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The world's climate is judged by many factors.
Perhaps the main indicator is the Global Temperature Record which
has been recorded for about 140 years. Other phenomena include precipitation,
the melting of ice in the polar regions and from mountains, and the severity
of extreme weather conditions such as droughts and floods across the world
as a whole. There are many more indicators which are used to assess the
climate as it has changed in the past and to try to predict future trends.
Two references, recommended for more details are The
University of East Anglia Climatic Research Unit and The Environmental
Protection Agency (EPA).
Natural forces which we know influence the climate are:
- The Sun's output varies. The Sun is obviously the source
of most of the energy we perceive and it has been argued that
the well known sunspot cycle (approximately 11 years) produces
variations in the earth's climate. Another theory concerns the
Milankovitch cycle which is linked to the earth's orbit around
the sun and has a period measured in tens of thousands of years.
There are differences of scientific opinion but it seems that
neither of these effects can directly explain the known changes
which have taken place. Rather, it may be that the fluctuations
affect the earth's atmosphere which in its turn magnifies the
importance of the changes. In particular a favoured theory is
that the amount of CO2 in the atmosphere is a major feature which,
inter alia, changes temperatures at the surface.
- The chemical composition of the atmosphere
is such that the phenomenon we call the "Greenhouse Effect"
takes place, and it is generally accepted that CO2 is a major constituent
in this process (although many other chemicals are involved). The
mechanism traps a proportion of the heat and the temperature rises
until the escaping energy equals the incoming energy. The result
is that the earth is warmer than it would be without the effect.
Now as we say in the details on global warming elsewhere, this phenomenon
is not intrinsically bad, on the contrary life as we know it would
not exist without it. However the balance which has been reached
over countless ages is critical and must not be significantly upset
if the beneficial conditions are to be sustained. As CO2 is produced
naturally, an equal amount is absorbed; its part of nature's life
cycle. Nowadays, over and above this, man is releasing more CO2
and all the evidence indicates that as a consequence the results
of increasing temperatures globally are measurable. As the EPA
states [see link] humanity are adding about 3% or 4% to the naturally
generated CO2 and this is enough to knock the system out of balance.
- Volcanic eruptions have an immediate impact on the temperatures
at the earth's surface. The fine particles which remain suspended
in the atmosphere after an eruption circulate the globe and have
the opposite effect to CO2, producing significant cooling. Such
consequences are very rapid but are short lived and not considered
to be responsible for long term changes in the climate. Nevertheless,
even in the short term, the impact can be devastating for a few
years after a major eruption and we have current experience of
minor instances, and records obtained from tree rings indicate
the possibility that much more serious catastrophes have occurred.
It can only be surmise on our part but it seems probable that
if a sizeable asteroid struck the earth's surface the resulting
pollution would trigger identical mechanisms with a severity that
could be much worse (maybe we've seen too many Sci-Fi films).
- El Niño and La Niña
are well documented phenomena which occur in the Pacific ocean.
The warming and cooling effects are influential at great distances
away causing changes in the world's wind patterns and resulting
in uncharacteristic droughts or heavy rains. These consequences
are serious on a relatively local scale but are short lived (about
a year) and are approximately periodic every few years and so are
not major features in determining the major climatic conditions
globally over the long term.
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