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Climate & the Carbon Cycle Earth is a closed system. Carbon is not gained or lost, it just cycles through the different spheres (Atmosphere; Hydrosphere;

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Presentation on theme: "Climate & the Carbon Cycle Earth is a closed system. Carbon is not gained or lost, it just cycles through the different spheres (Atmosphere; Hydrosphere;"— Presentation transcript:

1 Climate & the Carbon Cycle Earth is a closed system. Carbon is not gained or lost, it just cycles through the different spheres (Atmosphere; Hydrosphere; Geosphere; Biosphere) Atmospheric CO2 is a GHG. It traps I.R. energy radiated from Earth’s surface; temperatures increase.

2 Climate Change: Global Warming Global Warming = Increase in air and ocean temperatures. Due to changes in Earth’s Energy Budget.

3 Greenhouse Effect & CO2 Greenhouse Gases = Gases that prevent I.R. wavelengths from E’s surface from escaping to outer space. CO2 = GHG

4 Measuring Carbon Dioxide in the Atmosphere Ice Cores: Gas bubbles trapped in ice are miniature atmospheres that can be studied. Measured directly from. Mauna Loa

5 Carbon Dioxide Levels CO2 levels are determined from gas bubbles trapped in ice (Vostock Lake, Antarctica) Temperatures can be determined from 18O:16O ratios.

6 CO2 levels are determined from gas bubbles trapped in ice (Vostock Lake, Antarctica) Temperatures can be determined from 18O:16O ratios.

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8 Evidence of Global Warming: Measured increases in Carbon Dioxide Levels Modern CO2 levels measured at Mauna Loa Observatory, Hawaii

9 Evidence of Global Warming: Increasing Sea Surface Temperatures & Sea Level Rise

10 Evidence of Global Warming: Glacial Retreats

11 Carbon Cycle: Key Ideas Reservoirs: a term used to describe the compartments that contain carbon in some form (e.g.: atmosphere, soil, water, in plants, etc) Photosynthesis: CO 2 from atmosphere turned into “sugar” Respiration: cells convert sugars from food into CO 2 Fossilization: processes involving extreme pressures that turn various kinds of carbon into fossil fuels (coal, crude oil, natural gas) Sedimentation: material settles to bottom of aquatic system Food Chain: carbon is transferred up the food chain as animals consume plants and other animals. Eventually, upon death, the carbon is returned to soil and sediments. Volcanism: volcanoes can cycle carbon back to the atmosphere. As rock melts to form magma, carbonate (CO 3 -2 ) is turned into CO 2 Chemical Weathering: Carbon dioxide from air dissolves in water to form carbonic acid. Carbonic acid weathers rock surfaces. Combustion: fires or burning of fossil fuels returns carbon to the atmosphere

12 Atmospheric CO 2 Carbon in Trees, Plants, Algae CO 2 Dissolved in Ocean Carbon in Animals Carbonate (CaCO 3 ) in shells, etc Carbon in Sediment Carbon in Fossil Fuels Carbon in Soil Carbonate (CaCO 3 ) Rock (limestone) uptake dissolving Uplift & Mt. Building exposes new rock

13 Atmospheric CO 2 Carbon in Trees, Plants, Algae CO 2 Dissolved in Ocean Carbon in Animals Carbonate (CaCO 3 ) in shells, etc Carbon in Sediment Carbon in Fossil Fuels Carbon in Soil Carbonate (CaCO 3 ) Rock (limestone) Respiration Bacterial Respiration photosynthesis Food Chain fossilizationpressure uptake Chemical weathering burning firesdissolving Uplift/Mt. Buidling exposes new rock volcanoes

14 Volcanism ADDS CO2 to the atmosphere. Mt. Building & the chemical weathering of new rock REMOVES CO2 from the atmosphere. Geosphere   Atmosphere

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16 Atmosphere   Hydrosphere  Geosphere CO2 gas Dissolved CO2 used by plankton which die Plankton settle to bottom of ocean floor. Sediment layers become rock.

17 Biosphere  Geosphere Plankton use dissoved CO2 in water for photosynthesis. Plankton die (or are consumed/decomposed by other organisms, which die). Dead plankton bring carbon to the ocean floor where it will become ROCK.

18 Warming or Cooling?  Increased volcanism?  Increase in mountain building & weathering?  Deforestation?  Increased photosynthesis by marine plankton?  Increased frequency of forest fires?  Increased combustion of fossil fuels?  Decreased volcanic activity  Increased use of solar energy or wind power.

19 Ways to Reduce atmospheric CO2?  Reduced volcanism?  Mountain building & increased weathering?  Increased photosynthesis?  Increased absorption of CO2 by ocean?  Changing land use (forests, urban areas, etc.)?  Increase the amount or rate that carbon becomes rock?  Decrease combustion of fossil fuels?

20 Results of increased levels of CO2  Increased atmospheric and sea surface temperature.  Ice caps/glaciers melt.  Flooding of coastal areas due to sea level rise.  Droughts in some locations/increased productivity in others.  Decrease in salinity of ocean water changes ocean circulation (& climate patterns).  Ocean acidification (dissolved CO2 forms an acid in water)  reef organisms dissolve  Increase in insect borne (tropical) diseases (Malaria, etc.)  Economic loses.

21 Results of Global Warming Flooding due to rise in sea level. Change in “who” grows food. Coral reefs die b/c acidification.

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