climate
chapter d1
the biosphere:
thin layer of earth
conditions suitable for supporting life
all living things on earth
contains all the spheres
weather: short term, hard to predict, acedotal
temp
air pressure
cloud cover
precipitation
humidity
particular place, particular time
climate: long term, easier to predict, more general
avg weather conditions
over a long period of time
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
temp ranges from 0-100 celsius
thermosphere (80-500) km
contains very little gases
temp: -100 - 1500 celsius '
hydrosphere
all water on earth
97% salt water in oceans
3% freshwater
lithosphere
solid portion of earth
rocks minerals elements
100km below surface
warmed by energy from the sun
chapter d2
thermal energy
temperature is a measure of thermal energy
energy possessed by a substance due to its kinetic energy
solar energy
radiant energy
transmitted as electromagnetic waves
insolation
amount of energy received by a region of the earths service
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
chapter d1
the biosphere:
thin layer of earth
conditions suitable for supporting life
all living things on earth
contains all the spheres
weather: short term, hard to predict, acedotal
temp
air pressure
cloud cover
precipitation
humidity
particular place, particular time
climate: long term, easier to predict, more general
avg weather conditions
over a long period of time
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
temp ranges from 0-100 celsius
thermosphere (80-500) km
contains very little gases
temp: -100 - 1500 celsius '
hydrosphere
all water on earth
97% salt water in oceans
3% freshwater
lithosphere
solid portion of earth
rocks minerals elements
100km below surface
warmed by energy from the sun
chapter d2
thermal energy
temperature is a measure of thermal energy
energy possessed by a substance due to its kinetic energy
solar energy
radiant energy
transmitted as electromagnetic waves
insolation
amount of energy received by a region of the earths service
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