Notes to Ijiraq and Kiviuq Orbital Evolution Reconstruction

Total Page:16

File Type:pdf, Size:1020Kb

Notes to Ijiraq and Kiviuq Orbital Evolution Reconstruction Lunar and Planetary Science XXXVII (2006) 1134.pdf NOTES TO IJIRAQ AND KIVIUQ ORBITAL EVOLUTION RECONSTRUCTION. A. E. Rosaev1, 1FGUP NPC "NEDRA" Svobody 8/38, Yaroslavl 150000, Russia,E-mail: [email protected] . Introduction: The problem of origin of outer Table 2 Main periods for Kiviuq and Ijiraq orbital irregular satellites of large planets is considered. The motion and evolution capture way of their origin most probable, however Kiviuq Ijiraq there is not detail theory. There are a number of P (days) 449.21942 451.46596 irregular satellites, discovered in recent time. It gives Tcon, , yr 245.7±0.2 an ability to investigate the statistics of orbital Pnode, yr 846.46 868.25 interaction and try to reconstruct real collision history Tnode ,yr 32880±30 of these objects. Nesvorny et all [1] research evolution ∆T between two nearest 6 of orbit orientations in asteroid families and prove fact conjunctions at epoch of (8.08±0.01)*10 of recent catastrophic destruction in asteroid main belt. intersections, yr On the other hand, the method of investigations of minimal distance between orbits successfully applied It is evident, that for breakup epoch the distance in our previous works [2]. It is naturally to apply these between orbits must be close to zero, and conjunction two ideas to irregular satellites orbits with close (around longitude of minimal distance) must take elements for determination their parent body possible place. Let breakup take place at epoch t. Next ability to catastrophic destruction epoch. There are few groups exact repeat breakup configuration will take place of irregular satellites in Jupiter and Saturn systems. We through about 33000 years due to mutual node motion restrict this consideration by pair of orbits with close (orbit precession), however, due to long time between elements: Kiviuq and Ijiraq (table 1). subsequent conjunctions (240 years), not each The quasi coorbital objects have a particular configurations is suitable. A very long period between interest. It is natural to suppose, that such close orbits conjunction and orbit configuration repeating for appear not causal, but a product of catastrophic Kiviuq and Ijiraq case (deltaT) means, that we have breakup with small relative velocity. It is evident, that relative small number of similar events (about 500) at breakup process may be related with capture; and this the history of the Solar system and can to consider process could be multistage each more carefully. Due to Yarkovsky effect, close Table 1 Kiviuq and Ijiraq mean orbital elements (R. A. orbits can change their mutual positions, so most Jacobson, private communications) recent cases of close encounters are most possible for breakup. Kiviuq Ijiraq a 1.1365000 1.1442000 Moreover, if conjunction takes place close to epoch e 0.3336 0.3215 33000 year, according to precession period, it can take ω 83.043 85.523 place far from longitude of orbit intersection point. It i 46.148 46.73 means, that the longitude of minimal distance between Ω 359.519 136.348 orbits must take into account in ∆T value (table 2). The calculations show that really zero encounters between To the Epoch of Ijiraq and Kiviuq Parent Body Saturnian moonlets can take place about one time per Destruction Determination: The studying outer 100 million years. So, we must consider only about 40 natural satellite close orbits rather easy than asteroids cases. by some reasons first of all, the main perturbation from In according with our data, main result of this the Sun change in more narrow range, than Jupiter investigation – a most close to present possible Epoch perturbation for minor planets, and there are no of catastrophic breakup when Kiviuq and Ijiraq appear subsequent encounters with another objects. is 1.938±0.002 *106 yr. The orbital periods and rates of orbit precession are Conclusions: The unique orbital characteristics of given in table 2. The period Tcon between conjunction small irregular Saturn satellites Ijiraq and Kiviuq and period Tnode between two similar orbit provide a very rare mutual close encounters . It is orientations are calculated by expressions: possible to calculate main periods in studied system. The epoch of most recent close encounter is calculated. Tcon=P /(P -P )*P /365.24 1 2 1 2 References: [1] Nesvorny D., et al. (2002). Nature, Vol 417, 721. [2] Rosaev A.E. (2001) In: Dynamics of Tnode=Pnode1/(Pnode2 – P node1)*Pnode2 Natural and Artifical Celestial bodies, 301-303. and it was verified by numeric calculations. .
Recommended publications
  • Cassini Update
    Cassini Update Dr. Linda Spilker Cassini Project Scientist Outer Planets Assessment Group 22 February 2017 Sols%ce Mission Inclina%on Profile equator Saturn wrt Inclination 22 February 2017 LJS-3 Year 3 Key Flybys Since Aug. 2016 OPAG T124 – Titan flyby (1584 km) • November 13, 2016 • LAST Radio Science flyby • One of only two (cf. T106) ideal bistatic observations capturing Titan’s Northern Seas • First and only bistatic observation of Punga Mare • Western Kraken Mare not explored by RSS before T125 – Titan flyby (3158 km) • November 29, 2016 • LAST Optical Remote Sensing targeted flyby • VIMS high-resolution map of the North Pole looking for variations at and around the seas and lakes. • CIRS last opportunity for vertical profile determination of gases (e.g. water, aerosols) • UVIS limb viewing opportunity at the highest spatial resolution available outside of occultations 22 February 2017 4 Interior of Hexagon Turning “Less Blue” • Bluish to golden haze results from increased production of photochemical hazes as north pole approaches summer solstice. • Hexagon acts as a barrier that prevents haze particles outside hexagon from migrating inward. • 5 Refracting Atmosphere Saturn's• 22unlit February rings appear 2017 to bend as they pass behind the planet’s darkened limb due• 6 to refraction by Saturn's upper atmosphere. (Resolution 5 km/pixel) Dione Harbors A Subsurface Ocean Researchers at the Royal Observatory of Belgium reanalyzed Cassini RSS gravity data• 7 of Dione and predict a crust 100 km thick with a global ocean 10’s of km deep. Titan’s Summer Clouds Pose a Mystery Why would clouds on Titan be visible in VIMS images, but not in ISS images? ISS ISS VIMS High, thin cirrus clouds that are optically thicker than Titan’s atmospheric haze at longer VIMS wavelengths,• 22 February but optically 2017 thinner than the haze at shorter ISS wavelengths, could be• 8 detected by VIMS while simultaneously lost in the haze to ISS.
    [Show full text]
  • A Deeper Look at the Colors of the Saturnian Irregular Satellites Arxiv
    A deeper look at the colors of the Saturnian irregular satellites Tommy Grav Harvard-Smithsonian Center for Astrophysics, MS51, 60 Garden St., Cambridge, MA02138 and Instiute for Astronomy, University of Hawaii, 2680 Woodlawn Dr., Honolulu, HI86822 [email protected] James Bauer Jet Propulsion Laboratory, California Institute of Technology 4800 Oak Grove Dr., MS183-501, Pasadena, CA91109 [email protected] September 13, 2018 arXiv:astro-ph/0611590v2 8 Mar 2007 Manuscript: 36 pages, with 11 figures and 5 tables. 1 Proposed running head: Colors of Saturnian irregular satellites Corresponding author: Tommy Grav MS51, 60 Garden St. Cambridge, MA02138 USA Phone: (617) 384-7689 Fax: (617) 495-7093 Email: [email protected] 2 Abstract We have performed broadband color photometry of the twelve brightest irregular satellites of Saturn with the goal of understanding their surface composition, as well as their physical relationship. We find that the satellites have a wide variety of different surface colors, from the negative spectral slopes of the two retrograde satellites S IX Phoebe (S0 = −2:5 ± 0:4) and S XXV Mundilfari (S0 = −5:0 ± 1:9) to the fairly red slope of S XXII Ijiraq (S0 = 19:5 ± 0:9). We further find that there exist a correlation between dynamical families and spectral slope, with the prograde clusters, the Gallic and Inuit, showing tight clustering in colors among most of their members. The retrograde objects are dynamically and physically more dispersed, but some internal structure is apparent. Keywords: Irregular satellites; Photometry, Satellites, Surfaces; Saturn, Satellites. 3 1 Introduction The satellites of Saturn can be divided into two distinct groups, the regular and irregular, based on their orbital characteristics.
    [Show full text]
  • Cassini Observations of Saturn's Irregular Moons
    EPSC Abstracts Vol. 12, EPSC2018-103-1, 2018 European Planetary Science Congress 2018 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2018 Cassini Observations of Saturn's Irregular Moons Tilmann Denk (1) and Stefano Mottola (2) (1) Freie Universität Berlin, Germany ([email protected]), (2) DLR Berlin, Germany 1. Introduction two prograde irregulars are slower than ~13 h, while the periods of all but two retrogrades are faster than With the ISS-NAC camera of the Cassini spacecraft, ~13 h. The fastest period (Hati) is much slower than we obtained photometric lightcurves of 25 irregular the disruption rotation barrier for asteroids (~2.3 h), moons of Saturn. The goal was to derive basic phys- indicating that Saturn's irregulars may be rubble piles ical properties of these objects (like rotational periods, of rather low densities, possibly as low as of comets. shapes, pole-axis orientations, possible global color variations, ...) and to get hints on their formation and Table: Rotational periods of 25 Saturnian irregulars evolution. Our campaign marks the first utilization of an interplanetary probe for a systematic photometric Moon Approx. size Rotational period survey of irregular moons. name [km] [h] Hati 5 5.45 ± 0.04 The irregular moons are a class of objects that is very Mundilfari 7 6.74 ± 0.08 distinct from the inner moons of Saturn. Not only are Loge 5 6.9 ± 0.1 ? they more numerous (38 versus 24), but also occupy Skoll 5 7.26 ± 0.09 (?) a much larger volume within the Hill sphere of Suttungr 7 7.67 ± 0.02 Saturn.
    [Show full text]
  • PDS4 Context List
    Target Context List Name Type LID 136108 HAUMEA Planet urn:nasa:pds:context:target:planet.136108_haumea 136472 MAKEMAKE Planet urn:nasa:pds:context:target:planet.136472_makemake 1989N1 Satellite urn:nasa:pds:context:target:satellite.1989n1 1989N2 Satellite urn:nasa:pds:context:target:satellite.1989n2 ADRASTEA Satellite urn:nasa:pds:context:target:satellite.adrastea AEGAEON Satellite urn:nasa:pds:context:target:satellite.aegaeon AEGIR Satellite urn:nasa:pds:context:target:satellite.aegir ALBIORIX Satellite urn:nasa:pds:context:target:satellite.albiorix AMALTHEA Satellite urn:nasa:pds:context:target:satellite.amalthea ANTHE Satellite urn:nasa:pds:context:target:satellite.anthe APXSSITE Equipment urn:nasa:pds:context:target:equipment.apxssite ARIEL Satellite urn:nasa:pds:context:target:satellite.ariel ATLAS Satellite urn:nasa:pds:context:target:satellite.atlas BEBHIONN Satellite urn:nasa:pds:context:target:satellite.bebhionn BERGELMIR Satellite urn:nasa:pds:context:target:satellite.bergelmir BESTIA Satellite urn:nasa:pds:context:target:satellite.bestia BESTLA Satellite urn:nasa:pds:context:target:satellite.bestla BIAS Calibrator urn:nasa:pds:context:target:calibrator.bias BLACK SKY Calibration Field urn:nasa:pds:context:target:calibration_field.black_sky CAL Calibrator urn:nasa:pds:context:target:calibrator.cal CALIBRATION Calibrator urn:nasa:pds:context:target:calibrator.calibration CALIMG Calibrator urn:nasa:pds:context:target:calibrator.calimg CAL LAMPS Calibrator urn:nasa:pds:context:target:calibrator.cal_lamps CALLISTO Satellite urn:nasa:pds:context:target:satellite.callisto
    [Show full text]
  • Perfect Little Planet Educator's Guide
    Educator’s Guide Perfect Little Planet Educator’s Guide Table of Contents Vocabulary List 3 Activities for the Imagination 4 Word Search 5 Two Astronomy Games 7 A Toilet Paper Solar System Scale Model 11 The Scale of the Solar System 13 Solar System Models in Dough 15 Solar System Fact Sheet 17 2 “Perfect Little Planet” Vocabulary List Solar System Planet Asteroid Moon Comet Dwarf Planet Gas Giant "Rocky Midgets" (Terrestrial Planets) Sun Star Impact Orbit Planetary Rings Atmosphere Volcano Great Red Spot Olympus Mons Mariner Valley Acid Solar Prominence Solar Flare Ocean Earthquake Continent Plants and Animals Humans 3 Activities for the Imagination The objectives of these activities are: to learn about Earth and other planets, use language and art skills, en- courage use of libraries, and help develop creativity. The scientific accuracy of the creations may not be as im- portant as the learning, reasoning, and imagination used to construct each invention. Invent a Planet: Students may create (draw, paint, montage, build from household or classroom items, what- ever!) a planet. Does it have air? What color is its sky? Does it have ground? What is its ground made of? What is it like on this world? Invent an Alien: Students may create (draw, paint, montage, build from household items, etc.) an alien. To be fair to the alien, they should be sure to provide a way for the alien to get food (what is that food?), a way to breathe (if it needs to), ways to sense the environment, and perhaps a way to move around its planet.
    [Show full text]
  • Request Riders Start (SCET) Start (Calenda Duration
    Request Riders Start (SCET) Start (calenda Duration End Primary Secondary Comments (SPASS) Object Samp Line Phase Mag Post‐downlink comments (Tilmann Denk, FU Berlin) (pre‐ Notes : This spreadsheet somehow summarizes the Cassini observations of dic‐ For this sheet, information from the Project's SPASSes (SPacecraft Attitude ted) Almost all observations in this sheet were planned by myself (at DLR and Fr The SATELLORB requests (displayed in blue in this sheet) were planned by t Rider instruments (mainly UVIS and VIMS) can be taken from column B. No An occasionally updated version of this document plus lots of other stuff co https://tilmanndenk.de/outersaturnianmoons Cruise phase (Jupiter flyby) This is the document version of 15 Mar 2018. Sequence C023 2000‐310T05:25:00 069T21:35:00 2001‐014T03:00:00 VIMS_C23HI_HIM1X1001_PRIME I, U 2000‐353T20:00:00 2000‐12‐18 000T06:00:00 2000‐354T02:00:00 (Himalia) Himalia 789 237 70 disk‐res. Irregular moon of Jupiter. Object was resolved (~4x6 NAC pixels). Very redu Cruise phase (Saturn approach) Sequence S001, length = 35 ... 2004‐135T18:40:00 036T03:12:00 2004‐171T21:52:00 ISS_000PH_FULROTIN001_PRIME C, U, V 2004‐162T01:53:00 2004‐06‐10 000T11:44:00 2004‐162T13:37:00 CIRS_FP3 to Phoebe NEG_X to Sun Accomodate CIRS and U Phoebe 530 340 87 disk‐res. Day before targeted flyby. Phoebe is already visible as a disk. ISS_000PH_LOWRES0001_PRIME C, U 2004‐163T05:23:00 2004‐06‐11 000T00:16:00 2004‐163T05:39:00 ISS_NAC to Phoebe POS_Z to NEP S_N_ER_‐5a Phoebe 87 disk‐res. Targeted flyby inbound.
    [Show full text]
  • Rotation Periods of Irregular Satellites of Saturn
    EPSC Abstracts Vol. 6, EPSC-DPS2011-1452, 2011 EPSC-DPS Joint Meeting 2011 c Author(s) 2011 Rotation Periods of Irregular Satellites of Saturn T. Denk (1), S. Mottola (2), Th. Roatsch (2), H. Rosenberg (1), and G. Neukum (1) (1) FU Berlin, Germany ([email protected]), (2) DLR Berlin, Germany Abstract ~60x to ~240x closer to the objects than the Earth is, and long duration observations are possible because Rotation periods of six irregular moons of Saturn there is no 24-h day/night cycle at Cassini. Dis- have been measured as follows: Siarnaq ~06:40 h; advantages are the relatively small telescope mirror Ymir ~07:20 h; Albiorix 13:19±0:08 h; Bebhionn of the Cassini ISS camera (0.17 m), the smaller field- ~16 h; Paaliaq ~19 h; Kiviuq 21:49±0:13 h (Tab. 1). of-view of the ISS resulting in a significantly higher pointing accuracy requirement, and the inability of doing image quality checks and exposure parameter 1. Introduction adaptations during data acquisition. We observe irregular moons of Saturn with the Imaging Experiment (ISS) of the Cassini spacecraft 2. Results [1]. Motivation is the determination of basic properties of these objects like rotation periods, polar Measured rotation periods for seven satellites are axes orientations, object sizes and shapes, phase shown in Tab. 1. The values vary significantly: curves, colors, or the search for binaries. This might While Siarnaq, with a period of ~6 h 40 min., rotates allow a better understanding of the impact history in relatively fast, Kiviuq needs almost 22 h for one the saturnian system including the question about the day/night cycle.
    [Show full text]
  • Irregular Satellites of the Giant Planets 411
    Nicholson et al.: Irregular Satellites of the Giant Planets 411 Irregular Satellites of the Giant Planets Philip D. Nicholson Cornell University Matija Cuk University of British Columbia Scott S. Sheppard Carnegie Institution of Washington David Nesvorný Southwest Research Institute Torrence V. Johnson Jet Propulsion Laboratory The irregular satellites of the outer planets, whose population now numbers over 100, are likely to have been captured from heliocentric orbit during the early period of solar system history. They may thus constitute an intact sample of the planetesimals that accreted to form the cores of the jovian planets. Ranging in diameter from ~2 km to over 300 km, these bodies overlap the lower end of the presently known population of transneptunian objects (TNOs). Their size distributions, however, appear to be significantly shallower than that of TNOs of comparable size, suggesting either collisional evolution or a size-dependent capture probability. Several tight orbital groupings at Jupiter, supported by similarities in color, attest to a common origin followed by collisional disruption, akin to that of asteroid families. But with the limited data available to date, this does not appear to be the case at Uranus or Neptune, while the situa- tion at Saturn is unclear. Very limited spectral evidence suggests an origin of the jovian irregu- lars in the outer asteroid belt, but Saturn’s Phoebe and Neptune’s Nereid have surfaces domi- nated by water ice, suggesting an outer solar system origin. The short-term dynamics of many of the irregular satellites are dominated by large-amplitude coupled oscillations in eccentricity and inclination and offer several novel features, including secular resonances.
    [Show full text]
  • Moon-O-Meter
    Earth Number Name Designation a (mi) a (km) i (°) e Per (days) Mag Size (mi) Size (km) Year the Moon 238,800 384,400 5.145 0.0549 27.3217 -12.7 2,159 3,476 n/a Mars Number Name Designation a (mi) a (km) i (°) e Per (days) Mag Size (mi) Size (km) Year I Phobos 5,825 9,378 1.08 0.0151 0.31891 11.3 7 11 1877 II Deimos 14,571 23,459 1.79 0.0005 1.26244 12.4 4 6 1877 Jupiter Number Name Designation a (mi) a (km) i (°) e Per (days) Mag Size (mi) Size (km) Year XVI Metis 79,600 128,100 0.021 0.001 0.3 17.5 27 44 1979 XV Adrastea 80,100 128,900 0.027 0.002 0.3 18.7 10 16 1979 V Amalthea 112,700 181,400 0.389 0.003 0.5 14.1 104 168 1892 XIV Thebe 137,800 221,900 1.07 0.018 0.68 16 61 98 1979 I Io 262,000 421,800 0.036 0 1.77 5 2,263 3,643 1610 II Europa 416,800 671,100 0.467 0 3.55 5.3 1,939 3,122 1610 III Ganymede 664,800 1,070,400 0.172 0.001 7.16 4.6 3,268 5,262 1610 IV Callisto 1,169,400 1,882,700 0.307 0.007 16.69 5.7 2,994 4,821 1610 XVIII Themisto S/2000 J1 4,662,700 7,507,000 43.08 0.242 130 21 6 9 2000 XIII Leda 6,934,800 11,165,000 27.46 0.164 240.9 20.2 11 18 1974 VI Himalia 7,118,600 11,461,000 27.5 0.162 250.6 14.8 114 184 1904 X Lysithea 7,277,600 11,717,000 28.3 0.112 259.2 18.2 24 38 1938 VII Elara 7,292,500 11,741,000 26.63 0.217 259.6 16.6 48 78 1905 S/2000 J11 7,798,100 12,555,000 28.3 0.248 287 22.4 2 4 2000 XLVI Carpo S/2003 J20 10,552,200 16,989,000 51.4 0.43 456.1 23 2 3 2003 XXXIV Euporie S/2001 J10 11,988,800 19,302,000 145.8 0.144 550.7 23.1 1 2 2001 XXXV Orthosie S/2001 J9 12,870,200 20,721,000 145.9 0.281 622.6 23.1
    [Show full text]
  • Cassini Observations of Saturn's Irregular Moons. T
    50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 2654.pdf CASSINI OBSERVATIONS OF SATURN'S IRREGULAR MOONS. T. Denk1 and S. Mottola2, 1Freie Univer- sität Berlin, Malteserstr. 74-100, 12249 Berlin, Germany ([email protected]), 2Deutsches Zentrum für Luft- und Raumfahrt (DLR), Rutherfordstr. 2, 12489 Berlin, Germany ([email protected]). Introduction: Saturn's outer or irregular moons Since Cassini was located inside the orbits of the represent a distinct class of objects in the Solar Sys- irregular moons, but the illumination source (the Sun) tem. They were discovered between 2000 and 2007 was far away (outside the orbits), the phase angles except for Phoebe which has been photographed since could take all values between 0° and 180° (see Table 1 1898. The distances between Saturn and the 38 known for ranges of actual observation phases). This unique objects vary between 7.6 Gm (126 RS; Kiviuq periap- advantage of Cassini would be given to any spacecraft sis) and 33.2 Gm (550 RS; Surtur apoapsis). The irreg- orbiting a giant planet while observing outer moons. ulars are found on orbits of large eccentricity and high The total number of ISS images targeting irregular inclination, both prograde and retrograde. moons is ~38,000, obtained during ~200 observations. Large moon Phoebe has a retrograde orbit and ac- Our Cassini campaign represents the first utilization of counts for more than 98% of the total mass of Saturn's an interplanetary spacecraft for a systematic photomet- irregulars. Of the remaining mass, ~92% belongs to ric survey of irregular moons in the Solar System.
    [Show full text]
  • Models of Saturn's Protoplanetary Disk Forming In-Situ Its Regular Satellites
    Model of Saturn’s protoplanetary disk forming in-situ its regular satellites and innermost rings before the planet is formed Dimitris M. Christodoulou1, 2 and Demosthenes Kazanas3 1 Lowell Center for Space Science and Technology, University of Massachusetts Lowell, Lowell, MA, 01854, USA. 2 Dept. of Mathematical Sciences, Univ. of Massachusetts Lowell, Lowell, MA, 01854, USA. E-mail: [email protected] 3 NASA/GSFC, Laboratory for High-Energy Astrophysics, Code 663, Greenbelt, MD 20771, USA. E-mail: [email protected] March 5, 2019 ABSTRACT We fit an isothermal oscillatory density model of Saturn’s protoplanetary disk to the present-day major satellites and innermost rings D/C and we determine the radial scale length of the disk, the equation of state and the central density of the primordial gas, and the rotational state of the Saturnian nebula. This disk does not look like the Jovian and Uranian disks that we modeled previously. Its power-law index is extremely steep (k = −4.5) and its radial extent is very narrow (∆R . 0.9 Gm), its rotation parameter that measures centrifugal support against self-gravity is somewhat larger (β0 = 0.0431), as is its radial scale length (395 km); but, as was expected, the size of the Saturnian disk, Rmax = 3.6 Gm, takes just an intermediate value. On the other hand, the central density of the compact Saturnian core and its angular velocity are both comparable to that of Jupiter’s core (density of ≈ 0.3 g cm−3 in both cases, and rotation period of 5.0 d versus 6.8 d); and significantly less than the corresponding parameters of Uranus’ core.
    [Show full text]
  • Sidereal Periods, Pole Solutions, and Shape Models of Saturn's Irregular Moons
    EPSC Abstracts Vol. 13, EPSC-DPS2019-710-2, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. Sidereal Periods, Pole Solutions, and Shape Models of Saturn's Irregular Moons Tilmann Denk (1) and Stefano Mottola (2) (1) Freie Universität Berlin, Germany ([email protected]), (2) DLR Berlin, Germany During the Cassini mission, the irregular moons of produce intolerable additional noise. Furthermore, Saturn [1] have been targeted more than 200 times due to platform stability control deadbanding, for remote observations, marking the first exploration observed objects moved back and forth on the CCD of irregular moons through an interplanetary space- over a range of 10-20 pixels with typical periods of craft orbiting the common planet [2]. The moons tens of minutes. For this reason undercorrected pixels have been observed with the Narrow Angle Camera would also contain an additional quasi-periodic noise (NAC) of Cassini's ISS instrument which was a signal. Therefore, we decided to use science observ- spacecraft-fixed Ritchey-Chretien reflector telescope ations taken close in time to the actual observation to with a focal length of 2 m and an aperture of 0.19 m produce updated dark frames for each individual [3]. Since the irregulars were (except for Phoebe observation. during a targeted flyby) always more than 4∙106 km and mostly even more than 107 km away from the Color data calibration will be done in a similar way. spacecraft and thus too far away for disk-resolved In addition, making use of data from Cassini-ISS imaging, the goal was to obtain lightcurves through observations of solar-analog stars 16 Cygni B and disk-integrated photometry.
    [Show full text]