Over 95% of total CO<SUB>2</SUB> emissions are natural. For example, the natural decay of organic material in forests and grasslands, such as dead trees, results in the release of about 220 gigatonnes of carbon dioxide every year. In
1997, Indonesian peat fires were estimated to have released between 13% and 40% of the average carbon emissions caused by the burning of fossil fuels around the world in a single year.<SUP class=reference id=cite_ref-8>
[9]</SUP><SUP class=reference id=cite_ref-9>
[10]</SUP><SUP class=reference id=cite_ref-10>
[11]</SUP> Although the initial carbon dioxide in the atmosphere of the young Earth was produced by
volcanic activity, modern volcanic activity releases only 130 to 230
megatonnes of carbon dioxide each year,<SUP class=reference id=cite_ref-11>
[12]</SUP> which is less than 1% of the amount released by human activities.<SUP class=reference id=cite_ref-12>
[13]</SUP>
<SUP></SUP>
These natural sources are nearly balanced by natural sinks, physical and biological processes which remove carbon dioxide from the atmosphere. For example, some carbon dioxide dissolves in sea water, and some is removed by plants via photosynthesis.
There is a large natural flux of CO<SUB>2</SUB> into and out of the biosphere and oceans. In the pre-industrial era these fluxes were largely in balance. Currently about 57% of human-emitted CO<SUB>2</SUB> is removed by the biosphere and oceans.<SUP class=reference id=cite_ref-13>
[14]</SUP> The ratio of the increase in atmospheric CO<SUB>2</SUB> to emitted CO<SUB>2</SUB> is known as the
airborne fraction (Keeling et al., 1995); this varies for short-term averages but is typically about 45% over longer (5 year) periods.
Burning
fossil fuels such as
coal and
petroleum is the leading cause of increased
anthropogenic CO<SUB>2</SUB>;
deforestation is the second major cause. In 2008, 8.67 gigatonnes of carbon (31.8
gigatonnes of CO<SUB>2</SUB>) were released from fossil fuels worldwide, compared to 6.14 gigatonnes in 1990.<SUP class=reference id=cite_ref-Le_Quere_14-0>
[15]</SUP> In addition, land use change contributed 1.20 gigatonnes in 2008, compared to 1.64 gigatonnes in 1990.<SUP class=reference id=cite_ref-Le_Quere_14-1>
[15]</SUP>
<SUP></SUP>
This addition, about 3% of annual natural emissions as of 1997<SUP class="plainlinks noprint asof-tag update" style="DISPLAY: none">
[update]</SUP>, is sufficient to exceed the balancing effect of sinks.<SUP class=reference id=cite_ref-15>
[16]</SUP> As a result, carbon dioxide has gradually accumulated in the atmosphere, and as of 2008<SUP class="plainlinks noprint asof-tag update" style="DISPLAY: none">
[update]</SUP>, its concentration is 38% above pre-industrial levels.<SUP class=reference id=cite_ref-carbon_budget_1-1>
[2]</SUP>
<SUP></SUP>
Various techniques have been proposed for removing excess carbon dioxide from the atmosphere in
carbon dioxide sinks.