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MET 112 Global Climate Change – Lecture 10 Observations of Recent Climate Change Dr. Craig Clements San Jose State University Outline How do we observe? Recent trends in temperature Recent trends in GHGs
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What does to observe mean? Measurements –Of what? Who compiles these measurements for governments and society? IPCC: Intergovernmental Panel on Climate Change www.ipcc.ch Where do our observations come from? - to watch and record.
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Temperature stations
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Change in surface temperature in 20 th century
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Bubbles Trapped in ice core Petit, Jean-Robert, et al (1999). “Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica”. Nature 399: 429-436.
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Ice Core layers GISP2 ice core (Greenland Summit)GISP2ice core Archived at the National Ice Core Laboratory in CO. from 1837-1838 meters in which annual layers are clearly visible. The appearance of layers results from differences in the size of snow crystals deposited in winter versus summerwintersummer Counting such layers has been used (in combination with other techniques) to reliably determine the age of the ice. This ice was formed ~16250 years ago during the final stages of the last ice age and approximately 38 years are represented here.ice age
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Ice Cores
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Coring Earth’s ice sheets
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Coring mountain glaciers
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Ice core record
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Ice core CO 2 record
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Retreat of mountain glaciers: ‘visual inspection’ Boulder Glacier, Mt. Baker, Washington
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Retreat of mountain glaciers
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Melting of Greenland Icesheet
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Global rise in sea level last 20,000 years
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Global rise in sea level in the 20 th century
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Shorter winters in Alaska
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Latest global temperatures
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Current CO 2 : ~383 ppm
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What Changed Around 1800? Industrial Revolution –Increased burning of fossil fuels Also, extensive changes in land use began –the clearing and removal of forests
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Burning of Fossil Fuels Fossil Fuels: Fuels obtained from the earth are part of the buried organic carbon “reservoir” –Examples: Coal, petroleum products, natural gas The burning of fossil fuels is essentially –A large acceleration of the oxidation of buried organic carbon
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Land-Use Changes Deforestation: –The intentional clearing of forests for farmland and habitation This process is essentially an acceleration of one part of the short-term carbon cycle: –the decay of dead vegetation Also causes change in surface albedo (generally cooling)
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Greenhouse Gases Carbon Dioxide Methane Nitrous Oxide CFCs (Chlorofluorocarbons) Others
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Methane
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Anthropogenic Methane Sources Leakage from natural gas pipelines and coal mines Emissions from cattle Emissions from rice paddies
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Nitrous Oxide N 2 O
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Anthropogenic Sources of Nitrous Oxide Agriculture Bacteria in Soils Nitrogen fertilizers
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CFCs (Chlorofluorocarbons) CFC-11 CFC-12
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Sources of CFCs Leakage from old air conditioners and refrigerators Production of CFCs was banned in 1987 because of stratospheric ozone destruction –CFC concentrations appear to now be decreasing –There are no natural sources of CFCs
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Latest global temperatures
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The Land and Oceans have both warmed
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Precipitation patterns have changed
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