Greenhouse Effect
In the 1980s scientists
determined the average temperature of the Earth's surface was
slowly rising. This trend is referred to as global warming. There
has emerged a broad scientific consensus the cause of this rise is
a build up of gases in the atmosphere.
A greenhouse is a glass house in which plants grow which lets
light in and at the same time keeps heat from getting out. This
heat keeps the plants warm, even when it is cold outside.
It is believed the same thing is happening with the Earth's
atmosphere. It lets sunlight in and CO2 and other gases restrict
this heat from escaping into space.
Anthropogenic factors are human activities that change the
environment. Various hypotheses for human-induced climate change
have been argued for many years though, generally, the scientific
debate has evolved from scepticism to a scientific consensus that
human activity is the probable cause for the rapid changes in
world climate in the past several decades. Consequently, the
debate has largely shifted onto ways to reduce further human
impact and to find ways to adapt to change that has already
occurred.
Of most concern in these anthropogenic factors is the increase of
CO2 levels due to emissions from fossil fuel combustion, followed
by aerosols (particulate matter in the atmosphere) and cement
manufacture. Other factors, including land use, ozone depletion,
animal agriculture and deforestation, are also of concern in the
roles they play - both separately and in conjunction with other
factors - in affecting climate change.
Human activities since the industrial revolution have increased
the atmospheric concentration of various greenhouse gases, leading
to increased radiative forcing from CO2, methane, tropospheric
ozone, CFCs and nitrous oxide. The atmospheric concentrations of
CO2 and methane have increased by 36% and 148% respectively since
the beginning of the industrial revolution in the mid-1700s. These
levels are considerably higher than at any time during the last
650,000 years, the period for which reliable data has been
extracted from ice cores. Less direct geological evidence
indicates that CO2 values this high were last seen approximately
20 million years ago. Fossil fuel burning has produced
approximately three-quarters of the increase in CO2 from human
activity over the past 20 years. Most of the rest is due to
land-use change, in particular deforestation.
CO2 concentrations are expected to continue to rise due to ongoing
burning of fossil fuels and land-use change. The rate of rise will
depend on uncertain economic, sociological, technological, and
natural developments.
Beginning with the industrial revolution in the 19th Century and
accelerating since, the human consumption of fossil fuels has
elevated CO2 levels from a concentration of approximately 280
parts per million (ppm) in pre-industrial times to around 387 ppm
today. The concentrations are increasing at a rate of about 2-3
ppm/year. If current rates of emission continue, these increasing
concentrations are projected to reach a range of between 535 to
983 ppm by the end of the 21st century. Along with rising methane
levels, it is suggested that these changes may cause an increase
of 1.4–5.6°C between 1990 and 2100 Proposals by some scientists
and international coalitions, aimed at attempting to prevent
drastic climate change, have suggested setting goals to try to
limit concentrations of CO2 to a range of 450 to 500 ppm.
One alternative hypothesis, widely refuted, to the consensus view
that anthropogenic factors are causing temperature increase is
that recent warming may be the result of variations in solar
activity.
Models are used to help investigate the causes of recent climate
change by comparing the observed changes to those that the models
project from various natural and human-derived causes. Although
these models do not unambiguously attribute the warming that
occurred from approximately 1910 to 1945 to either natural
variation or human effects, they do suggest that the warming since
1975 is dominated by man-made greenhouse gas emissions.
The Northern Hemisphere has more land than the Southern
Hemisphere, so it warms faster. The Northern Hemisphere also has
extensive areas of seasonal snow and sea-ice cover subject to the
ice-albedo feedback. More greenhouse gases are emitted in the
Northern than Southern Hemisphere, but this does not contribute to
a difference in warming between the north and south because the
major greenhouse gases persist long enough to mix between the
hemispheres.
Some economists have tried to estimate the aggregate net economic
costs of damages from climate change across the globe. Such
estimates have so far yielded no conclusive findings; in a survey
of 100 estimates, the values ran from $US-3 per tonne of CO2 up to
$US95 per tonne of CO2, with a mean of $US12 per tonne of CO2.
One widely publicized report on potential economic impact is the
2006 Stern Review. The report said the costs of acting to counter
climate change, by stabilizing emissions of carbon dioxide in the
atmosphere, might be about 1 per cent of annual global gross
domestic product (GDP) by 2050. But the cost of doing nothing was
found to be far greater – risking up to 20 per cent of the world's
wealth. The report's methodology, advocacy and conclusions have
been criticized by many economists, primarily around the Review's
assumptions of discounting and its choices of scenarios. Others
have supported the general attempt to quantify economic risk, even
if not the specific numbers.
In a 2009 update Lord Stern revised his 2006 prediction, saying
the cost of inaction would be "50 per cent or more higher" than
his previous highest estimate – meaning it could cost a third of
the world's wealth.
The International Panel on Climate Change (IPCC) Working Group is
responsible for crafting reports that deal with the mitigation of
global warming and analyzing the costs and benefits of different
approaches. The 2007 IPCC Fourth Assessment Report concluded that
no one technology or sector can be completely responsible for
mitigating future warming. They find there are key practices and
technologies in various sectors, such as energy supply,
transportation, industry, and agriculture that should be
implemented to reduce global emissions. They estimate that
stabilization of CO2 equivalent between 445 and 710 ppm by 2030
will result in between a 0.6 percent increase and three percent
decrease in global GDP.
For the purpose of this invention the 1 percent global GDP
decrease suggested by the Stern Review is used for comparative
purposes.
According to the IPCC Working Group, to limit temperature rise to
2 degrees Celsius, developed countries as a group would need to
reduce their emissions to below 1990 levels in 2020 (on the order
of -10 percent to 40 percent below 1990 levels for most of the
considered regimes) and to still lower levels by 2050 (80 percent
to 95 percent below 1990 levels), even if developing countries
make substantial reductions.
Human nature what it is, changing current energy regimes and
reducing man’s detrimental impacts on the environment will be
difficult if not impossible to achieve. It is an objective of the
current invention therefore to reduce the human impact of CO2 on
climate change, whether or not energy regimes are changed or other
impacts are lessened. In one aspect of the current invention
substantial amounts of the greenhouse gas CO2 will be sequestered
in vegetation planted in irrigated deserts.
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