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Climate Change Climate is what we expect, weather is what we get. ~Mark Twain
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Climate Average weather conditions of the Earth or a particular area Main focus: temperature & precipitation Minimum period: 3 decades
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Climate Change: Historical Radioisotopes in rocks & fossilsrocks Plankton & radioisotopes in ocean sediments Pollen from the bottom of lakes & ponds Tree rings Ice cores Regular temperature measurements (1861)
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Climate Change
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Climate Change: Historical Volcanic Emissions Changes in solar input Impacts by meteors Changes in air & ocean circulation
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Climate Change: Human Activities Significant increase in greenhouse gases (CO 2, CH 4, & N 2 O) since mid-1700s –Industrial revolution –Burning fossil fuels –Deforestation –Agriculture
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Carbon dioxide (CO2) Year 1800190020002100 260 310 360 410 Parts per million Fig. 18.4a, p. 450
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Methane (CH 4 ) Year 1800190020002100 0.6 1.2 1.8 2.4 Parts per million Fig. 18.4b, p. 450
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Year Parts per million 1800190020002100 260 290 300 310 320 Fig. 18.4c, p. 450 Nitrous Oxide
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Year 199020002025205020752100 100 150 200 250 Index (1900 = 100) Carbon dioxide Methane Nitrous oxide Fig. 18.5, p. 451
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Intergovernmental Panel on Climate Change (IPCC) Earth’s lower atmosphere is warming Most increase in gases are due to human activities Combo of human induced changes to air composition & temperature of the atmosphere are beginning to change the Earth’s climate Increased greenhouse gas conc. will likely trigger a significant climate disruption this century Climate disruption will have ecological, economic, & social effects
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IPCC (2010) 1906–2005: Ave. temp increased about 0.74˚C 1970–2009: Annual greenhouse emissions from human activities up 70% 2000-2009 warmest decade since 1881 Past 50 years: Arctic temp rising almost twice as fast as the rest of the earth Melting of glaciers and increased floating sea iceMelting of glaciers Last 100 years: sea levels rose 19 cm
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Key Players in Climate Change Carbon Dioxide Waste Heat Solar Input Oceans Cloud Cover
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CO2 Emissions Role Mainly burning of fossil fuels –Burning forest (agriculture) –Deforestation 1850: 285 ppm 2010: 389 ppm 2050: 560 ppm Tipping point: 450 ppm
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Carbon Emitters (2009) Total 1.China 2.United States 3.European Union(27) 4.Indonesia 5.Russia Per Capita 1.Australia 2.United States 3.Canada 4.Netherlands 5.Saudi Arabia
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Heat Waste Burning fossil fuels Main sources –Combustion engines –Power plant –Lights
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Solar Input No correlation between increased solar input & increase temperatures Since 1975 –Troposphere warmer –Stratosphere cooler
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Oceans Carbon Sink –Absorbs 25=30% of anthropogenic CO 2 –Cooler temps = increased absorption Warmer Oceans –Average temp = increase 0.32-0.67 ⁰ C –Less CO 2 absorptions Ocean Acidity –Increased 30% in last 200 years –Affects: coral bleaching, phytoplankton populations, & ability to absorb CO 2
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Cloud Cover Increase temp = increased evaporation = increase in clouds Low clouds: decrease surface temp High clouds: increase surface temp
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Climate Change Possible Effects…
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Droughts Severe/prolonged droughts affect 30% of Earth Consequences: –Increased wildfires –Decrease in water –Decrease in agriculture
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More Ice & Snow Melt
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Arctic Temperatures have risen at twice the rate Mountain glaciers affected by: –Average snowfall –Average temperatures Mountain glaciers supply water to rivers
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Permafrost Melt Releases methane
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Permafrost Melt
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Sea Level Rising Prediction: 0.8-2 meter rise by 2100
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Sea Level Rise Effects Degradation of coastal estuaries & wetlands Disruption of coastal fisheries Coastal flooding –Shanghai –New York –Miami –Bangkok –Calcutta Area floods with one meter rise
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Sea Level Rise Effects Flooding of low-lying barrier islands Area floods with one meter rise
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Sea Level Rise Effects Flooding of agriculture lowlands & deltas Saltwater contamination of freshwater
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Extreme Weather Increase Heat waves Hurricanes –increase 0.8°C = increase in storms by 1/3 –Intensity increase by 45% Flooding/droughts increase
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Threat to Biodiversity Most susceptible areas: –Coral reefs –Polar seas –Coastal areas –Tundra Organisms with limited ranges & temperature tolerance
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Agriculture Regions of farming may shift –Decrease at tropics & subtropics –Increase in northern latitudes Low productivity because of low soil quality
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Human Health Temperature related death increase Increase in insects, molds, & microbes
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Climate Change What can we do…
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Difficult to do... Global issue Long term political issue Impacts are not distributed evenly Proposed solutions disrupt economies & lifestyles
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Ways to Manage Greenhouse Gases Improve energy efficiency Increase use of renewable resources Stop deforestation Shift to more sustainable agriculture
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Collect Greenhouse Gases Massive tree planting Restore wetlands Plant perennials on degraded land Preserve and restore natural forests Stimulate phytoplankton growth
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Government Involvement Strictly regulate CO 2 and CH 4 Carbon tax on fossil fuelsCarbon tax Cap and trade approach Increase subsidies to encourage energy efficiencyefficiency
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Kyoto Protocol 1997 treaty to slow climate change Reduce CO 2, CH 4, & N 2 O emissions by 5.2% by 2012 Not signed by US
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