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Where is this?

Learn about the composition of ice giants, the densities of different planets, the emissions from Enceladus' tiger stripes, the lifetime of protoplanetary disks, and the problem solved by the Nice Model in the Solar System. Discover fascinating facts about the moons of Uranus and expand your knowledge of the Solar System.

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Where is this?

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  1. Where is this?

  2. Solar System Explorers 02 1. What three ices dominate the ice giants’ composition (that is ice)? … 2. Which planet has the lowest density? the highest density? … 3. If Enceladus’ tiger stripes have a temperature of 180 K, at what wavelength do they emit the most photons? … 4. Do protoplanetary disks last roughly 105, 107, or 109 years? … 5. What particular problem does the Nice Model solve in the Solar System? … B. Name any moon of Uranus. …

  3. Solar System Explorers 02

  4. Solar System Explorers 02 1. What three ices dominate the ice giants’ composition (that is ice)? H2O … NH3 … CH4 2. Which planet has the lowest density? the highest density? Saturn = 0.69 g/cm3… Earth = 5.52 g/cm3 3. If Enceladus’ tiger stripes have a temperature of 180 K, at what wavelength do they emit the most photons? 16 microns 4. Do protoplanetary disks last roughly 105, 107, or 109 years? 107 years 5. What particular problem does the Nice Model solve in the Solar System? 4 giant planets are not in circular, coplanar orbits B. Name any moon of Uranus. Juliet, Portia, Puck, Miranda, Ariel, Umbriel, Titania, Oberon …

  5. Solar System Explorers 03 Describe something you have already learned in this course that you did not know previously. 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20.

  6. Where is this?

  7. Dynamics I

  8. Basic Newton G mEarth m2 F gravity on Earth = — _______________ r2 What about the Moon? mEarth = 5.97e24 kg Earth-Moon has FEarth ~ 1.98e20, Sun-Moon has FSun ~ 4.34e20

  9. Dynamics: Kepler I Kepler I: planetary orbits are ellipses with the Sun at a focus a (1 − e2) rEarth-Sun = ______________ 1 + e cos f e, eccentricity = (1 − b2minor/a2major)1/2 f (or θ, or ν), true anomaly = angle between perihelion and current position

  10. Dynamics: Kepler I Kepler I: planetary orbits are ellipses with the Sun at a focus a (1 − e2) rEarth-Sun = ______________ 1 + e cos f e, eccentricity = (1 − b2minor/a2major)1/2 f (or θ, or ν), true anomaly = angle between perihelion and current position Newton I : both bodies move along elliptical paths, with one focus of each ellipse located at the center of mass m1r1 + m2r2 rCM = _________________ M M = m1 + m2 Application: discovery of extrasolar planets

  11. Dynamics: Kepler II Kepler II: a line between a planet and the Sun sweeps out equal areas in equal times dA/dt = constant Newton II : a line connecting two bodies (or connecting one body to the center of mass position) sweeps out equal areas in equal times dL/dt= 0 (conservation of angular momentum) Application: spectroscopic binary orbits; prediction of planet locations

  12. Dynamics: Kepler III Kepler III: planetary orbital periods and distances from the Sun are directly (and simply) related as long as you assume SS units P2(yr) = a3 (AU) Newton III: it also works outside of the Solar System 4π2a3 a3 P2= __________________ or Mtotal = _______ G (m1 + m2) P2 solar masses, AU, yrs Application: stellar and planetary masses need fractional mass, f, for individual masses dirty little secrets of exoplanet masses …

  13. M Dwarf Masses scatter = 0.023 M ~ 7% scatter = 0.014 M ~ 4% MK MV Benedict, Henry, Franz et al. 2016

  14. Orbital Elements a semimajor axis size e eccentricity shape i inclination (~0 in SS, edge on = 90 outside) tilt angle P orbital period time T epoch of periastron a date Ω longitude of ascending node spin angle ω argument of periastron tωist angle

  15. Spin Ω: Longitude of Ascending Node

  16. Tωist ω: Longitude of Periastron

  17. Orbital Elements a semimajor axis size e eccentricity shape i inclination tilt P orbital period time T epoch of periastron a date Ω longitude of ascending node flip angle ω longitude of periastron twist angle equinox equinox of date sets direction of equinox f fractional mass a number Two observations will not yield an orbit. Why? Each point has (X position, Y position, time). There are 7 classical unknowns, so you need a third point to give you 9 pieces of data to solve equations.

  18. Stars: Very Low Mass GJ 1245 AC

  19. Stars: Triples theory: about 7:1 ratio in semimajor axis is critical point optical triples spectroscopic triples SETI sample projected separations our Solar System is different … why?

  20. New Orbits in Solar System located 44.7 AU Psun ~ 300 yrs HST WFPC2 images V = 23.1 Porb 590 ± 40 days a 22400 ± 900 km mtot 0.02% Pluto at least 75 multiple TNOs known www2.lowell.edu/users/grundy/tnbs/status.html 587.3 ± 0.2 days

  21. Counter-Intuitive Dynamics Lagrangian Points: where objects feel no net force in rotating frame;gravitational force of two masses cancels centrifugal force because of rotation 5 per two body system Trojan asteroids at Jupiter (>5000), Mars (6+), Neptune (7+) small moons at Sat/Tethys (Telesto+Calypso) and Sat/Dione (Helene+Polydeuces) Earth orbiting spacecraft WMAP Gaia JWST SOHO

  22. Counter-Intuitive Dynamics Tadpole orbits: librating positions around L4 and L5 (note corotating frame!) Trojan asteroids at Jupiter, Mars, and Neptune

  23. Counter-Intuitive Dynamics Horseshoe orbits: orbit swapping due to particles passing in orbits, or in resonance with larger bodies (note corotating frame!) Janus and Epimetheus (Saturn) swap orbits every 4 years Cruithne and Asteroid 2002 AA29 around Earth

  24. Counter-Intuitive Dynamics Horseshoe orbits: Cruithne --- each loop takes 1 yr www.astro.uwo.ca/~wiegert/3753/3753.html

  25. Counter-Intuitive Dynamics Horseshoe orbits: Asteroid 2002 AA29 --- each vertical loop takes 1 yr www.astro.uwo.ca/~wiegert/AA29/AA29.html “at least three others”

  26. Counter-Intuitive Dynamics Chaotic motion: trajectories that begin arbitrarily close together will diverge exponentially with time (note that 4.6 Gyr is often not “sufficient time”) Mars’ axis tilt Hyperion rotation in Saturn-Titan tug-of-war Resonances: orbital periods with ratios A : B (both integers) Io : Europa : Ganymede (1 : 2.008 : 4.044) … oblate? tides? Neptune : Plutinos (3:2) Asteroids : Jupiter (lots) --- pumped up e leads to Kirkwood gaps Saturn ring particles : Saturn moons (Mimas, Atlas, …)

  27. 1 : 2 : 4

  28. …………………………

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