000 JD-24 57000 0.3 0.3 Before GDC (2.4 m) Before GDC (2.4 m) 0.2 After GDC (2.4 m) 0.2 After GDC (2.4 m) Before GDC (1 m) Before GDC (1 m) C After GDC (1 m) C After GDC (1 m) E 0.1 E 0.1 D D n n c) i c) i se 0.0 se 0.0 c c ar ar O-C ( -0.1 O-C ( -0.1 -0.2 -0.2 -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-2457000 JD-2457000 Figure 2. (O-C) residuals of the positions of Himalia in comparison with the ephemeris retrieved from JPL, including the satellite ephemeris JUP300 and planetary ephemeris DE431, with respect to the Julian Dates. The catalogue Gaia DR1 was used for data reduction. The upper two panels show the (O-C) residuals in right ascension in the year 2015 and 2016, respectively. The lower two panelsshowthe(O-C)residualsindeclinationinthetwoyears.Thedarkandredpointsrepresentthe(O-C)residualsforobservations obtainedfromthe2.4mtelescopebeforeandafterGDcorrections,respectively.Theblueandgreenpointsrepresentthe(O-C)residuals forobservationsobtainedfromthe1mtelescopebeforeandafterGDcorrections,respectively.Ineachpanel,thedarkdashlineandred dash line represent the means of (O-C) residuals before and after GD corrections on right ascension and declination for the two years separately. quitesmallerthanthe2.4mtelescope.Themeansof(O-C) sion using Gaia DR1 has been improved by a factor of two residuals for all data sets after GD corrections are 0.071′′ thantheresultsusingUCAC4.Thisismainlyresultingfrom and -0.001′′ in right ascension and declination, respectively. the unprecedent precision of reference star catalogue Gaia Their standard deviations are estimated at about 0.03′′ in DR1. Our results give proof that the tremendous potential each direction. We can see that this precision is improved in improving astrometric precision of CCD observations of bya factor of two than theresults before GD corrections. irregular satellites byusing Gaia DR1. In order to analyze the effects on positional precision madebythereferencestarcatalogue,thecatalogueUCAC4 (Zacharias et al. 2013) was also used for astrometric reduc- 5 DISCUSSIONS tion.Fig.3showsthe(O-C)residualsofpositionsofHimalia using UCAC4 and Gaia DR1. The same ephemeris which In order to analyze the dispersion of (O-C) residuals of Hi- was retrieved from JPL was used.Itcan beseen larger sys- malia, the (O-C) residuals of Himalia by using both cat- tematic errors appearing in the (O-C) residuals of Himalia alogue Gaia DR1 and UCAC4 are drawn together. Fig. 4 byusingUCAC4thantheresultsbyusingGaiaDR1,bothin shows the details. It can been seen that the dispersion of rightascensionanddeclination.Thismaybemainlycaused (O-C) residuals for Gaia DR1 is much more compact than by the existence of zonal errors in the reference star cata- UCAC4.Thesystematicerrorsappearinginthe(O-C)resid- logueUCAC4.However,thesystematicerrorsbyusingGaia ualsofHimaliabyusingGaiaDR1aresignificantlyreduced. DR1 are significantly reduced. Table 4 shows the statistics This is because the zonal errors existing in catalogue Gaia on the (O-C) residuals for Himalia for UCAC4 and Gaia DR1 are quite subtle. We can also see from Fig. 2 that the DR1, respectively. It can be seen that the positional preci- dispersion of (O-C) residuals for Himalia after GD correc- MNRAS000,1–9(2016) 6 H. W. Peng et al. 0.4 0.4 UCAC4 UCAC4 0.3 Gaia DR1 0.3 Gaia DR1 A 0.2 A 0.2 R R n n c) i 0.1 c) i 0.1 e e s s c c ar 0.0 ar 0.0 C ( C ( O- O- -0.1 -0.1 -0.2 -0.2 -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-24 57000 JD-24 57000 0.4 0.4 UCAC4 UCAC4 0.3 Gaia DR1 0.3 Gaia DR1 C 0.2 C 0.2 E E D D n n c) i 0.1 c) i 0.1 se se arc 0.0 arc 0.0 C ( C ( O- -0.1 O- -0.1 -0.2 -0.2 -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-2457000 JD-2457000 Figure3.(O-C)residualsofthepositionsofHimaliaincomparisonwiththeephemerisretrievedfromJPLwhichincludesthesatellite ephemerisJUP300andplanetary ephemerisDE431, withrespecttothe JulianDates. Thecatalogue UCAC4andGaiaDR1wereboth used. The upper two panels show the (O-C) residuals in right ascension in the year 2015 and 2016, respectively. The lower two panels showthe(O-C)residualsindeclinationinthetwoyears.Thedarkpointsrepresentthe(O-C)residualsafterGDcorrectionsforUCAC4 and the redones represent the (O-C)residualsafter GD corrections forGaia DR1.In each panel, the darkdash lineand reddash line representthemeansof(O-C)residualsafterGDcorrectionsonrightascensionanddeclinationforthetwoyearsseparately. DE431. Fig. 5 shows the (O-C) residuals of topocentric as- Table4.Statisticsonthe(O-C)residualsofpositionsofHimalia forGaiaDR1andUCAC4.Column1showsthenumberofCCD trometric positions of Himalia in comparison with the two observations. Column 2 shows the catalogue used. The follow- different ephemerides. Table 5 shows the statistics on the ingcolumnslistthemeansof(O-C)residualsandtheirstandard (O-C)residualsforHimaliaafterGDcorrectionsforthetwo deviations in right ascension and declination, respectively. The ephemerides.Themeansof(O-C)residualsforephemerisre- ephemerides wereretrievedfromJPLwhich includethe satellite trievedfromIMCCEare0.062′′and0.011′′inrightascension ephemerisJUP300andplanetaryephemerisDE431.Allunitsare and declination, respectively. Their corresponding standard inarcseconds. deviationsare0.040′′ and0.030′′.Themeansof(O-C)resid- ualsforalldatasetsbetweenthetwoephemeridesarenearly N Catalogue hO-Ci SD hO-Ci SD equal.Wecanalso see from Table5thattheirstandardde- RA DEC viationsbetweenthetwoephemeridesforthetwoyearssep- 598 UCAC4 0.118 0.058 -0.019 0.055 aratelyareingoodagreement.However,adifferenceforthe GaiaDR1 0.071 0.029 -0.001 0.030 meansof(O-C)residualsinrightascensionbetweenthetwo ephemeridesin2015couldbefound.Inconsiderationofthe same planetary ephemeris DE431 was used, this difference tionsintheyear2016issomewhatworsethantheresultsin should befrom thedifferent satellite ephemeridesused. the year 2015. This is mainly due to the seeing of observa- tions in 2016 is worse than theseeing in 2015. To compare our CCD observations with previous ones, For comparison, the ephemerides retrieved from Insti- some major observational statistics of Himalia are listed in tute de M´echanique C´eleste et de Calcul des E´ph´em´erides Table6.ThedataareretrievedfromtheMinorPlanetCen- (IMCCE) were also obtained, including the satellite ter (MPC). The ephemeris used for our observations was ephemeris by Emelyanov (2005) and planetary ephemeris retrieved from JPL which includes the satellite ephemeris MNRAS000,1–9(2016) Precise CCD positions of Himalia using Gaia DR1 7 Table 6. Comparisons made with other observations retrieved from the MPC. Column 1 shows the IAU code of observatory. Column 2 lists the number of CCD observations. The following 0.4 columns show the mean (O-C) residuals and its standard devi- ation (SD) in right ascension and declination, respectively. All 0.3 positions of Himalia are observed topocentric astrometric posi- tions.Allunitsareinarcseconds. C 0.2 DE IAU No. hO-Ci SD hO-Ci SD Time(yr) n code RA DEC c) i 0.1 e 689 277 -0.013 0.163 -0.013 0.160 2000-2007 s arc 0.0 415 24 -0.008 0.106 0.065 0.088 2008 C ( 809 23 -0.051 0.092 0.014 0.045 2007-2009 O--0.1 511 357 -0.021 0.049 -0.008 0.061 1997-2008 874 56 -0.039 0.112 -0.026 0.070 1992-2014 874 238 -0.077 0.175 -0.009 0.034 1992-2014 UCAC4 -0.2 874 560 0.001 0.069 -0.018 0.053 1992-2014 Gaia DR1 Our 598 0.071 0.029 -0.001 0.030 2015-2016 -0.3 -0.3 -0.2 -0.1 0.0 0.1 0.2 0.3 0.4 O-C (arcsec) in RA Table7.Extractexampleoftheobservedtopocentricastromet- ric positions of Himalia. These positions are comparable to the Figure4.(O-C)residualsofHimaliaindeclinationwithrespect astrometric positions of stars at the same pixel locations with to right ascension. The dark points represent the (O-C) residu- Himalia.According to Urban & Seidelmann (2013), only proper als after GD corrections for catalogue UCAC4 and the red ones motionandannualparallaxesaretakenintoaccountintheastro- represent the (O-C) residualsafter GD corrections forcatalogue metricplacecomputationofstars.Thustheaberrationisignored. GaiaDR1.TheephemeriswasretrievedfromJPLwhichincludes TheobservedtopocentricastrometricpositionsofHimaliainthis thesatelliteephemerisJUP300andplanetaryephemerisDE431. paper can also be directly compared to the positions in its as- Thetwodarkdashlinesrepresentzerolinesineachdirection. trometric ephemeris. Column 1 shows the exposure middle time ofeachCCDobservationinformofJulianDate(UTC).RAand DEC are the observed topocentric astrometric positions inright ascensionanddeclination,respectively. Table 5. Statistics on the (O-C) residuals for Himalia in com- parisonwiththetwodifferentephemerides. Column1showsthe Date RA DEC number of CCD observations. Column 2 shows the ephemeris JD hms ◦ ′ ′′ used. The following columns list the means of (O-C) residuals andtheirstandarddeviationsinrightascensionanddeclination, 2457054.134398 092228.8650 164524.733 respectively. The ephemerides retrieved from IMCCE and JPL 2457054.136921 092228.8028 164525.122 are Emelyanov (2005)/DE431 and JUP300/DE431, respectively. 2457054.138322 092228.7675 164525.338 Allunitsareinarcseconds. ...... ...... ...... 2457489.135787 110312.1353 071608.834 Year N Ephemeris hO-Ci SD hO-Ci SD 2457489.136609 110312.1150 071608.979 RA DEC 2457489.137488 110312.0936 071609.134 2015 185 IMCCE 0.017 0.023 0.026 0.023 JPL 0.056 0.023 0.015 0.022 2016 413 IMCCE 0.082 0.029 0.004 0.030 6 CONCLUSIONS JPL 0.078 0.029 -0.009 0.030 Inthispaper,atotalof598CCDobservationsobtainedfrom Total 598 IMCCE 0.062 0.040 0.011 0.030 the 2.4 m and 1 m telescopes administered by YunnanOb- JPL 0.071 0.029 -0.001 0.030 servatories were processed. Several factors were analyzed, including the reference star catalogue used, the geometric distortionandthephaseeffect.Thereferencestarcatalogue JUP300andplanetaryephemerisDE431.Table6showsthe GaiaDR1andUCAC4werebothusedforastrometricreduc- statistics on the (O-C) residuals. The positions of Himalia tion and havebeen made with comparisons. Positional pre- are observed topocentric astrometric positions. It can be cision of Himalia has been significantly improved after GD seen that our positional precision has significant improve- corrections. The systematic errors existingin theresultsby ments. usingUCAC4 aresignificantly reducedafter Gaia DR1was Table 7 lists the extract example of the observed used. Comparisons between the two different ephemerides topocentric astrometric positions of Himalia. The positions whichretrievedfromJPLandIMCCEhavebeenmade.Our are listed with respect to Julian Date (UTC). RA which results show that the means of (O-C) residuals of Himalia expressed in hours, minutes and seconds are the observed are 0.071′′ and -0.001′′ by using ephemeris retrieved from topocentric astrometric positions of Himalia in right ascen- JPL in right ascension and declination, respectively. Their sion. DEC are the observed topocentric astrometric posi- standarddeviationsareestimatedatabout0.03′′ ineachdi- tionsofHimaliaindeclination,expressedindegrees,arcmin- rection. This positional precision of Himalia is significantly utesand arcseconds. improved by taking advantage of the unprecedent precision MNRAS000,1–9(2016) 8 H. W. Peng et al. 0.3 0.3 JPL JPL IMCCE IMCCE 0.2 0.2 A A R 0.1 R 0.1 n n c) i c) i se 0.0 se 0.0 c c ar ar C ( C ( O- -0.1 O- -0.1 -0.2 -0.2 -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-24 57000 JD-24 57000 0.3 0.3 JPL JPL IMCCE IMCCE 0.2 0.2 C C E 0.1 E 0.1 D D n n c) i c) i se 0.0 se 0.0 c c ar ar O-C ( -0.1 O-C ( -0.1 -0.2 -0.2 -0.3 -0.3 52 54 56 58 60 62 64 66 68 70 445 450 455 460 465 470 475 480 485 490 495 JD-2457000 JD-2457000 Figure5.(O-C)residualsofthepositionsofHimaliaincomparisonwiththetwodifferentephemerides.Theuppertwopanelsshowthe (O-C)residualsinrightascensionintheyear2015and2016,respectively.Thelowertwopanelsshowthe(O-C)residualsindeclination in the two years. The dark points represent the (O-C) residuals after GD corrections for the ephemeris retrieved from IMCCE which includesthesatelliteephemerisbyEmelyanov(2005)andplanetaryephemerisDE431.Theredpointsrepresentthe(O-C)residualsafter GD corrections for the ephemeris retrieved from JPL which includes the satellite ephemeris JUP300 and planetary ephemeris DE431. Ineach panel,the darkdashlineandreddashlinerepresentthemeans of(O-C)residualsafterGD corrections onrightascension and declinationforthetwoyearsseparately. of star catalogue Gaia DR1 in comparison with previous REFERENCES works. AgnorC.B.,HamiltonD.P.,2006,Nature,441,192 ColomboG.,FranklinF.A.,1971, Icarus,15,186 deBruijneJ.H.J.,2012,Ap&SS,341,31 ACKNOWLEDGEMENTS EmelyanovN.V.,2005,A&A,435,1173 FanY.F.,BaiJ.M.,ZhangJ.J.,WangC.J.,ChangL.,XinY.X., This research work is financially supported by the Na- ZhangR.L.,2015,ResearchinAstronomyandAstrophysics, tional Natural Science Foundation of China (grant nos. 15,918 U1431227,11273014). 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