Protestors dressed in CO2 molecule costumes, demonstrate in Essen,  Germany, as part of the initiative 'ByeBye CO2' against carbon dioxide  pollution (Source: Reuters)
   Carbon dioxide is the number one reason for man-made  climate change. But what is carbon dioxide, actually? Where does it come  from? And why are governments and businesses now scrambling to reduce  their carbon dioxide emissions?
       
Contribution to Human-Induced Climate Change: 70 percent
 Global Warming Potency (100 years): 1 (benchmark to other gases)
Carbon dioxide is the second most important greenhouse gas behind water  vapor, but the most important contributor to anthropogenic climate change. Methane and ozone are more potent, but have less effect on  climate change due to their smaller atmospheric concentrations.
The amount of carbon dioxide (CO2) in the atmosphere has been in flux throughout the Earth’s history, but the United Nations Intergovernmental Panel on Climate Change (IPCC) estimates that in pre-industrial times CO2 made up around 280 ppmv (parts per million volume) of the Earth’s atmosphere.
Since the beginning of the  Industrial Revolution, however, the average  amount of carbon dioxide in  the atmosphere has increased by nearly 40  percent from an estimated 280  to more than 380 ppmv.
Sources of CO2
Carbon dioxide has always been with  us. Scientists say Earth’s earliest  atmosphere was made up mostly of  steam, carbon dioxide, and ammonia  from volcanic eruptions.
Today,  carbon dioxide is naturally produced by the combustion of organic matter  like coal, oil, and wood, and the fermentation or respiration processes  of living organisms.
People are another source. The air we exhale is made up of about 4.5   percent CO2. Bacteria in the soil release CO2 when they digest leaves  and  carcasses. Even plants that usually absorb CO2 'exhale' it at night.
CO2 is one of the most important substances on Earth. Besides providing  warmth to the world, it is the world’s most  important fertilizer.
Plants, phytoplankton, and algae need the  gas for their photosynthesis  to produce sugar and to grow. While doing  so they absorb and bind  carbon dioxide and produce oxygen. That is why  forests are one of the world’s most important absorbers of CO2, otherwise known as  'carbon sinks'.
There are a number of  artificial uses of carbon dioxide, in fire  extinguishers, as dry ice and, as the food additive E290, CO2 adds the  fizz to soft drinks and sparkling water.
Human-induced increase
The increase in CO2’s share of the atmosphere is mostly due to   anthropogenic (man-induced) factors, such as burning fossil fuels,  deforestation, and industrial production.
Most anthropogenic CO2 is produced by energy production and  transport.  Cement production is just one among many chemical processes  that release  the gas. Rotting organic materials release CO2, and so landfills are big CO2 contributors  too.
In total, humans emit around 32 gigatons of carbon dioxide each  year. Half of this stays in the atmosphere; the rest is absorbed by  oceans and vegetation.
       
But with sharp increases in man-made CO2 emissions, the  natural CO2  cycle has been thrown out of balance: vegetation can no  longer transform  the same proportion of CO2 into oxygen, and oceans are steadily  reaching saturation level.
 
 Theoretically, rising CO2 levels should be compensated for by plants and   algae. Up to a certain concentration, more CO2 means more   photosynthesis and more growth. 
 
 Unfortunately, under hot and dry  conditions many plants close their  pores to prevent the loss of water  and switch to a process called  photorespiration during which they  consume oxygen and produce carbon  dioxide.  Only areas with enough  precipitation and fertile soils will  see increased growth as a result of  rising CO2 levels.
 
 The result is an enhanced greenhouse effect   and, subsequently, climate change. While CO2 is only responsible for  20  percent of the natural greenhouse effect, it accounts for about 60   percent of the anthropogenic greenhouse effect that is causing the   current global warming.