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Astronomy 161
Introduction to Solar System Astronomy
Prof. Paul Martini

Lecture 29: Overview of the Solar System


Key Ideas:

The Solar System contains:
The Sun
Terrestial Planets
Jovian Planets
Giant Moons
Dwarf Planets
Smaller rocky and icy bodies (asteroids, comets, etc.)


The View from Afar

What observations can we make of the planets without leaving Earth?
Orbits: direction, ellipticity, tilt (or inclination), distance
Rotation: speed, tilt
Number and sizes of moons
Masses and radii (and thus density)
Reflectivity, presence of craters
Spectroscopy (temperature, chemical composition)


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
Dwarf Planets: Pluto, Eris, Ceres
Giant Moons
Icy bodies: Icy moons, Kuiper Belt Objects, Comets
Rocky bodies: 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
About 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
The abundance of the Sun is nearly equal to that of the entire Solar System


Terrestrial Planets

Mercury, Venus, Earth, and Mars
"Earth-like," rocky planets
Largest is the Earth
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


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)


The Giant Moons

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


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

Five 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
Haumea
Makemake


Trans-Neptunian Objects

Any object that orbits at the distance of Neptune or beyond
Three regions
Kuiper Belt from 30-50 AU (e.g. Pluto)
Scattered Disk out to 100s of AU (e.g. Eris, Quaoar)
Oort Cloud postulated to exist 50,000 to 100,000 AU from the Sun (e.g. Sedna???)
More than 1000 objects orbit beyond Neptune. Only a small number (e.g. Pluto and Charon) were known prior to 1992.


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


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: 2010 February 14 Copyright © Paul Martini All Rights Reserved.