Carbon dioxide has been surmised as an significant component in ceasing the last Ice Age, but its precise function has always been indecipherable as rising temperatures pondered in Antarctic ice cores came up before rising levels of CO2.

But if temperatures on a global scale are reconstructed and not just analyze Antarctic temperatures it gets evident that the CO2 alteration somewhat predated much of the global warming. It means the global greenhouse effect had an significant role in driving up global temperatures.

Many researchers have analyzed that growing levels of carbon dioxide and the global warming that terminated the last Ice Age were in some manner related with each other. Nevertheless setting up a absolved cause-and-effect relationship among global warming and CO2 from the geological track record has been hard.

An issue of main interest is the potential outcome of the burning of fossil fuels and other contributors that raise the level of carbon dioxide in the atmosphere. The activity of carbon dioxide and other greenhouse gases in entrapping infrared radiation is referred as the greenhouse effect. It may increase the total average temperature of the earth to a measurable degree, which could have calamitous impacts. Sometimes the impacts of the greenhouse effect are expressed in terms of the albedo of the earth, the total average reflection coefficient.

The greenhouse effect denotes to considerations where the short wavelengths of visible light from the sun pass via transparent medium and absorbed. The longer wavelengths of the infrared radiation from the inflamed objects are not able to pass via that medium. The trapping of the long wavelength radiation contributes to more heating and a more prominent resultant temperature.

In addition to the heating of an automobile by sunlight via the windshield and the namesake illustration of heating the greenhouse by sunlight passing via sealed off, crystal clear windows, the greenhouse effect has been commonly employed to distinguish the entrapping of excess heat by the growing concentration of carbon dioxide in the atmosphere. The carbon dioxide powerfully absorbs infrared and does not permit as much of it to escape into space.

The global warming potential (GWP) is based on:

ñ  The efficiency of the molecule as a greenhouse gas.

ñ  Atmospheric lifespan of a greenhouse gas.

GWP is assessed relative to the same mass of CO2 and measured for a particular timescale. Therefore, if a gas has a high radiative forcing along with a short lifespan, it will have a prominent GWP on a 20 year scale but a smaller one on a 100 year scale. With the terms of the relation reversed, if a molecule has a more proficient atmospheric lifespan than CO2 its GWP will raise with the timescale regarded. Carbon dioxide is outlined to have a GWP of 1 over all time periods.

The Carbon Cycle

In order to interpret whether or not human being are having an impact on atmospheric carbon concentrations, carbon moves via the environment are being analyzed. Carbon is laid in in four main reservoirs.

1.    In the atmosphere in form of CO2 gas. From atmosphere it exchanges with seawater  in the atmosphere to return to the oceans. Or it will also interchanges with the biosphere by the process of the photosynthesis and extracted from the atmosphere by plants. CO2  also come back to the atmosphere by the process respiration from living organisms. Also  from weathering of rocks, from decay of dead organisms,from burning of fossil fuels by humans and from leakage of petroleum reservoirs.

2.    In the hydrosphere, CO2 is in form of dissolved CO2. It is then precipitated naturally to constitute chemical sedimentary rocks. It can also be  taken up by living organisms to enter the biosphere. CO2 come  back to the hydrosphere by disintegration of carbonate minerals in shells and rocks. Also by the process of respiration of living organisms, by input from groundwater and by reaction with the atmosphere.

3.    In the biosphere it is present as organic compounds in organisms. CO2 comes in the biosphere chiefly via photosynthesis. From organisms it can come back to the atmosphere by decay when organisms die, it can become buried in the earth or by the process of respiration.

Global warming primarily impacts the atmosphere. In whatever way, if the climate alteration that takes place refers that there is increments in the  rainfall, then possibly erosion rates will be raised. It is highly unbelievable that it has any impact the underlying forces of plate tectonics or on plate motions. It is the contrary, instead of tectonics like mountain building can impact the atmosphere and the climate. In peculiar if the landmasses move so that the currents in the oceans are disrupted, this will have a fundamental impact on the climate.

Global warming is induced by the emission of greenhouse gases. 72% of the entirely emitted greenhouse gases is carbon dioxide (CO2), 9% Nitrous oxide (Nox) and  18% Methane. Carbon dioxide emissions consequently are the most significant reason of the global warming. CO2 is  commonly produced by burning fuels like for illustration,  natural gas, ethanol, oil, organic-diesel, diesel, organic-petrol and petrol. The expelling of CO2 have been increased  in a dramatic manner among the last 50 years and are still raising by almost 3% each year.

Recent probes have demonstrated that unimaginable ruinous alterations in the environment will take place if the global temperatures raise by more than 2° C.  A warming of 2° C represents a carbon dioxide (CO2) concentration of about 450 ppm in the atmosphere. As of beginning of the year 2007, the CO2 concentration was registered at 380 ppm and it arouses on average 2 - 3 ppm each year.

The carbon dioxide is discharged to the atmosphere where it remains for 100 to 200 years. This contributes to an increasing concentration of carbon dioxide in our atmosphere. This in turn causes the average temperature on earth to increase up to certain level. On the earth's lithosphere as graphite, carbonate minerals, petroleum and coal are commonly found. It can bring back to the atmosphere by volcanic eruptions, weathering, by human extraction, burning to produce energy and  hot springs.

 
Cycling among the atmosphere and the biosphere take place within 4.5 years. Cycling among the other reservoirs likely to take place on an average of millions of years.

For illustration, carbon laid in in the earth in sedimentary rocks or as fossil fuels  comes in the atmosphere by nature when erosion and weathering disclose these materials to the surface of the earth. When humans burn and extract fossil fuels the process take place much more quickly than it would take place by natural procedures. With an enhanced rate of cycling among the atmosphere and the earth, extraction from the atmosphere by enhanced interaction with the oceans or by increased extraction by organisms must take place to balance the input. If this does not take place, it may lead to the global warming.

Average global temperatures changes with time as an outcome of many procedures interacting with each other. These fundamental interaction and the leading variation in temperature can take place on a variety of time scales arraying from yearly cycles to cycles with times assessed in millions of years. Such variation in global temperatures is hard to interpret due to the complication of the interactions and as exact records of global temperature do not go back more than 100 years. Except for, even analyzing at the track record for the past 100 years, one can see that overall, there is an raise in average global temperatures, with minor postpones that may have been ascertained by random events such as volcanic eruptions. Records for the past 100 years show that average global temperatures have been raised by about 0.5oC. While this may not look like much, the deviation in global temperature among the coldest period of the last geologic process and the present was only about 5oC