Global Climate Change - Chapter 18

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LauraDT  on April 13, 2012

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Global Climate Change - Chapter 18

Climate changes
Contributing to the complex evolutionary history of the earth system
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Climate changes Contributing to the complex evolutionary history of the earth system
Earth system Interactions between atmosphere and oceans and solid earth and biosphere
Weather What is occuring now or in the near future in terms of temperature, pressure, cloudiness, precipitation
Climate Average of the weather over longer time periods
Monitoring Regular collection of data for a specific purpose
Real-time monitoring Collecting data while a process is actually occuring
Major climate zones Controlled by global circulation and movement of air masses
Nitrogen (78%)
Oxygen (21%)
Argon (0.9%)
Carbon Dioxide (0.03%)
Atmosphere is mainly
1. Amount of sunlight
2. Amount of solar energy reflected and absorbed
3. Amount of heat retention
Temperature of earth determined by 3 factors
Electromagnetic radiation Earth receives energy from the sun in the form of
Hotter objects More electromagnetic energy is emitted from
Greenhouse effect Trapping of heat in the atmosphere by water vapor, carbon dioxide, methane, and chlorofluorocarbons
Equal When in balance the total carbon dioxide emissions and removals from the entire carbon cycle are
Burning of oil, coal and gas Human activities that increase CO2 concentrations in atmosphere
Methane Important greenhouse gas
Bacteria in marsh areas (70%) Biggest discharge of methane comes from
Coal mining
Landfills
Natural gas production
Domesticated livestock
Total = 50%
Human activities that result in methane release
Instrumental record Started in 1860s today temperature measured at about 7000 stations around the world
Historical record People's written recollections of the Medieval Warm period and the Little Ice Age
Medieval Warming Period 300 year period where earth was considerably warmer than normal
Little Ice Age Mind 1400-1700. Resulted in crop failures, climate can have tremendous effect on population
Paleo-Proxy Record Study of past eliminate has provided some of the strongest data to support and test theories of recent change
Tree rings Growth of trees influenced by climatic conditions
Pollen If climate cools there will be a change in the assemblage of pollen in sediments that reflects the change in climate
CO2 and Methane in Ice Cores Measurement in this confirm the link between greenhouse gas levels and global warming
Global warming The observed increase in the average temperature of the near-surface land and ocean environments of earth
Carbon 14 Produced in upper atmosphere by collisions between neurons and nitrogen-14
14, 7.5 Since, US emissions of CO2 have increased by __%, CH4 by __%
Eemian Last major interglacial warm period, even warmer than today (sea level was also a few meters higher than it is today)
1970s Most of the increase in climate as been in the
Ocean Conveyor Belt- global circulation of ocean water, may contribute to change
- warm surface water is transported westward and northward to near Greenland, where it cools from contact with cold Canadian air
- as water increases in density, it sinks to the bottom and flows south, then east to the Pacific, where upwelling occurs
Positive forcing Earth will warm
Negative forcing Earth will cool
1.5, 4.5 Doubling greenhouse gases cause _ to _ degree increase in average global temperature
Glacial ice Forms as snow accumulates over a period of years, is compressed from the weight of overlying snow, and recrystallizes as a granular ice known as firn
10 Glacial ice only covers __% of the earth
CO2 and methane Thawing of permafrost releases
50 Permafrost affects __% of Canada
Expand and rise Warming of the ocean causes the sea water to

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