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CHARACTERIZING THE
PROPERTIES OF THE
GALILEAN MOONS
Trevor Picard
• Background
• Goals
• Methods
• Analysis
• Results
• Errors
• Conclusions
Astrometry: Optical Surveys
• Past: POSS (89 million objects → primarily to
study galaxy morphology)
• Present: SDSS (500 million objects)
• Future (2019): LSST (200,000 images/year)
Source: Astrophysical Research Consortium (ARC) & Sloan Digital Sky Survey (SDSS)
Astrometry: Applications
• Instrumental in time-keeping (UTC)
• Important rung of cosmic distance ladder
• Exoplanet detection verification
• Near-earth object tracking
• Orbital Mechanics…
• Background
• Goals
• Methods
• Analysis
• Results
• Conclusions
Project Goals
• Determine the masses of the Galilean moons
through astrometric observations.
• Kepler’s 3rd Law: simplified 2-body problem
• Knowing an object’s mass provides valuable
insight into many other properties (ρave, gs, etc.)
• Get as many measurements as possible to
precisely and accurately infer orbital period and
average orbital radius.
• Background
• Goals
• Methods
• Analysis
• Results
• Conclusions
Tools: Pre-Observing
Sky & Telescope Online Observing Tool: shows which
moons will be visible at certain dates and times
Tools: Pre-Observing
HORIZON Interface: provided RA and Dec of
Jupiter, current distance between Jupiter and Earth,
actual values for calculated quantities (needed to
calculate error)
Observational Methods
• MDM Observatory: 1.3-meter +
4K Imager
• FOV: 0.31”/pixel, 21.3” span
• Took images with U, g, and Y
band filters ranging from 1- to 6-
second exposures.
• More frequent and numerous
observations allows us to better
infer p and a.
Source: MDM, KPNO
Source: MDM, KPNO
Source: MDM, KPNO
• Background
• Goals
• Methods
• Analysis
• Results
• Conclusions
Periodic Regression Analysis
• Mathematica: r (“) = A sin(B t + C)
• r: the angular distance of the moon from Jupiter
• t: time (minutes)
• A: the max angular distance between Jupiter and
each moon (amplitude)
• B: used to find the orbital period (p = 2𝜋 / B).
• B and C are used in combination to find the time
of maximum elongation
Calculations
• r = dJupiter(A x π)/(3600 x 180)
• Since dJupiter varies slightly over the course of
our observations, we used B t + C = π/2 to
find t(dmax).
• Periodicity: 2π/B
Calculating Moon Masses
Kepler’s 3rd Law
a
• Background
• Goals
• Methods
• Analysis
• Results
• Conclusions
Mass Discrepancy
• MJ >> m → our calculated orbital radii still
generated moon masses off by several orders
of magnitude
• Decided to use known values of orbital radii,
but our own calculated periods (which were
more accurate) to perform the calculations
Example: Europa
0.042% error
3.551181 days (accepted)
3.55 days (observed)
1.17% error
0.6709 x 106 m (mean accepted)
0.6632 x 106 m (observed)
1.898 x 1027 kg4.7998 x 1022 kg
Results
• Periods: all extremely accurate (within 0.05%).
• Orbital radii: Not precise enough to calculate masses.
Io Europa Ganymede Callisto
p (days) 1.77 3.55 6.10 16.69
Error in p (%) 0.002 0.042 0.008 0.006
a (106 km) 0.42113 0.66324 1.06920 1.87250
Error in a (%) 0.15 1.17 0.08 0.56
Inferred Moon Properties
Error was surprisingly small…
• Background
• Goals
• Methods
• Analysis
• Results
• Conclusions
Sources of Error: Restrictions
• Very few observations
• short time span of observations
• imprecise periodic fit in Mathematica
Sources of Error: Random Error
• Jupiter’s saturation → imprecise zero point
• Clouds → improvised exposure times
?
Sources of Error: Systematic Error
• Instead of using barycenter, assumed a
center of mass at Jupiter’s center.
• Assumed circular orbits when they are
actually elliptical.
Conclusions
Question: Is astrometry + Kepler’s 3rd Law a
reasonable way to calculate masses?
Answer: Maybe
Summary
• Astrometry is important (gives us our bearings).
• Ellipticity, mass barycenter, orbit inclination, etc.
must be accounted for.
• Mass of orbiting bodies are often orders of
magnitude smaller than the bodies they orbit,
requiring very precise astrometry.
• Astrometry requires many precise observations over
long periods of time.
• Doppler Shift > Astrometry for mass calculation.

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429Talk

  • 1. CHARACTERIZING THE PROPERTIES OF THE GALILEAN MOONS Trevor Picard
  • 2.
  • 3. • Background • Goals • Methods • Analysis • Results • Errors • Conclusions
  • 4. Astrometry: Optical Surveys • Past: POSS (89 million objects → primarily to study galaxy morphology) • Present: SDSS (500 million objects) • Future (2019): LSST (200,000 images/year) Source: Astrophysical Research Consortium (ARC) & Sloan Digital Sky Survey (SDSS)
  • 5. Astrometry: Applications • Instrumental in time-keeping (UTC) • Important rung of cosmic distance ladder • Exoplanet detection verification • Near-earth object tracking • Orbital Mechanics…
  • 6. • Background • Goals • Methods • Analysis • Results • Conclusions
  • 7. Project Goals • Determine the masses of the Galilean moons through astrometric observations. • Kepler’s 3rd Law: simplified 2-body problem • Knowing an object’s mass provides valuable insight into many other properties (ρave, gs, etc.) • Get as many measurements as possible to precisely and accurately infer orbital period and average orbital radius.
  • 8. • Background • Goals • Methods • Analysis • Results • Conclusions
  • 9. Tools: Pre-Observing Sky & Telescope Online Observing Tool: shows which moons will be visible at certain dates and times
  • 10. Tools: Pre-Observing HORIZON Interface: provided RA and Dec of Jupiter, current distance between Jupiter and Earth, actual values for calculated quantities (needed to calculate error)
  • 11. Observational Methods • MDM Observatory: 1.3-meter + 4K Imager • FOV: 0.31”/pixel, 21.3” span • Took images with U, g, and Y band filters ranging from 1- to 6- second exposures. • More frequent and numerous observations allows us to better infer p and a.
  • 15. • Background • Goals • Methods • Analysis • Results • Conclusions
  • 16. Periodic Regression Analysis • Mathematica: r (“) = A sin(B t + C) • r: the angular distance of the moon from Jupiter • t: time (minutes) • A: the max angular distance between Jupiter and each moon (amplitude) • B: used to find the orbital period (p = 2𝜋 / B). • B and C are used in combination to find the time of maximum elongation
  • 17. Calculations • r = dJupiter(A x π)/(3600 x 180) • Since dJupiter varies slightly over the course of our observations, we used B t + C = π/2 to find t(dmax). • Periodicity: 2π/B
  • 19. • Background • Goals • Methods • Analysis • Results • Conclusions
  • 20. Mass Discrepancy • MJ >> m → our calculated orbital radii still generated moon masses off by several orders of magnitude • Decided to use known values of orbital radii, but our own calculated periods (which were more accurate) to perform the calculations
  • 21. Example: Europa 0.042% error 3.551181 days (accepted) 3.55 days (observed) 1.17% error 0.6709 x 106 m (mean accepted) 0.6632 x 106 m (observed) 1.898 x 1027 kg4.7998 x 1022 kg
  • 22.
  • 23.
  • 24.
  • 25.
  • 26. Results • Periods: all extremely accurate (within 0.05%). • Orbital radii: Not precise enough to calculate masses. Io Europa Ganymede Callisto p (days) 1.77 3.55 6.10 16.69 Error in p (%) 0.002 0.042 0.008 0.006 a (106 km) 0.42113 0.66324 1.06920 1.87250 Error in a (%) 0.15 1.17 0.08 0.56
  • 27. Inferred Moon Properties Error was surprisingly small…
  • 28. • Background • Goals • Methods • Analysis • Results • Conclusions
  • 29. Sources of Error: Restrictions • Very few observations • short time span of observations • imprecise periodic fit in Mathematica
  • 30. Sources of Error: Random Error • Jupiter’s saturation → imprecise zero point • Clouds → improvised exposure times ?
  • 31. Sources of Error: Systematic Error • Instead of using barycenter, assumed a center of mass at Jupiter’s center. • Assumed circular orbits when they are actually elliptical.
  • 32. Conclusions Question: Is astrometry + Kepler’s 3rd Law a reasonable way to calculate masses? Answer: Maybe
  • 33. Summary • Astrometry is important (gives us our bearings). • Ellipticity, mass barycenter, orbit inclination, etc. must be accounted for. • Mass of orbiting bodies are often orders of magnitude smaller than the bodies they orbit, requiring very precise astrometry. • Astrometry requires many precise observations over long periods of time. • Doppler Shift > Astrometry for mass calculation.