Energy consumption and the environment


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Effects of our Activities(global Warming)

Global warming is the Process that increasedwarming. Although global warming and ozone
the average temperature of the Earth,depletion often are linked in the media, the
near-surface air and oceans. The term globalrelationship between the two is not strong.
warming is a specific example of the broaderScientists have stated with 66-90% confidence
term climate change, which can also refer tothat the effects of volcanic and human-caused
global cooling. In principle, global warmingaerosols have offset some of global warming,
is neutral as to the period or causes, but inand that greenhouse gases would have resulted
both common and scientific usage the termin more warming than observed if not for this
generally refers to recent warming andeffect. Many estimates of aggregate net
implies a human influence. The climate systemeconomic costs of damages from climate change
varies through natural, internal processesacross the globe, the social cost of carbon
and in response to variations in external(SCC), expressed in terms of future net
"forcing" factors including solar activity,benefits and costs that are discounted to the
volcanic emissions, variations in the earth'spresent, are now available. Peer-reviewed
orbit In the past 200 years human industrialestimates of the SCC for 2005 have an average
activity has injected carbon dioxide andvalue of US$43 per tonne Rising global
other greenhouse gases into the atmosphere,temperature might cause forest fires to occur
and recently global average temperatures haveon larger scale, and more regularly. This
been increasing. The predicted effects forreleases more stored carbon into the
the environment and for human life areatmosphere than the carbon cycle can
numerous and varied. The main effect is annaturally re-absorb, as well as reducing the
increasing  global  average  temperature.overall forest area on the planet, creating a
positive feedback loop Projected climate
The scientific consensus is that thesechanges due to global warming have the
greenhouse gases have been responsible forpotential to lead to future large-scale and
most of the present warming trend. Thatpossibly irreversible changes in our climate
consensus is not unanimous. The earth hasresulting in impacts at continental and
experienced natural global warming andglobal scales. With increasing average global
cooling many times in the past. The recenttemperature, the water in the oceans expands
Antarctic EPICA ice core spans 800,000 years,in volume, and additional water enters them
including eight glacial cycles withwhich had previously been locked up on land
interglacial warming periods much hotter thanin glaciers, for example, the Greenland and
current temperatures.the time of the lastthe Antarctic ice sheets. The sea level has
glacial maximum about 20,000 years ago.risen more than 120 metres since the peak of
Scientists have studied global warming withthe last ice age about 18,000 years ago. For
computer models of the climate. These modelssome time it was hoped that a positive effect
are based on physical principles of fluidof global warming would be increased
dynamics, radiative transfer, and otheragricultural yields, because of the role of
processes, with some simplifications beingcarbon dioxide in photosynthesis, especially
necessary because of limitations in computerin preventing photorespiration While local
power. Some effects on both the naturalbenefits may be felt in some regions (such as
environment and human life are, at least inSiberia), recent evidence is that global
part, already being attributed to globalyields will be negatively affected.



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