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Part 1: In this lesson we will be exploring the question, “What causes global warming?” We will be learning the current science that focuses on human causes, in particular CO2 emissions, but we will also look at the arguments of those who dispute this. At three points in the lesson we will analyze short video clips that weigh in on this controversy. Watch the following commercial and answer the questions on your worksheet. Video 1 – View video on website page Part 2: The commercial that was previously viewed was produced to sway public debate on the controversial issue of climate change. We will take a look at two more video clips that take contradictory positions. Part 3: Although most scientists think that the recent spike in global temperature is caused by anthropogenic CO2 concentrations in the atmosphere, there are dissenting opinions. We will now analyze clips from two documentary films that argue different sides of the debate. First you will to view a clip from a British documentary titled The Great Global Warming Swindle. Although you will not see it in its entirety, the documentary features many of the major players (scientists, economists, writers, etc.) that represent and work for organizations from the U.K., the U.S., and Canada who have been publically questioning and debating the role of anthropogenic CO2 in the current global warming trend. Watch the following video clip and answer the questions on your worksheet Video 2 - View video on website page Al Gore’s Academy Award-winning documentary, An Inconvenient Truth, has been credited with raising awareness about global warming. Politicians, industrialists, activists, and thousands of citizens have credited the movie with changing their opinion on climate change. But the film and filmmaker have plenty of critics, and some of the information in Gore’s film has been challenged. We will now watch one of the more controversial segments from An Inconvenient Truth and ask some of the same questions we did for The Great Global Warming Swindle. Watch the following video clip and answer the questions on your worksheet Video 3 - View video on website page Global Dimming (49 minutes) View video on website page What is global dimming? What is the cause? What does this mean for the greenhouse effect? If there is anytime remaining, show (73 min) “The Great Global Warming Swindle” View video on website page Bellwork What 2 things cause sea level rise when global temperatures increase? Potential Effects of Increased Mean Global Temperature Sea level rise Thermal expansion Ice melt Outcome Flooding of cities, estuaries, wetlands, reefs Beach erosion Disruption of fisheries Contamination of coastal aquifers with salt Potential Effects Coastal residents forced to migrate inland Results in overcrowding of inland cities Lack of infrastructure to support population Result in shortages of resources Potential Effects Increase in sea temperatures Results in more intense hurricanes and typhoons Potential Effects Increased temperature also changes the density of ocean water Affects the upwelling of deep ocean water Affects the global conveyor belt that moves the heat energy around the planet This could ultimately push the world climate into another ice age Potential Effects Effects on polar ice caps: Greenland ice sheet completely melts Slows/stops North Atlantic Drift (NAD) current by diluting the salt water. If the NAD current and the Gulf Stream slow/stop climate of the UK and Scandinavia would be much colder The melting of the Artic could open up trade routes allow for exploitation of undersea minerals and fossil fuel reserves. Methane clathrate is a form of ice under the Artic ocean floor that traps methane. If it were to melt and reach the surface, the release of methane might trigger a rapid increase in temperatures. Potential Effects Effects on biodiversity and ecosystems: Melting of tundra permafrost - release methane trapped in the frozen soils. Animals can move to cooler regions plants cannot. The distribution of plants can shift as they disperse seeds which germinate and grow in more favourable habitats could be too slow to stop them from becoming extinct Alpine, tundra, and polar species could become extinct Birds and butterflies have already shifted their ranges to higher latitudes. Plants are breaking their winter dormancy earlier. Loss of glaciers decrease the salinity of marine waters and changes to ocean currents alter habitats. Potential Effects Effects on food production: Higher temp = increase biochemical reactions (photosynthesis) Higher temp = increase in respiration – therefore no increase in NPP In Europe the crop growing season has expanded. If biomes shift away from the equator, there will be winners and losers. It depends on the fertility of soils as well. For example if production shifts northwards from the Ukraine with its rich black soils to Siberia with its thinner, less fertile soils, NPP will decrease. In seas, a small increase in temperature can kill plankton, the basis of many marine food webs. Agriculture Shifts in growing areas Changes in crop yields Increased irrigation demands Increases pests, crop diseases and weeds Potential Effects Effects on human health: malaria, yellow fever, and dengue fever could spread to higher latitudes. In a wetter climate fungal diseases will increase. In a drier climate dust increases leading to asthma and chest infections. Warmer temperatures in higher latitudes would reduce the number of people dying from the cold each year and reduce heating bills for households. Potential Effects Effects on human migration: If people can not grow food or find water, they will move to regions where they can. Global migration of millions of environmental refugees is quite possible and this would have implications for nation states, services and economic and security policies. The IPCC estimates that a 150 million refugees from climate change in 2050. Potential Effects Effects on national economies: Some economies would suffer if water supplies decrease or drought occurs. This could open up new resources such as tar sands in Canada and Siberia, which have been frozen under permafrost. If rivers don’t freeze hydroelectric power generation will be possible at higher latitudes. Agricultural production may increase in higher latitudes but fall in the tropics Impacts of Global Climate Change in U.S. Arid deserts in Southwestern U.S. will shrink as precipitation increases Savanna/shrub/woodland systems will replace grasslands in the Great Plains Eastern U.S. – forests will expand northerly – weather conditions will become more severe Southeastern U.S. – increasing droughts will bring more fires – triggering a rapid change from broadleaf forests to Savannas woodland shrub land grassland forest arid Present day grassland forest grassland grassland shrub land woodland Predicted Distribution Impacts of Global Climate Change Increases in evaporation in tropical areas Results in a change in global rain patterns Increased precipitation resulting in increased flooding Decreased precipitation may result in drought, crop failures and famine References Blasing, T. (2009, December). Recent greenhouse gas concentrations. Retrieved from http://cdiac.ornl.gov/pns/current_ghg.html Greenhouse gases frequently asked questions. (2010, February 23). NOAA Satellite and Information Service. Retrieved from http://lwf.ncdc.noaa.gov/oa/climate/gases.html Our changing climate. United States Global Change Research Program [Image]. Retrieved from http://www.globalchange.gov/component/content/article/52-reports-and-assessments/343our-changing-climate Smith, S. M., & Owens, H. B. (2003, June). Investigating the Climate System. SPECS (The Secondary Education in Computational Science project) (1996, August 21). The Electromagnetic Spectrum [Chart]. Retrieved from http://www.lcse.umn.edu/specs/labs/glossary_items/em_spectrum.html United Nations Environment Programme & GRID-Arendal (2010). Planet and atmospheres [Diagram]. Retrieved from http://www.climateark.org/overview/01.asp Working Group I. (2007). Fourth Assessment Report of the Intergovernmental Panel on Climate Change (S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. Averyt, . . . H. Miller, Eds.). Cambridge, United Kingdom: Cambridge University Press.