1. Recent Carbon Trends and the Global Carbon Budget updated to 2006 GCP-Global Carbon Budget team: Pep Canadell, Philippe Ciais, Thomas Conway, Chris Field, Corinne Le Quéré, Skee Houghton, Gregg Marland, Mike Raupach, Erik Buitenhuis, Nathan Gillett Last update: 13 June 2008

2. Outline 1.Recent global carbon trends (2000-2006) 2.The perturbation of the global carbon budget (1850-2006) 3.The declining efficiency of natural CO 2 sinks 4.Attribution of the recent acceleration of atmospheric CO 2 5.Conclusions and implications for climate change

3. 1. Recent global carbon trends

4. FAO-Global Resources Assessment 2005; Canadell et al. 2007, PNAS Tropical Americas 0.6 Pg C y -1 Tropical Asia 0.6 Pg C y -1 Tropical Africa 0.3 Pg C y -1 2000-2005 Tropical deforestation 13 Million hectares each year Anthropogenic C Emissions: Land Use Change 1.5 Pg C y -1 Borneo, Courtesy: Viktor Boehm

5. Houghton, unpublished Carbon Emissions from Tropical Deforestation Pg C yr -1 0.00 0.20 0.40 0.60 0.80 1.00 1.20 1.40 1.60 1.80 1850186018701880189019001910192019301940195019601970 1980 19902000 Africa Latin America S. & SE Asia Anthropogenic C Emissions: Land Use Change SUM 2000-2006 1.5 Pg C y -1 (16% total emissions)

6. Anthropogenic C Emissions: Fossil Fuel Raupach et al. 2007, PNAS; Canadell et al 2007, PNAS 1990 - 1999: 1.3% y -1 2000 - 2006: 3.3% y -1 185018701890191019301950197019902010 2006 Fossil Fuel: 8.4 Pg C [2006-Total Anthrop. Emissions:8.4+1.5 = 9.9 Pg]

7. Trajectory of Global Fossil Fuel Emissions Raupach et al. 2007, PNAS SRES (2000) growth rates in % y -1 for 2000-2010: A1B: 2.42 A1FI: 2.71 A1T: 1.63 A2: 2.13 B1: 1.79 B2: 1.61

8. Trajectory of Global Fossil Fuel Emissions Raupach et al. 2007, PNAS SRES (2000) growth rates in % y -1 for 2000-2010: A1B: 2.42 A1FI: 2.71 A1T: 1.63 A2: 2.13 B1: 1.79 B2: 1.61 Observed 2000-2006 3.3%

9. Carbon Intensity of the Global Economy Canadell et al. 2007, PNAS Carbon intensity (KgC/US$) Kg Carbon Emitted to Produce 1 $ of Wealth 1960 1970 1980 1990 2000 2006 Photo: CSIRO

10. Raupach et al 2007, PNAS 0.5 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4 1.5 1980 0.5 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4 1.5 1980 World 0.5 0.6 0.7 0.8 0.9 1 1.1 1.2 1.3 1.4 1.5 198019851990199520002005 F (emissions) P (population) g = G/P h = F/G Factor (relative to 1990) Emissions Population Wealth = per capita GDP Carbon intensity of GDP Drivers of Anthropogenic Emissions

11. Regional Pathways (Kaya identity) C emissions Population C Intensity Developed Countries (-) Developing CountriesLeast Developed Countries Wealth pc Raupach et al 2007, PNAS

12. Raupach et al. 2007, PNAS Cumulative Emissions [1751-2004] Flux in 2004 Flux Growth in 2004 Population in 2004 0% 20% 40% 60% 80% 100% D3-Least Developed Countries India D2-Developing Countries China FSU D1-Developed Countries Japan EU USA Anthropogenic C Emissions: Regional Contributions

13. 2000 - 2006: 1.9 ppm y -1 1970 – 1979: 1.3 ppm y -1 1980 – 1989: 1.6 ppm y 1 1990 – 1999: 1.5 ppm y -1 Year 2007 Atmospheric CO 2 concentration: 382.6 ppm 35% above pre-industrial NOAA 2007; Canadell et al. 2007, PNAS Atmospheric CO 2 Concentration 185018701890191019301950197019902010 [CO 2 ]

14. 2. The perturbation of the global carbon cycle (1850-2006)

15. deforestation tropics extra-tropics 1.5 2000-2006 CO 2 flux (Pg C y -1 ) Sink Source Time (y) Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

16. deforestation fossil fuel emissions 7.6 1.5 2000-2006 CO 2 flux (Pg C y -1 ) Sink Source Time (y) Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

17. fossil fuel emissions deforestation 7.6 1.5 2000-2006 CO 2 flux (Pg C y -1 ) Sink Source Time (y) Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

18. fossil fuel emissions deforestation 7.6 1.5 4.1 2000-2006 CO 2 flux (Pg C y -1 ) Sink Source Time (y) atmospheric CO 2 Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

19. atmospheric CO 2 fossil fuel emissions deforestation ocean 7.6 1.5 4.1 2.2 CO 2 flux (Pg C y -1 ) Sink Source Time (y) 2000-2006 Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

20. atmospheric CO 2 ocean land fossil fuel emissions deforestation 7.6 1.5 4.1 2.2 2.8 2000-2006 CO 2 flux (Pg C y -1 ) Sink Source Time (y) Perturbation of Global Carbon Budget (1850-2006) Le Quéré, unpublished; Canadell et al. 2007, PNAS

21. Canadell et al. 2007, PNAS Perturbation of the Global Carbon Budget (1959-2006) CO 2 flux (Pg CO 2 y -1 ) Carbon flux (Pg C y -1 ) Carbon intensity (KgC/US$) Sink Source Time (y)

22. 3. The declining efficiency of natural sinks

23. Fate of Anthropogenic CO 2 Emissions (2000-2006) Canadell et al. 2007, PNAS 1.5 Pg C y -1 + 7.6 Pg C y -1 Atmosphere 45% 4.1 Pg y -1 Land 30% 2.8 Pg y -1 Oceans 25% 2.2 Pg y -1

24. Climate Change at 55% Discount Natural sinks absorb 5 billions tons of CO 2 globally every year, or 55% of all anthropogenic carbon emissions. Canadell et al. 2007, PNAS

25. Natural Sinks: Large Economic Subsidy Natural sinks are a huge subsidy to our global economy worth half a trillion Euros annually if an equivalent sink had to be created using other climate mitigation options (based on the cost of carbon in the EU-ETS). Canadell & Raupach 2008, Science

26. 1.The rate of CO 2 emissions. 2.The rate of CO 2 uptake and ultimately the total amount of C that can be stored by land and oceans: –Land: CO 2 fertilization effect, soil respiration, N deposition fertilization, forest regrowth, woody encroachment, … –Oceans: CO 2 solubility (temperature, salinity),, ocean currents, stratification, winds, biological activity, acidification, … Factors that Influence the Airborne Fraction Canadell et al. 2007, Springer; Gruber et al. 2004, Island Press

27. % CO 2 Emissions in Atmosphere 1960 2000 19801970 1990 Canadell et al. 2007, PNAS 2006 Decline in the Efficiency of CO 2 Natural Sinks Fraction of anthropogenic emissions that stay in the atmosphere Emissions 1 tCO 2 400Kg stay Emissions 1 tCO 2 450Kg stay

28. Efficiency of Natural Sinks Land Fraction Ocean Fraction Canadell et al. 2007, PNAS

29. Part of the decline is attributed to up to a 30% decrease in the efficiency of the Southern Ocean sink over the last 20 years. This sink removes annually 0.7 Pg of anthropogenic carbon. The decline is attributed to the strengthening of the winds around Antarctica which enhances ventilation of natural carbon-rich deep waters. The strengthening of the winds is attributed to global warming and the ozone hole. Causes of the Declined in the Efficiency of the Ocean Sink Le Quéré et al. 2007, Science Credit: N.Metzl, August 2000, oceanographic cruise OISO-5

30. Angert et al. 2005, PNAS; Buermann et al. 2007, PNAS; Ciais et al. 2005, Science Drought Effects on the Mid-Latitude Carbon Sinks Summer 1982-1991 Summer 1994-2002/04 NDVI Anomaly 1982-2004 [Normalized Difference Vegetation Index] A number of major droughts in mid-latitudes have contributed to the weakening of the growth rate of terrestrial carbon sinks in these regions.

31. 4. Attribution of the recent acceleration of atmospheric CO 2

32. 65% - Increased activity of the global economy Canadell et al. 2007, PNAS 17% - Deterioration of the carbon intensity of the global economy 18% - Decreased efficiency of natural sinks 2000 - 2006: 1.9 ppm y -1 1970 – 1979: 1.3 ppm y -1 1980 – 1989: 1.6 ppm y 1 1990 – 1999: 1.5 ppm y -1 Attribution of Recent Acceleration of Atmospheric CO 2 To: Economic growth Carbon intensity Efficiency of natural sinks

33. 5. Conclusions and implications for climate change

34. The growth of carbon emissions from fossil fuels has tripled compared to the 1990s and is exceeding the predictions of the highest IPCC emission scenarios. Conclusions (i) Atmospheric CO 2 has grown at 1.9 ppm per year (compared to about 1.5 ppm during the previous 30 years) The carbon intensity of the world’s economy has stopped decreasing (after 100 years of doing so). Since 2000:

35. Conclusions (ii) The efficiency of natural sinks has decreased by 10% over the last 50 years (and will continue to do so in the future), implying that the longer we wait to reduce emissions, the larger the cuts needed to stabilize atmospheric CO 2. All of these changes characterize a carbon cycle that is generating stronger climate forcing and sooner than expected.

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