C13 - Atmosphere Flashcards
C13 - Earth’s early atmosphere
Similar to the atmosphere of mars
Mostly carbon dioxide
Small amounts of nitrogen
No oxygen
C13 - Earth’s current atmosphere
78% nitrogen
21% oxygen
0.04% carbon dioxide
C13 - Evolution of Earth’s atmosphere
Early volcanic activity produced the atmosphere
As the Earth cooled, water vapour condensed to from oceans
Evolution of algae 2.7billion years ago oxygenated the planet
Over the next few billion years oxygen levels increase
Carbon dioxide levels decrease as it is absorbed by plants and as it is incorporated into the tissues of living organisms
C13 - Explain how the earth’s atmosphere evolved
Early atmosphere mostly carbon dioxide and little oxygen - due to volcanic activity.
Nitrogen produced by volcanoes gradually builds up in atmosphere.
The water vapour from volcanic eruptions condensed to form oceans.
Carbon dioxide dissolved in ocean water reducing the carbon dioxide in the atmosphere.
Algae evolved and produced the first oxygen.
Plants evolved and percentage of oxygen increased. This increases to a level that enables animals to evolve.
C13 - Greenhouse gases
Carbon dioxide - from respiration and combustion (burning fossil fuels)
Methane - from swamps, rice fields, landfill sites and grazing cattle
Levels off both of these gases are increasing
C13 - Explain how the greenhouse effect causes an increase in global temperatures.
Radiation from the sun enters the earth’s atmosphere and warms the surface of the planet.
The earth’s surface becomes hotter and radiates heat back out.
Some of this heat is absorbed by greenhouse gases. These gases then radiate the heat back towards earth.
The atmosphere becomes hotter as a result.
C13 - What are the effects of global warming
Loss of habitat
Changes in distribution
Changes in migration patterns
Reduced biodiversity
C13 - solving global warming
Carbon footprint: the total amount of carbon dioxide and other greenhouse gases released over the life cycle of a product
Carbon capture and storage: pumping carbon dioxide from fossil fuel power stations deep underground to be absorbed into porous rock.
Reduced demand for beef: this would reduce the amount of grazing cattle and thus the amount of methane.
Biofuels: carbon neutral fuels that lead to no net increase in carbon dioxide levels.