Carbon respiration

Carbon respiration

Carbon respiration is a phrase used in combination with carbon storage to calculate the amount of carbon (as CO2) flux occurring in the atmosphere through the various processes that add and subtract atmospheric carbon. The result of this calculation is known as the carbon flux ratio.

Carbon is added to the atmosphere through the burning of fossil fuels, organic respiration, wood burning, and volcanic eruptions. The uptake of carbon from the atmosphere occurs through carbon dissolution into the oceans, plant respiration, and the storing of carbon in various forms such as peat bogs, oil accumulation, and formation of minerals such as coal.

The calculation of the annual net difference between carbon respiration and carbon storage constitutes the annual global atmospheric carbon accumulation rate. Using this method, the annual carbon flux ratio has been calculated to be approaching zero. This means that the carbon respiration rate and carbon storage rate are in balance when generating a global estimate of this figure. [cite web
url=http://www.eia.doe.gov/oiaf/1605/gg97rpt/chap7.html
title=Land Use Issues
publisher=
accessdate=2006-09-09 ]

Annual net carbon flux has been grossly calculated to be close to zero, implying the respiration and storage rates are roughly in balance worldwide. This finding is contradicted by measuring the concentrations of carbon dioxide in the atmosphere, an important indication that the balance is tipped toward emission. [cite web
url=http://en.wikipedia.org/wiki/


title=Graph of CO2, temperature, and dust concentration measured from the Vostok, Antarctica ice core as reported by Petit et al., 1999.
publisher=
accessdate=2006-09-09 ] Using this data atmospheric concentrations appear to have increased rapidly over the past 100 years and are currently higher than ever in human history. This suggests that more carbon is being released than can be absorbed on earth.

References


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