Lecture 6: Solar System / Earth Flashcards
1
Q
Earth
A
- Strong magnetic field
- Differentiated interior
- Active Surface
2
Q
Planetary Interiors
A
- Seismic Waves, Magnetic Fields, Surface Features, and Gravitational Deviations are the best way to determine the inside of a planet
3
Q
Earthquake Waves
A
- P waves are primary or pressure waves and are the fastest seismic waves
- S waves are secondary or shear waves
- Surface waves are slower than S and P waves
4
Q
Earth Seismic Waves
A
- Waves refract depending on different things
- Temperature and density increase with depth
- heat generate dis proportional to planet’s mass
- Heat escapes through planet’s surface
5
Q
Heating vs. Cooling of Planets
A
- Heating mechanisms are proportional to mass, volume or radius cubed
- Cooling mechanisms are proportional to surface area or radius squared
- Larger bodies cool more slowly
6
Q
Planetary magnetic fields
A
- A rotating metallic core will act as a dynamo and produce a magnetic field
- Earth’s magnetic field comes form charged particles in its outer liquid core
- Solar wind distorts shape of magnetosphere
- Aurora’s are caused by solar winds with magnetic field (northern lights)
7
Q
Planetary Surfaces: Earth
A
- The surface of a planet can give clues to what’s happening inside the planet
- Continental drift causes constant changes to surface (mountains)
- Erosion of surface, meteorite impacts
- North America result of subduction, collisions, volcanism, erosion, and sedimentary deposits
8
Q
Techtonic Plates
A
- Can compress or stretch the crust
- Can slide along each other and pull apart, causing earthquakes and rift valleys
9
Q
Volcanism
A
- An upwelling of molten rock (magma) from deep within the planet to the surface
- Can cover up old surface features and make new ones, as well as produce additional gas
- Caused by Techtonic plates and thermal plumes
10
Q
Impact Cratering
A
- Features depend on speed, angle, impactor, and surface material, and are different from volcanic craters
- Small craters bowl shaped
- Large craters have central peak and concentric rings, multiring basins
11
Q
Erosion
A
- Atmosphere and Surface Water act to level the surface
- Acts on all scale
- Chemical Reactions
12
Q
Planetary Atmospheres: Earth
A
- CO2 has increased in the last 50 years likely due to global warming
- Surface Temperature is a combination of solar heating, infrared radiation trapped by cloud layer, and hot interior
- Climate depends on heating and rotation
- Atmosphere blocks some light, transmits others
13
Q
Atmospheric Mass Change
A
- Greenhouse effect heats surface
- Atmospheres gain mass due to outgassing, evaporation, and impacts
- Atmospheres lose mass by thermal escape, solar winds, impacts, condensation, and chemical reactions
14
Q
Atmospheric Heating
A
- Warm air rises near the equator and cools as it gets to the poles
- Circulation cell in each hemisphere
- Rotation affects atmospheric circulation
- Coriolis Effect causes circulation cells to divide into three cells per hemisphere