Exosphere mostly hydrogen, weather satellites are here polar climate zone high pressure, sea ice most of the year biosphere all the living things on earth doldrums no wind, happens in the equatorial climate zone coal, oil, natural gas sources of CO2 glacial retreat, decreased snow cover, shrinking ice sheet, extreme everts evidence of climate change 1-4 feet How much the sea level could rise by 2100. weather conditions of the atmosphere at a particular time and place climate long-term average of weather, includes precipitation and temperature atmosphere extends from the ground up and into space methane produced from landfills and cattle ocean acidification When there is too much CO2 in the ocean. greenhouse effect when gases in the atmosphere trap heat energy from the sun Proxy data indirect evidence thermosphere Where the Hubble and ISS orbit equatorial climate zone rising air and doldrums CO2 product of burning fossil fuels water vapor 66-85% of greenhouse effect cryosphere all the frozen water on Earth stratosphere contains the ozone layer hydrosphere all the liquid water on Earth Paleoclimatology the study of ancient climates Glacial ice rings used to determine climate of the past including CO2 levels geosphere interior and exterior of Earth Ionosphere conducts electricity and the auroras form here Milankovitch Theories Eccentricity, obliquity, and Precession Exosphere mostly hydrogen, weather satellites are here polar climate zone high pressure, sea ice most of the year biosphere all the living things on earth doldrums no wind, happens in the equatorial climate zone coal, oil, natural gas sources of CO2 glacial retreat, decreased snow cover, shrinking ice sheet, extreme everts evidence of climate change 1-4 feet How much the sea level could rise by 2100. weather conditions of the atmosphere at a particular time and place climate long-term average of weather, includes precipitation and temperature atmosphere extends from the ground up and into space methane produced from landfills and cattle ocean acidification When there is too much CO2 in the ocean. greenhouse effect when gases in the atmosphere trap heat energy from the sun Proxy data indirect evidence thermosphere Where the Hubble and ISS orbit equatorial climate zone rising air and doldrums CO2 product of burning fossil fuels water vapor 66-85% of greenhouse effect cryosphere all the frozen water on Earth stratosphere contains the ozone layer hydrosphere all the liquid water on Earth Paleoclimatology the study of ancient climates Glacial ice rings used to determine climate of the past including CO2 levels geosphere interior and exterior of Earth Ionosphere conducts electricity and the auroras form here Milankovitch Theories Eccentricity, obliquity, and Precession
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mostly hydrogen, weather satellites are here
high pressure, sea ice most of the year
all the living things on earth
no wind, happens in the equatorial climate zone
sources of CO2
evidence of climate change
How much the sea level could rise by 2100.
conditions of the atmosphere at a particular time and place
long-term average of weather, includes precipitation and temperature
extends from the ground up and into space
produced from landfills and cattle
When there is too much CO2 in the ocean.
when gases in the atmosphere trap heat energy from the sun
indirect evidence
Where the Hubble and ISS orbit
rising air and doldrums
product of burning fossil fuels
66-85% of greenhouse effect
all the frozen water on Earth
contains the ozone layer
all the liquid water on Earth
the study of ancient climates
used to determine climate of the past including CO2 levels
interior and exterior of Earth
conducts electricity and the auroras form here
Eccentricity, obliquity, and Precession
