CGS NS 202 Final: NS Final pt 6

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Ex: england growing season shortened by 1-2
Atmospheric Conditions
o Greenhouse gases
CO2
Miocene Epoch: 25 mya
CO 2 level as high as today
o Methane and water vapor
o Soot in the atmosphere
Volcanic events
Asteroid impacts
Human Activity and Climate Change
Anthropogenic climate change: alterations in longer-term atmospheric conditions caused by human activities
History of thought
o 1869: Svante Arrhenius
Introduces idea that fossil fuel burning might increase CO2 levels
Suggests this enhanced greenhouse effect
o 1958: Charles Keeling
Develops accurate method for measuring CO2 in the atmosphere
Evidence CO2 increasing in atmosphere each year
Human Additions of Greenhouse Gases
o Agricultural Revolution
Cutting and burning forests
Domestication of cows and sheep (CH4)
o Iron Age
Cut forests and burn wood to make charcoal for Iron Age furnaces
o Industrial Revolution
Burning of Fossil Fuels
Addition of carbon to the Atmosphere
o Coal, Petroleum and Natural Gas
High energy carbon fuels produced and stored in prehistory
Each year *25 billion tons of CO2 are added to atmosphere by burning fossil fuels
o Deforestation/Human Land Use
o Forest fires and burning of wood for fuel
Black carbon: absorbs light and warms the atmosphere
Falls on glaciers and snow
o Synthetic greenhouse gases
CFC compounds
Refrigerants, cleaning solvents, plastic foam products
Absorb light 10,000-20,000x more than CO2
Estimating Global Temperature
o Patterns of temperature variation in many locations
o Benchmark
Average annual temperature over specific time interval
o Temperature Anomaly
Difference between years average temperature and benchmark
Positive anomaly: year is warmer than benchmark
Negative Anomaly: year is cooler than benchmark
A warmer planet
o Water absorbs more heat energy
Accelerates ice melting
o Increased energy to atmospheric circulation cells
Greater precipitation in some areas
Intense drying in other areas
Ecosystems will alter
Increase of productivity due to nutrient addition
o Phytoplankton, algae, seaweeds, grow quickly on surface
o Cause dead zone below them
Prevent light from penetrating surface
Prevent oxygen from being absorbed by organism living beneath them
Decomposition on sea floor uses up oxygen
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