Earth Astronomy 311 Professor Lee Carkner Lecture 12
Terra -- The Earth Goddess Greeks and Romans personified the Earth as a mother goddess
Earth Facts Size: km diameter Orbit: 1 AU (1.5 X 10 8 km) Description: wet, temperate, inhabited
Earth’s Celestial Motions Earth is tilted on its axis by 23 1/2 degrees Earth has large satellite, The Moon May stabilize tilt of axis
Earth’s Atmosphere Composition: small amounts of water vapor, CO 2 other gasses Very different from other atmospheres
Early Atmosphere Where did the original atmosphere come from? Early composition: Carbon dioxide (CO 2 ) Water (H 2 O) Methane (CH 4 ) Ammonia (NH 3 )
Formation of Atmosphere Start with CO 2, H 2 O, CH 4, NH 3 C, H, O form H 2 O, CO 2 CO 2 dissolves in H 2 O, H 2 O rains out to form oceans, N 2 left behind Final atmosphere -- O 2 and N 2
Earth’s Atmosphere
Temperature Temperature and composition of Earth’s atmosphere is regulated by the carbonate-silicate cycle Surface temperature stays near the point where water is mostly liquid
Climate The atmosphere circulates due to convection (hot thing rise, cool things sink) Two basic sources of convection The Earth’s rotation breaks the atmosphere up into convection cells that keep the air circulating, producing global weather patterns
The Earth’s Surface What shapes the Earth’s surface? Also, volcanoes and cratering Unlike other planets the Earth does not have many craters Craters on Earth are largely obliterated by erosion
Plate Tectonics The two top layers of the Earth are the crust and the mantle Crust is broken up into plates that float on the upper mantle Plates move around and crash into each other forming trenches and mountains
How Plate Tectonics Work
Plate Boundaries
Water The Earth has more liquid water on its surface than any other planet Water is present on Earth in all three phases (ice, liquid water, vapor) and continuously cycles between them
Water on the Earth
Effects of Surface Alteration Plate tectonics and erosion alter the Earth’s surface Earth’s surface is constantly changing
Plate Collision -- The Himalayas
The Grand Canyon
Meteor Crater
The Earth’s Interior The crust and atmosphere are very thin compared the rest of the planet (like the skin of an orange) We learn about them by studying the seismic waves from earthquakes
Seismic Waves Types of waves: P waves: pressure or compression wave S waves: shear waves The different densities of the inner earth refract the waves When an earthquake occurs we can measure the strength of S and P waves all over the Earth
Earthquake Studies of the Earth’s Interior
Seismic Waves and the Earth’s Interior No S waves detected on opposite side of Earth There is a shadow zone where no P or S waves are detected Very faint P waves detected in shadow zone Refracted by solid inner core
Structure of the Earth Crust: surface to 35 km Mantle km Outer core km Inner core km Density increases toward the center
Structure of the Earth
Earth’s Magnetic Field Rotation and the motions of the liquid iron core produce a magnetic field via the dynamo effect This magnetic field helps shield the Earth from the solar wind
The Earth’s Magnetosphere
The Habitable Zone In order to support life a planet must be in the habitable zone Width of zone determined by the effectiveness of the carbonate-silicate cycle Inner Edge -- Outer Edge -- For our solar system habitable zone width is about AU
Hypothetical Habitable Zone Too hot, water is destroyed can’t remove CO 2 Too cold, try to warm up with more CO 2 but CO 2 forms clouds and blocks sunlight Just right, temperature kept stable at ~273 K (water is liquid)
Why is the Earth Habitable? It has the right temperature for liquid water (~273 K) because: Has both water and plate tectonics for carbonate-silicate cycle
Summary Earth is unique for at least two reasons Large amounts of liquid water Large amounts of free oxygen Earth has liquid water and life because it is in the habitable zone
Summary: Atmosphere Earth’s initial atmosphere composed of CHON Mild temperature maintained by carbonate-silicate cycle
Summary: Surface Solid iron inner core, liquid iron outer core, solid mantle and crust Plate tectonics and erosion constantly alter surface