the earth in space. the solar system inner planets
TRANSCRIPT
The Earth in Space
The Solar SystemInner Planets
The Earth-Moon-Sun System
Phases of the Moon
The Moon’s Orbit and Rotation
The Moon makes 1 rotation per orbit. Why?
(Solid) Tides
The Moon is pulled into anoblong shape So is the Earth,
but to a lesser extent.Mostly the oceans are affected
Putting on the Brakes on the Early Moon
Earth pulls on the moonSlowing it down
Eventually the Moon’s rotation slowed toonce per revolution
Putting on the Brakeson the Earth
Moon pulls on the Earth’s oceans, which sloshagainst the continents. This slows down the Earth.
Our days are getting longer by about 0.016 seconds per century400 Ma ago, the day was 22 hours long! (400 days/year) (coral)900 Ma ago, the day was 18 hours long! (486 days/year) (sed rx)
Seasons, Tropics, and Circles
How hot would the Earth be if there was no atmosphere?
• What is the average temperature of the moon?– The moon’s soil is ~252 K, or -21°C on
average (Little et al, 2001, AGU Abstracts)• (K = °C + 273.15)
Blackbody RadiationObservation: When something gets hot, it
begins to glowFirst, dark redThen, bright redThen, yellowEventually, blue
Note: This is NOT related to which part of a flame is hottest
Blackbody Radiation
Infrared
Ultr
avio
let
• Maximum Wavelength?– Wien Displacement Law Max (m) = 2898/T
• Total amount of Energy Emitted– Stefan-Boltzmann Law– E (W/m2) = 5.7 x 10-8 T4
• T in degrees Kelvin
Blackbody Radiation
Blackbody Radiation
• What’s the Point?– Any body, at any temperature greater than
absolute zero, is emitting light– Cool objects emit light we can’t see with
our naked eye (in the infrared)– Emitting light means that the objects are
emitting energy (in the form of light), and thus are losing energy
So, what temperature should the Earth be?
• It’s a simple calculation:– Energy hitting the Earth from the Sun must
equal the energy leaving the Earth– 1367 W/m2 is hitting the Earth from the Sun
• But 30% of it is reflected back to space– Albedo = 0.3
• Leaving 973 W/m2 at the Equator
We have to figure out what the AVERAGE amount of light is hitting the entire Earth
This is the amount hitting the Earth at the Equator (973 W/m2)
Times the area of the EARTH’S DISK (=r2)
Divided by the Earth’s total SURFACE AREA (=4r2)
So, what temperature should the Earth be?
• It’s a simple calculation:– Energy hitting the Earth from the Sun must
equal the energy leaving the Earth– 1367 W/m2 is hitting the Earth from the Sun
• But 30% (planetary albedo) of it is reflected back to space, leaving 973 W/m2 at the Equator
• So, there’s an average of 243 W/m2 over the entire surface
– (5.67 x 10-8 * T4) W/m2 are leaving the Earth
So, what temperature should the Earth be?
• The Answer: -18.3°C – The average temperature of the Earth is really ~
15°C– The Greenhouse effect is ~33°C [ 15° - (-18°) ]
• 4 Ga ago, the sun was 30% fainter, but the Earth was warmer– Equilibrium temperature with faint early sun: -40°C
• A Paradox?
What Impacts Insolation?
• Sunspots– 11 year cycle
• The Eccentricity of the Earth’s Orbit– 100 ka cycle and a 413 ka cycle
What Impacts Insolation?
• The Tilt of the Earth’s Axis– 41 ka cycle
What Impacts Insolation?
WarmerSummer
CoolerSummer
• The wobble of the Earth’s axis and its orbit (precession) - 23 ka cycle
What Impacts Insolation?
11,500 years ago
26 ka 112 ka
What is the impact of changes in insolation?
• How much of a difference does 30 W/m2 make?
• -18.99°C to -17.59°C
• A range of 1.4°C
Earth’s Orbit in the News….
Aurorae
• Aurora Australis (Southern Hemisphere)
• Aurora Borealis (Northern Hemisphere)
http://dotearth.blogs.nytimes.com/2008/11/14/from-above-animated-aurora/?hp
The Magnetosphere
• The Earth has a Magnetic Field that extends into space
The Solar Wind• The Sun emits charged particles that
spew into space– The amount of particles increase during
high sunspot activity– And coronal mass ejections (solar flares)
Contact, the origin of the aurorae
Aurorae on other planets
• Also– Mars– Neptune