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Global
Warming
Global Warming
is the gradual increase in the average mean global temperature of
the earth. Scientists have attributed this warming of the planet
to both natural and human induced activities. Global temperature
is determined by the balance between the inflow of solar radiation
into the atmosphere, the trapping of some of this heat due to what
is referred to as the "greenhouse effect" and the reradiation
of heat back into space. To maintain its long term thermal balance/equilibrium,
the Earth must reradiate back to space on average, the same amount
of energy that is absorbed. Anything that interferes with this energy
balance will cause a shift in global temperatures. When on average,
there is less energy being reradiated than absorbed, the earth will
experience a rise in global temperature referee to as global warming.
This gradual warming is occurring and has been for decades and is
used to explain much of the change scientists are seeing in climate
today.
The United
Nations Framework Convention on Climate Change has developed a
Climate Change information Kit. This kit contains detailed
information on climate change science approaching and explaining the
science in a simple easy to understand manner. Whether you are an
expert or a novice in the field of climate change, this information
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Greenhouse
Gas Science:
The
earths climate is affected by the factors that cause a change
in the redistribution of energy (solar radiation) within the atmosphere
or between the atmosphere, Land and ocean. One factor (element) which determines and affects this global
energy balance is the Greenhouse Effect.
Gases such as carbon dioxide (CO2), nitrous oxide
(N2O), carbon monoxide (CO), methane (CH4),
halocarbons (HFCs) and sulphur hexaflouride (SF6) contribute
to the natural greenhouse effect, which is responsible for the overall
inflow and outflow of solar radiation.
They achieve this by trapping the solar radiation entering
the earths atmosphere and redistributing this energy over
time and space. The
amount of radiation that remains in the atmosphere is determined
by the concentration of greenhouse gases in it. Since the dawn of the industrial revolution
there has been an increase in the use of energy. The burning of fossil fuels has contributed significantly to
the observed increases in greenhouse gas concentration resulting
in the increased trapping of solar radiation and the enhanced greenhouse
effect.
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