8.6 - global warming
TRANSCRIPT
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8.6 – Global Warming
8.6.1 – Describe some possible models of global warming.
Records showing the history of the Earth’s temperature have illustrated the apparent
existence of global warming in the past few hundred years. There are a number of complex
atmospheric models currently in existence, including:
Changes in the composition of greenhouse gases in the atmosphere, due to
increased human combustion of fossil fuels and the natural diffusion of CO2 and
water vapour from oceans
Increased solar flare activity
Cyclical changes in the Earth’s orbit
Volcanic activity
Continental drift affecting the ocean currents and winds
8.6.2 – State what is meant by the enhanced greenhouse effect.
Greenhouse gas emissions from the burning of fossil fuels has increased the concentration
of carbon dioxide, nitrous oxides and CFC’s in the atmosphere, and the melting of
permafrost regions in the world and deforestation have increased levels of methane, which
then leads to infrared radiation increasing temperatures. The enhanced greenhouse effect is
the increase in greenhouse gasses in the atmosphere due to human activities.
8.6.3 – Identify the increased combustion of fossil fuels as the likely major cause of the
enhanced greenhouse effect.
Although still under investigation, Intergovernmental Panel on Climate Change (IPCC)
released a report stating that they believed that the observed increase in global
temperatures is likely due to human activities, such as the increased burning of fossil fuels
and the release of Carbon Dioxide.
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8.6.4 – Describe the evidence that links global warming to increased levels of greenhouse
gases.
Each year, as snow falls on the Arctic Circle, the atmospheric concentrations of gasses that
were present in that year are retained in the snow. This means that through interpretation
of arctic ice core drills, scientists are able to observe the fluctuations in atmospheric
temperature and greenhouse gas concentrations. Ice cores showing up to 420,000 years of
snowfall have been drilled in the Russian Antarctic base, Vostok, and these samples present
a correlation between global temperature and atmospheric greenhouse gas concentrations.
Additionally, tree rings can provide information into seasons and water precipitation levels
during the growth of the tree, and sedimentary records can be used to identify the seasonal
fluctuations in water levels of lakes. Core samples taken from the seabed of oceans can
establish a continuous and accurate record of historical surface sea-temperatures.
8.6.5 – Outline some of the mechanisms that may increase the rate of global warming.
There are a number of mechanisms that can increase the rate of global warming. These
include the following factors:
Due to the melting of ice, more of the Earth’s surface is covered by water as a result
of rising sea levels. Because of the positive feedback generated by the decrease in
albedo, more ice melts into water, which again lowers the albedo, causing the
temperature to rise, melting more ice.
The rising sea level as a result of the ice melting also causes a higher evaporation of
water vapour. As a greenhouse gas, the water vapour will continue heat the
atmosphere.
Higher temperatures in the water reduces the solubility of CO2, allowing less to
diffuse from the atmosphere into the water.
Changing forests to dry land through deforestation causes an increase in albedo,
causing more radiation to be reflected back to the atmosphere rather than absorbed
and used in carbon fixation. Burning the trees after they have been cut down also
increases the presence of CO2 in the atmosphere.
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8.6.6 – Define coefficient of volume expansion.
The coefficient of volume expansion is the fractional change in volume per degree change in
temperature.
Sea level rises are not only due to the melting of ice, but also because of the higher volume
taken up by water. Water is at its highest density (lowest volume) at 4oC, as it contracts
between 0 and 4oC, then expands at temperatures higher than 4oC.
Given a volume at a temperature of , the volume after a temperature change of will
increase by given by
Where is the coefficient of volume expansion, in K-1 or oC-1.
8.6.7 – State that one possible effect of the enhanced greenhouse effect is a rise in mean
sea level.
Changes in mean sea level affect the amount of water that can evaporate and the amount
of thermal energy that can be exchanged with the atmosphere. Also, changes in sea level
can affect ocean currents, which can influence the dispersal of heat between warm and cold
water.
8.6.8 – Outline possible reasons for a predicted rise in mean sea level.
The change in sea level is a natural occurrence caused by varying atmospheric pressure,
plate tectonic movements, wind, tides, increased rainfall, flow of large rivers into oceans
and changes in water salinity. However, an increase in the greenhouse effect could lead to
increase in Earth’s temperature, which would melt ice and snow causing the water level to
rise. It is important to notice that when the ice on water melts it does not result in a change
in sea level, as the weight of the ice is equal to the weight of the displaced water, and so
when the ice melts it will occupy a volume equal to the volume of the displaced water. As
such, only the melting of ice on land will result in a change of sea level.
Precise predictions are difficult to make due to factors such as:
Anomalous expansion of water
Different effects of ice melting on sea water compared to ice melting on land
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8.6.9 – Identify climate change as an outcome of the enhanced greenhouse effect.
We have seen from charts of CO2 levels and temperature from the past that a correlation
exists between the two. As there has been a significant increase in the emission of
greenhouse gases in the past hundred years, we can infer that the recent change in climate
is a result of the release of greenhouse gasses, the enhanced greenhouse effect.
8.6.10 – Solve problems related to the enhanced greenhouse effect.
E.G. a) The area of the Earth’s oceans is around 3.6×108 km2, with an average depth of
3.7 km. Assuming the coefficient of volume expansion of water of 2×10-4 K-1, estimate the
expected rise in sea level due to a temperature increase of 2 K
Therefore, the increase in volume:
So, the change in height:
b) Radiation of intensity 340 Wm-2 is incident on a lake of depth 50 m. Determine the
time required to increase the water temperature by 1 K.
By recognising that the power per area incident on the lake = 340 Wm-2, we know that
Therefore:
( )
As such, power per unit area is:
Therefore, change in temperature per time is equal to:
So, to find the time taken, the reciprocal is:
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8.6.11 – Identify some possible solutions to reduce the enhanced greenhouse effect.
Some measures that nations and individuals alike can take onboard to reduce the emission
of greenhouse gases and thus reduce the rate of global warming include:
Using fuel efficient cars and developing hybrid cars further
Increasing the efficiency of coal power plants or replacing with natural gas power
plants
Capturing the CO2 emitted by fossil fuel power plants (Carbon Capture)
Increasing use of renewable energy sources, including nuclear, solar, wind and
hydroelectric power
Stopping deforestation
Being conscious of energy usage
8.6.12 – Discuss international efforts to reduce the enhanced greenhouse effect.
A number of panels and self-imposed regulations have been introduced in an attempt to
decrease the emission of greenhouse gases. Some of these committees include:
Intergovernmental Panel on Climate Change (IPCC): countries and organisations that
regularly assess the current evidence from international research into global
warming and the human induced greenhouse effect.
Kyoto Protocol: In 1997, in Kyoto, Japan, an agreement towards cutting greenhouse
gases was reached, with the target of cutting greenhouse gas emissions by 5.2%
between 2008 and 2012. The protocol became legally binding when Iceland, the 55th
country to sign, joined the protocol.
Asia-Pacific Partnership on Clean Development and Climate (APPCDC): Six countries
that represent around 50% of the world’s energy use signed an agreement to work
together and with private sector partners to meet goals for energy security, national
air pollution reduction and climate change in ways that promote sustainable
economic growth and poverty reduction. These countries include Australia, China,
India, Japan, Korea and the United States.