Contents of the Solar System

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Transcription:

The Solar System

Contents of the Solar System Sun Planets 9 known (now: 8) Mercury, Venus, Earth, Mars ( Terrestrials ) Jupiter, Saturn, Uranus, Neptune ( Jovians ) Pluto (a Kuiper Belt object?) Natural satellites (moons) over a hundred Asteroids and Meteoroids 6 known that are larger than 300 km across Largest, Ceres, is about 940 km in diameter Comets Rings Dust

Size matters: radii of the Planets

Sun: Jupiter: Earth: Moon = 110:11:1:1/4

The Astronomical Unit A convenient unit of length for discussing the solar system is the Astronomical Unit (A.U.) One A.U. is the average distance between the Earth and Sun About 1.5 10 8 km or 8 light-minutes Entire solar system is about 80 A.U. across

The solar system is a disk, not a sphere

The Terrestrial Planets Small, dense and rocky Mercury Mars Venus Earth

The Jovian Planets Large, made out of gas, and low density Saturn Jupiter Uranus Neptune

Asteroids, Comets and Meteors Debris in the Solar System

Most asteroid orbits are situated between Mars and Jupiter Asteroids

Asteroid Discovery First (and largest) Asteroid Ceres discovered New Year s 1801 by G. Piazzi, fitting exactly into Bode s law: a=2.8 A.U. Today more than 100,000 asteroids known Largest diameter 960 km, smallest: few km Most of them are named about 20 of them are visible with binoculars

Most asteroids are very small

Comets - Traveling Dirty Snowballs Small icy bodies, dirty snowballs Develops a tail as it approaches the Sun

Comet Anatomy Tail may be up to 1 A.U. long Ion tail points away from sun

Shapes Comet Giacobini- Zinner (1959) Ion tail 500,000 km long Coma: 70,000 km across Comet Hale-Bopp (1997) Tail 40 long as seen from earth

Halley s Comet a typical Comet Highly eccentric orbit, inclined substantially

Halley s Comet Now and then Halley s Comet in 1910 Top: May 10, 30 tail Bottom May 12, 40 tail Halley s Comet in 1986 March 14, 1986

Comet Shoemaker-Levy 9 Headed for Jupiter

Impact on Jupiter

Meteor Showers caused by comets Radiant Duration Quadrantids (QUA) Dec. 28-Jan. 7 Lyrids (LYR) Apr. 16-25 Eta Aquarids Apr. 21-May 12 Beta Taurids June 30 Delta Aquarids July 25-31 Perseids (PER) Aug. 10-14 Draconids Oct. 6-10 Orionids (ORI) Oct. 15-29 Taurids Oct.12- Dec 2 Leonids (LEO) Nov. 14-20 Geminids (GEM) Dec. 6-19

Most probably caused the extinction of the dinosaurs Impact on Earth

Impact Craters Quebec's Manicouagan Reservoir. Large meteorite landed about 200 million years ago. The lake, 45 miles in diameter, now fills the ring. Barringer Crater, AZ 0.8 mi diameter, 200 yd deep; produced by impact about 25,000 years ago

Tunguska ~30 m body struck Siberia in 1908 Energy equal to that of a 10 Megaton bomb! Detonation above ground; several craters

2013: Siberia Again! 1000 people injured as 20m rock strikes Explodes about 20km overhead 16 hours before known non-fatal asteroid encounter

Frequency of Impact Events

The Earth-Moon System Earth/Moon radius: ¼ Earth/Moon mass: 1/81 Earth-Moon distance: 384,000 km

Features of the Earth & Moon Mass: Earth: 6 10 24 kg Radius: Earth: 6400 km Moon: 1/81 Earth s Moon: 1/4 Earth s ra Density: Earth: 5500 kg/m 3 Moon: 3300 kg/m 3 5.5 times that of water About 2 times that of a rock Gravity: Earth: 9.8 m/s 2 Moon: 1/6 Earth s gravity (about the same as in water)

Core Mostly iron and nickel Inner core solid, outer core liquid Mantle Mostly basalt, a heavy mineral containing iron and magnesium Soft; can flow even though it is solid rock Crust Solid surface layer; floats on the mantle Structure of the Earth Density and temperature both increase with depth

78% Nitrogen, 21% Oxygen, 1% Other Troposphere region of weather Stratosphere stable and calm Ionosphere gases charged by interaction with radiation from space Earth s Atmosphere

Ozone Layer (O 3 ) Absorbs most UV radiation from the Sun Hole over Antarctic Chlorofluorocarbons (CFC s) released by spray cans, refrigerators

Earth absorbs energy from the Sun and heats up Earth re-radiates the absorbed energy in the form of infrared radiation The infrared radiation is absorbed by carbon dioxide and water vapor in the atmosphere Greenhouse Effect

Magnetosphere Magnetic north pole about 7 west of geographic north pole Driven by motion of molten metals in core

Magnetic field/shield: Motion of Charged Particles Charged particles trapped by magnetic fields Origin of the Van Allen radiation belts Protects us!

Aurora Borealis from Space