chapter d1
the biosphere:
weather: short term, hard to predict, acedotal
climate: long term, easier to predict, more general
the atmosphere
layer of gases that surrounds the earth
nitrogen (78%)
oxygen (20.9%)
methane (0.97%)
trace amounts of argon, carbon dioxide, neon, helium
soot, pollen, microorganisms
four layers of the earths atmosphere
troposphere (0-10) km
80% of atmospheric gases and dust
avg temp 15 degrees celsius
temp decreases w altitude
only part of the atmosphere that can support life
where most weather occurs
stratosphere (10-50) km
ozone layer
-60 degrees celsius
mesosphere (50-80) km
thermosphere (80-500) km
hydrosphere
all water on earth
97% salt water in oceans
3% freshwater
lithosphere
chapter d2
thermal energy
solar energy
insolation
insolation and the angle of incidence
angle of incidence: angle between a ray falling on a surface and the line perpendicular to it
angle of incidence of incoming solar radiation increases as you move from the equator to the poles, due to the curvature of the earth
angle of inclination: degree that the earths poles r tilted from the perpendicular plane of orbit (23.5)
seasons
season changes are the result of earths inclination of orbit