Lecture 20 - Uranus and Neptune Lecture Notes

Uranus and Neptune

Discoveries of Uranus and Neptune

  • Uranus and Neptune are the 7th and 8th planets from the Sun, respectively.
  • They are gas giants (Jovian planets), similar to Jupiter and Saturn.
  • These planets are so far away that ancient astronomers were unaware of them.
  • Uranus was discovered in 1781 by William Herschel using a telescope, marking the first planet discovered in over 2000 years.
    • It is barely bright enough to be seen without a telescope, and only under ideal conditions if you know exactly where to look.
  • Herschel noticed an object that moved relative to background stars and realized it was not a star or comet.
  • Voyager 2 flew by Uranus in 1986, providing the first up-close images of the planet.
    • The upper atmosphere appeared nearly featureless, with only a few wispy clouds in the northern hemisphere.
  • The orbit of Uranus was found to deviate from a perfect ellipse; the discrepancy grew to 15 arc-seconds over 50 years.
  • In 1845-6, John Adams and Urbain Le Verrier independently deduced that another body was causing the orbital anomaly of Uranus.
    • They used Newton's Laws to predict the location of an eighth planet.
    • In late 1846, astronomer Johann Galle discovered Neptune within one or two degrees of the predicted location.
    • The mathematicians, Adams and Le Verrier, received credit for the discovery, and the planet was named Neptune.
  • Like Uranus, details of Neptune cannot be discerned from Earth-based telescopes.
  • Voyager 2 flew by Neptune in 1989, providing the first close-up pictures.
    • Neptune's upper atmosphere shows more features than that of Uranus, including cloud streaks ranging from 50 km to 200 km wide.

Orbital and Physical Properties

  • The period of Uranus' orbit is P=83.75P = 83.75 Earth years.
  • Kepler's Third Law can be used to calculate Uranus' semimajor axis, aa, using the formula: P2 (in Earth years)=a3 (in AU)P^2 \text{ (in Earth years)} = a^3 \text{ (in AU)}.
    • Solving for aa gives: a=(83.75)2/3 AU=19.2 AUa = (83.75)^{2/3} \text{ AU} = 19.2 \text{ AU}.
  • Uranus' orbit has an eccentricity of e=0.047e = 0.047.
    • The distance from Uranus to the Sun varies by about 10% during its orbit.
    • Perihelion: 18.3 AU
    • Aphelion: 20.1 AU
  • Observations of parallax of Neptune show that its semimajor axis is a=30.1 AUa = 30.1 \text{ AU}.
  • Kepler's Third Law can be used to calculate Neptune's orbital period, PP.
    • Solving for PP gives: P=(30.1)3/2 years=164 yearsP = (30.1)^{3/2} \text{ years} = 164 \text{ years}.
  • Neptune's orbit has an eccentricity of e=0.009e = 0.009.
    • The distance from Neptune to the Sun varies by about 2% during its orbit.
    • Perihelion: 29.8 AU
    • Aphelion: 30.3 AU
  • Neptune's orbital period is 164 years.
    • Since its discovery in 1846 (173 years ago), Neptune has completed just over one orbit around the Sun.
  • Like other Jovian planets, Uranus and Neptune rotate quickly and exhibit differential rotation.
  • The rotation period of Uranus is 17.2 hours, based on magnetic field measurements.
  • Unlike other Jovian planets, Uranus' spin axis is tilted by 98 degrees, which is almost perpendicular to its orbital axis.
  • The rotation period of Neptune is 16.1 hours, based on observations of its magnetic field, and the tilt of Neptune's spin axis is 29.6 degrees.
  • Due to Uranus' axial tilt of 98°, the planet experiences extreme seasons.
    • Its equatorial regions have two summers at the equinoxes (42 years apart) and two winters at the solstices, with its poles plunged into darkness for 42 years at a time.
  • During Uranus' solstices, when the northern hemisphere points toward the Sun, almost the entire southern hemisphere is in total darkness (and vice versa).
  • The reason for Uranus' large axial tilt is not well understood but might be the result of collisions during the solar system's formation.
  • Uranus' physical properties:
    • Radius: 25,559 km = 4.0 R⊕
    • Mass: 8.68×1025 kg=14.5M8.68 × 10^{25} \text{ kg} = 14.5 M⊕
    • Density: 1270 kg/m3
    • 27 moons (as of 2021)
    • Faint rings discovered from Earth
  • Neptune’s physical properties:
    • Radius: 24,766 km = 3.9 R⊕
    • Mass: 1.02×1026 kg=17.1M1.02 × 10^{26} \text{ kg} = 17.1 M⊕
    • Density: 1640 kg/m3
    • 14 moons (as of 2021)
    • Faint rings discovered by Voyager 2
  • Neptune and Uranus are very similar.

Atmospheres of Uranus and Neptune

  • Spectroscopic studies of reflected sunlight show that the outer atmospheres of Uranus and Neptune have a similar composition to those of Jupiter and Saturn, but with more methane (CH4\text{CH}_4).
    • Hydrogen (H2\text{H}_2): 84 %
    • Helium (He): 14 %
    • Methane (CH4\text{CH}_4): 2 %
    • Almost no Ammonia (NH3\text{NH}_3)
  • Abundances of ammonia (NH<em>3\text{NH}<em>3) and methane (CH</em>4\text{CH}</em>4) vary systematically across the Jovian planets.
    • Jupiter has more gaseous ammonia than methane.
    • Uranus has more gaseous methane than ammonia.
    • As distance from the Sun increases, the amount of ammonia in a planet's atmosphere decreases relative to methane.
    • Temperature is the reason: ammonia freezes into crystals at 70 K.
    • Since the upper atmosphere of Uranus is 58 K, ammonia does not exist as a gas, but as ice.
  • Methane is a good absorber at longer wavelengths (red light).
    • A higher concentration of methane means more red light is absorbed by the atmosphere, so the planet has a more bluish color.
    • The blue-green color of Uranus results from methane in its atmosphere.
  • The cloud-top temperature on Uranus is around 58 K, which is below the freezing point of ammonia.
    • This temperature is close to the predicted equilibrium value at that distance from the Sun.
    • Unlike the other Jovian planets, Uranus lacks an internal heat source.
  • Low amounts of high-level clouds mean that weather patterns (storms) cannot readily be seen, as they are blocked by high atmospheric haze.
  • High winds (200 km/h to 500 km/h) form bands like Jupiter, but are buried deeper in the atmosphere.
  • Uranus' atmosphere is efficient at transporting energy around the planet; the temperature difference between winter and summer sides is only a few K.
  • Wind speeds near the poles are higher than at the equator, probably due to the higher amount of sunlight these regions receive.
  • Composition of Neptune's atmosphere:
    • Hydrogen (H2\text{H}_2): 86.1 %
    • Helium (He): 13.8 %
    • Methane (CH4\text{CH}_4): 3%
    • Almost no Ammonia (NH3\text{NH}_3)
  • Neptune's atmosphere is similar in composition to Uranus', except that there is more methane (3% compared to 2% on Uranus), giving it a more blue appearance.
  • Despite being farther from the Sun, Neptune's upper atmosphere is slightly warmer than Uranus'.
  • Neptune has an internal heat source that is responsible for pronounced weather patterns.
    • High-level clouds are observed, and several storm systems are clearly visible from space.
    • The most prominent storm was the Great Dark Spot, observed by Voyager 2.
  • The Great Dark Spot was similar to Jupiter's storms.
    • Wind speeds exceeded 1500 km/h.
    • It was roughly the size of Earth.
    • By the time Hubble images were taken in 2011, the Great Dark Spot had disappeared for unknown reasons.
  • Other large storms have appeared and disappeared on Neptune since Voyager 2.
  • These storms are much more short-lived than those on Jupiter.

Magnetospheres and Internal Structure

  • Uranus and Neptune have strong magnetic fields, about 100 times stronger than Earth's.
  • Unlike other planets, their magnetic fields are inclined at large angles with respect to their rotation axes.
    • Uranus: 60°
    • Neptune: 40°
  • Unlike other planets, the magnetic fields of Uranus and Neptune are significantly off-center.
    • This suggests different physics are responsible for their magnetic fields.
    • Their magnetic fields must not be produced by dynamos, as other planets' fields are.
  • Theoretical models suggest that Uranus and Neptune have rocky cores similar to Jupiter and Saturn (about 10 Earth masses).
  • Uranus and Neptune are smaller than Jupiter and Saturn.
    • The rocky cores of Uranus and Neptune make up a larger fraction of the planet compared to Jupiter and Saturn.
  • Pressure outside the cores of Uranus and Neptune is too low to form metallic hydrogen.
    • The origin of the magnetic field is therefore probably very different than Jupiter and Saturn.
  • A possible