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Chapter # 21 Global Climate Change. Overview o Introduction to Climate Change Causes of Global Climate Change Causes of Global Climate Change o Effects.

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Presentation on theme: "Chapter # 21 Global Climate Change. Overview o Introduction to Climate Change Causes of Global Climate Change Causes of Global Climate Change o Effects."— Presentation transcript:

1 Chapter # 21 Global Climate Change

2 Overview o Introduction to Climate Change Causes of Global Climate Change Causes of Global Climate Change o Effects of Climate Change Melting Ice and Rising Sea Level Melting Ice and Rising Sea Level Changes in Precipitation Patterns Changes in Precipitation Patterns Effects on Organisms Effects on Organisms Effects on Human Health Effects on Human Health Effects on Agriculture Effects on Agriculture o Dealing with Global Climate Change

3 Climate Change- Mean Annual Global Temperature 1960-2005

4 Climate Change Terminology o Greenhouse Gas Gas that absorbs infrared radiation Gas that absorbs infrared radiation Ex: Carbon dioxide, methane, nitrous oxide, chlorofluorocarbons and tropospheric ozone Ex: Carbon dioxide, methane, nitrous oxide, chlorofluorocarbons and tropospheric ozone o Positive Feedback Change in some condition triggers a response that intensifies the changed condition Change in some condition triggers a response that intensifies the changed condition o Infrared Radiation Radiation that has a wavelength that is longer than that of visible light, but shorter than that of radio waves Radiation that has a wavelength that is longer than that of visible light, but shorter than that of radio waves o Greenhouse Effect Increase of heat in a system where energy enters (often as light), is absorbed as heat, and released sometime later Increase of heat in a system where energy enters (often as light), is absorbed as heat, and released sometime later

5 Climate Change o Evidence for Climate Change 11 of the 12 years between 1995 and 2006 were among the twelve warmest years since the mid-1800s 11 of the 12 years between 1995 and 2006 were among the twelve warmest years since the mid-1800s Phenological spring in N. hemisphere now comes 6 days earlier Phenological spring in N. hemisphere now comes 6 days earlier o Warming is not due to natural causes Human produced greenhouse gases are most plausible explanation Human produced greenhouse gases are most plausible explanation

6 Causes o Greenhouse gas concentrations increasing

7 o Increased concentration of CO 2 (right) Burning fossil fuels in cars, industry and homes Burning fossil fuels in cars, industry and homes Deforestation Deforestation Burning of forests Burning of forests Causes

8 Greenhouse Effect

9 Other Pollutants Cool the Atmosphere o Atmospheric Aerosols tend to cool the atmosphere Both human and natural sources Both human and natural sources Tiny particles that remain in troposphere for weeks or months Tiny particles that remain in troposphere for weeks or months Contain many chemicals, but often contain sulfur Contain many chemicals, but often contain sulfur o Complicates models of climate change

10 Climate Models o Climate affected by: winds, clouds, ocean currents, and albedo winds, clouds, ocean currents, and albedo o Used to explore past climate events o Advanced models can project future warming events o Models are only as good as the data and law used to program them They have limitations They have limitations

11 Climate Models

12 Effects of Global Climate Change o Ocean as CO 2 sink - excess CO 2 is starting to harm ocean life

13 Effects of Global Climate Change- Melting Ice and Rising Sea Levels o Sea level rise caused in 2 ways Thermal Expansion Thermal Expansion Water expands as it warms Water expands as it warms Melting of land ice Melting of land ice Retreat of glacier and thinning of ice at the poles Retreat of glacier and thinning of ice at the poles o Melting has positive feedback Increased melting decreases ice, which decreases albedo leading to further warming Increased melting decreases ice, which decreases albedo leading to further warming

14 Melting Ice and Rising Sea Levels 1957 1998

15 Case-In-Point Impacts in Fragile Areas o Eskimo Inuit live traditional life dictated by freezing climate o Climate change is altering their existence Wildlife are smaller or displaced Wildlife are smaller or displaced Reduced snow cover and shorter river ice seasons Reduced snow cover and shorter river ice seasons Thawing of permafrost (right) Thawing of permafrost (right)

16 o Some areas will get more water, some areas will have greater droughts Ex: Hurricanes will likely get stronger Ex: Hurricanes will likely get stronger Effects of Global Climate Change- Changing Precipitation Patterns

17 o Zooplankton in parts of California Current have decreased by 80% since 1951 Effecting entire food chain Effecting entire food chain o Decline in krill around Antarctica Caused decrease in penguin populations Caused decrease in penguin populations o Species have shifted their geographic range o Migrating birds are returning to summer homes earlier Food is not available at this time Food is not available at this time Effects of Global Climate Change- Effects on Organisms

18 Effects on Organisms - Coral Reefs o Coral reefs can be bleached (right) due to increase in water temperature Affects coral symbiotes and makes them more susceptible to diseases to which they would otherwise be immune Affects coral symbiotes and makes them more susceptible to diseases to which they would otherwise be immune

19 Effect on Organisms - Vegetation Beech Tree Range

20 Effects on Human Health o Increased number of heat-related illnesses and deaths

21 Effects on Agriculture o Difficult to anticipate Productivity will increase in some areas and decrease in others Productivity will increase in some areas and decrease in others o Rise in sea level will inundate flood plains and river valleys (lush farmland) o Effect on pests is unknown o Warmer temperatures will decrease soil moisture- requiring more irrigation o Location (i.e. elevation and altitude) where certain crops can be grown may have to change

22 International Implications of Climate Change o Developed vs. Developing countries Differing self-interests Differing self-interests Differing ability to meet the challenges of climate change Differing ability to meet the challenges of climate change

23 Dealing with Global Climate Change o To avoid the worst of climate change, CO 2 levels must be stabilized at 550ppm 50% higher than current levels 50% higher than current levels o Two ways to attempt to manage climate change Mitigation Mitigation Focuses on limiting greenhouse gas emissions to moderate global climate change Focuses on limiting greenhouse gas emissions to moderate global climate change Adaptation Adaptation Focuses on learning to live with to the environmental changes and societal consequences brought about by global climate change Focuses on learning to live with to the environmental changes and societal consequences brought about by global climate change

24 Dealing with Global Climate Change- Relationship Between Mitigation and Adaptation

25 Dealing with Global Climate Change- Mitigation o Locate/invent alternative fuels to fossil fuels o Increase efficiency of cars and trucks o Sequestering carbon before it is emitted o Plant and Maintain trees to naturally sequester carbon

26 Dealing with Global Climate Change- Adaptation o Rising sea levels and coastal populations Move inland Move inland Construct dikes and levees Construct dikes and levees o Adapt to shifting agricultural zones o NYC sewer line

27 “There were rumors of unfathomable things, and because we could not fathom them we failed to believe them, until we had no choice it was too late.”

28 Ozone Depletion o Stratospheric ozone o UV light o Chemical processes o Environmental effects o Solutions

29 Atmosphere o Stratospheric ozone o 20-30 km altitude o 19 mi at equator, 9 mi at the poles o 400 ppb

30 Ozone shield o 99% of all UV is absorbed (UVC and most UVB) o UVA is not affected by ozone

31 Production of ozone

32 Measurement of Ozone o Dobson units: 1 ppb ozone o Survey began in 1957 over the Antarctic o Taken in October, springtime o 1957-1970: 300 DU o 150 DU by 1986

33 Ozone and CFC’s o Molina and Rowland in 1974 o CFC’s are stable o Long residence in lower atmosphere o UV radiation breaks down CFC and releases Cl o Cl reacts with O 3 o Increase UVB at the surface

34 Formation and destruction of ozone

35 Emissions

36 Usage Usage 2003

37 Ozone Hole

38 Polar Stratospheric clouds o Polar winter formation o Have polar vortex o Isolated air mass o Nitrogen oxides held in clouds as nitric acid o NO 3 particles grow and fall out o Facilitates ozone depleting reactions

39 Polar vortex In Springtime, sunlight Returns No nitrate to form CloNO2

40 Environmental effects o UV damage to DNA o Skin cancer o Cataracts o Suppression of immune system o Ecosystem: o Primary producers o Food chains o Development in aquatic larva

41 Managing ozone depletion o Montreal protocol, Sept 1987– Production of CFC elimination o Economic gap o Replacements: HFC and HCFC o Shorter lifetime, less reactive o Collection and reuse (no venting) o Expensive replacements

42 Climate Change o Climate Swings o Greenhouse gases o Evidence o Predictions o Control

43 Historic Climate shifts o Milankovitch cycles: shifts in earth‘s orbit and tilt o Volcanic activity: Mt. Toba

44 El Nino/Southern Oscillation o Trade winds keep warm water in W. Pacific. La Nina o El Nino: Shift in tropical depression o Northern Jet stream splits changes rainfall patterns o Pacific decadal oscillation: warm water in northern pacific moves back and forth. o Cool water in north help Alsaka salmon runs, warm off coast and then switches.

45 Human Activities o Industrialization o CO 2 increased 31%, CH 4 inc 151%, N 2 O inc 17% over since pre- industrial times. o 40% of excess CO 2 absorbed by oceans o Methane a big problem

46 Evidence of Climate Change o Avg global temperature has climbed 0.6 o C over last century o Arctic sea ice is 40% thinner, Antarctic glaciers are retreating 50m/yr. o Alpine glaciers are retreating o Ocean acidification o Sea level has risen o Changes in animal behavior, breeding cycles o Storm frequency and intensity are increasing

47 Larsen B ice shelf-- Antarctica

48

49 Consequences Arctic sea ice Alpine glaciers

50 Predictions Sugar maple range Predicted warming with doubling of CO 2

51 Controls

52 Reduction of Carbon Emissions o Burn less fossil fuel: Turn down your thermostat o Plant Trees for shade and CO 2 uptake o Insulate your house o Replace old appliances o Use compact fluorescence light bulbs o Use renewable energy


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