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Climate Change November 4, 2014
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Global Climate Change Global Warming – describes a rapid increase in the temperature of Earth’s surface, water, and atmosphere, which is causing changing in most natural systems (such as seasons and life cycles)
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Global Temp Change since 1880
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Causes of Climate Change Variations in the Earth’s orbital characteristics Atmospheric variations in greenhouse gases Volcanic eruptions Variations in solar output Landforms
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Variations in the Earth’s orbital characteristics The Milankovitch theory – Cyclical variations in three of the Earth’s orbital characteristics Eccentricity Rotation Tilt – Vary the amount of solar radiation that reaches the Earth’s surface
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Milankovitch Cycles 1. 2. 3.
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Carbon Cycle
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Greenhouse Effect
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Carbon Dioxide Sources
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What are the Fossil Fuels?
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Greenhouse Gas-Temp Correlation from Ice Cores
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Volcanic Eruptions Sulfur dioxide reacts with water vapor causing haze Combined with ejected particulate matter One of the coldest years in the last two centuries was 1816, the “Year Without a Summer” Caused by eruption of Tambora in 1815 Temperatures can decrease after eruptions for up to 3 years Mount St. Helens
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Variations in Solar Output Climate models predict that a change in solar output of only 1 percent per century alters the Earth’s average temperature by 0.5°C (32.9°F) ̶ 1.0°C (33.8°F)
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Sea Level Rise
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Arctic Sea Ice Changes 2012
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GCM Predictions Crop patterns and natural plant/animal habitats will shift to maintain preferred temperatures During this century, climate regions could shift 90-350 miles poleward Soil moisture projected to decrease in midlatitudes Forest cover will undergo major species disturbances Expansion of zones affected by tropical diseases Alpine glaciers
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Reconstructing Climate Change Prior to recorded data, use Proxy Data: – Palynology - pollen in lake sediments shows veg type - > 15,000 year record – Dendrochronology - tree rings show growth patterns – 9000-yr record – Ice Cores – air trapped over 650K yrs shows past CO 2 concentrations
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Proxy Data Measures cause and effect relationships indirectly Paleoclimatology – science that studies past climates using proxy data Proxy data – ice cores, sediments, coral reefs, ancient pollen, tree-rings Antarctic ice cores have climate reconstructed back 740,000 years Air bubble in ice allow the reconstruction of atmospheric methane levels
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Tree-Ring Records
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Palynology
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Ocean Core Records
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