Between 2000 to 2006, human activities such as burning fossil fuels, manufacturing cement, and tropical deforestation contributed an average of 4.1 billion metric tons of carbon to the atmosphere each year, yielding an annual growth rate for atmospheric carbon dioxide of 1.93 parts per million (ppm). "This is the highest since the beginning of continuous monitoring in 1959," states the report. The growth rate of atmospheric carbon dioxide is significantly larger than those for the 1980s and 1990s, which were 1.58 and 1.49 ppm per year, respectively. The present atmospheric concentration of carbon dioxide is 381 ppm, the largest concentration in the last 650,000 years, and probably in the last 20 million years.

While the worldwide acceleration in carbon dioxide emissions had been previously noted, the current analysis provides insights into its causes. "The new twist here is the demonstration that weakening land and ocean sinks are contributing to the accelerating growth of atmospheric CO2," says co-author Chris Field, director of the Carnegie Institution's Department of Global Ecology.

Changes in wind patterns over the Southern Ocean resulting from human-induced global warming have brought carbon-rich water toward the surface, reducing the ocean's ability to absorb excess carbon dioxide from the atmosphere. On land, where plant growth is the major mechanism for drawing carbon dioxide out of the atmosphere, large droughts have reduced the uptake of carbon.

Emissions from the burning of fossil fuels constituted the largest source of anthropogenic carbon, releasing an average of 7.6 billion metric tons each year between 2000 and 2006, a significant jump from 6.5 billion tons in the 1990s. Emissions generated by land-use changes such as deforestation have remained constant, but shifted in geographic focus.

The study also shows that the carbon intensity of the global economy (kilograms of carbon per dollar of economic activity) has increased since 2000 at about 0.3% per year, reversing a 30-year decline of about 1.3% per year. Because practically all proposed scenarios for managing future emissions postulate improvements in carbon intensity in the global economy, this deterioration of carbon intensity presents a serious challenge in stabilizing atmospheric carbon dioxide and mitigating climate change.

The researchers for the study are Josep G. Canadell, CSIRO Marine and Atmospheric Research, Canberra, Australia; Corinne Le Quere, University of East Anglia, School of Environment Sciences, Norwich, UK, and British Antarctic Survey, Cambridge, UK; Michael R. Raupach, CSIRO Marine and Atmospheric Research, Canberra, Australia; Christopher B. Field, Carnegie Institution of Washington, Department of Global Ecology, Stanford, CA; Erik T. Buitehuis, University of East Anglia, School of Environment Sciences, Norwich, UK; Philippe Ciais, Commissariat a L'Energie Atomique, Laboratorie des Sciences du Climat et de l'Environnement, France; Thomas J. Conway, NOAA Earth System Research Laboratory, Boulder, CO; Nathan P. Gillett, University of East Anglia, School of Environment Sciences, Norwich,UK; R. A. Houghton, Woods Hole Research Center, Falmouth, MA; Gregg Marland, Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, Oak Ridge, TN, and International Institute for Applied Systems Analysis, Laxenburg, Austria

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