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Astronomy 171
Solar System Astronomy
Prof. Paul Martini

Lecture 30: Overview of the Solar System


Key Ideas:

The Solar System contains:
The Sun
Terrestial Planets
Jovian Planets
Dwarf Planets
Giant Moons
Smaller rocky and icy bodies (asteroids, comets, etc.)
What can we learn about the Solar System without leaving Earth?


Getting Goofy Over Pluto

The discovery of additional, 'pluto-sized' objects in the outer solar system led to a recent reconsideration of the definition of a planet
In August 2006 the International Astronomical Union adopted the new category of 'dwarf planet'
A Dwarf Planet is defined to be a celestial body that:
Is in orbit around the Sun
Must be in hydrostatic equilibrium due to its mass (must be round)
Has not cleared the neighborhood around its orbit
Is not a satellite


The Dwarf Planets

Three official (so far):
Pluto: Formerly the ninth planet, now the second-largest dwarf planet
Ceres: Largest member of the asteroid belt
Eris: Largest dwarf planet, whose discovery started the controversy


The Neighbors

Sun
A star (middle-aged, average-sized)
Terrestrial Planets
Rocky planets: Mercury, Venus, Earth, Mars
Jovian Planets
Gas/Ice giants: Jupiter, Saturn, Uranus, Neptune
The Rest
Pluto, Eris, Ceres
Icy bodies: Icy moons, Kuiper Belt Objects, Comets
Rocky bodies: Giant moons, asteroids


Basic Properties of the Planets

Location:
Terrestrial in the inner solar system: 0.4 - 1.5 AU
Jovian in the outer solar system: 5 - 30 AU
All orbit in the same direction and same plane:
Orbit counterclockwise, in the same sense as the rotation of the Sun
These facts provide clues to the formation of the Solar System


The Sun

A middle-aged, average star:
Mostly Hydrogen and Helium
99.8% of the entire Solar System
~4.6 Gyr old
Shines because it is hot:
Surface temperature ~6000 K
Mostly emits UV, visible, and infrared light
Kept hot by nuclear fusion in its core
Builds Helium from Hydrogen fusion
Can shine for ~12 Gyr
The Sun contains nearly all of the mass in the Solar System. Therefore the abundance of elements in the Sun is nearly equal to that of the entire Solar System.


Terrestrial Planets

Mercury, Venus, Earth, and Mars
"Earth-like," rocky planets
Earth is the largest terrestrial planet
Only found in the inner solar system (0.4 to 1.5 AU)
Rocky Planets:
Solid surfaces
Mostly silicates and iron
High density: 3.9-5.5 g/cm3 (rock and metal)
Earth, Venus, and Mars have atmospheres
Their composition is very different from the Sun


Jovian Planets

Jupiter, Saturn, Uranus, and Neptune
Largest planets: at least 15 times the mass of the Earth
Jupiter is the largest at 318 Earth masses
Only found in the outer solar system (5 to 30 AU)
Gas Giants:
No solid surfaces (mostly atmosphere)
Mostly Hydrogen and Helium
Rocky/icy inner cores
Low density: 0.7 to 1.7 g/cm3 (compare to water at 1 g/cm3)
Their composition is very similar to the Sun


The Giant Moons

Natural satellites orbiting planets
Giant Moons:
Earth: The Moon
Jupiter: Io, Europa, Ganymede, and Callisto (the Galilean moons)
Saturn: Titan
Neptune: Triton
Many smaller moons, both rocky and icy
Only Mercury and Venus have no moons


Trans-Neptunian Objects

Any object that orbits at the distance of Neptune or beyond
Split into three distinct regions
Kuiper Belt Objects (KBOs) from 30-50 AU (e.g. Pluto)
Scattered Disk Objects (SDOs) out to 100s of AU (e.g. Eris, Quaoar)
Oort Cloud is postulated to exist 50,000 to 100,000 AU from the Sun (e.g. Sedna???)
Since 1992 more than 1000 objects have been discovered beyond the orbit of Neptune. Only a small number (such as Pluto and Charon) were known previously.


Discovery of Eris (2003 UB 313)

Announced in August 2005
Larger than Pluto (and bigger than the Moon)
Highly inclined, very elliptical orbit
Aphelion at ~98 AU
Has a moon (Dysnomia)
Named for the Greek goddess of strife and discord. Apt choice, considering this object's impact on the astronomical community (and Pluto)


Atmospheres (or Not)

Jovian Planets:
Massive and cool enough to retain all elements, including light gasses
Terrestrial Planets and Moons:
Not always massive enough, or cool enough, to retain everything


The Leftovers (Minor Bodies)

Asteroids:
Made of rock and Metal (density of 2-3 g/cm3)
Sizes: 500 km (Ceres) to large boulders
Meteoroids:
Bits of rock and metal
Sizes: grains of sand to boulders
Comets:
Composite of rock and ice ("dirty snowballs")
Long tails of gas and dust are swept off them when they pass near the Sun


The Golden Age of Exploration

The Solar System has been explored with robotic spacecraft and astronauts
Landed men on the Moon
Robotic landers on the Moon, Venus, Mars, Titan, and the asteroid 433 Eros
Returned rocks from the Moon
Probed the atmospheres of Venus, Mars, and Jupiter
Flown spacecraft past all planets, and one on the way to Pluto
Mapped Venus and parts of Titan with radar
Flown by asteroids, comets, and returned comet dust to Earth


See A Note about Graphics to learn why some of the graphics shown in the lectures are not reproduced with these notes.

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Updated: 2007 February 19 Copyright © Paul Martini All Rights Reserved.