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Carbon Budget 2007 GCP-Global Carbon Budget team: Pep Canadell, Philippe Ciais, Thomas Conway, Christopher B. Field, Corinne Le Quéré, Richard A. Houghton, Gregg Marland, Michael R. Raupach Last update: 1 July 2009 Outline 1. Atmospheric CO2 Concentration 2. CO2 Emissions from Fossil Fuel and Cement 3. Drivers of Fossil Fuel Emissions 4. CO2 Emissions from Land Use Change 5. Natural CO2 Sinks 6. Summary of the Global Carbon Budget 1. Atmospheric CO2 Concentration Atmospheric CO2 Concentration Year 2007 Atmospheric CO2 concentration: 383 ppm 37% above pre-industrial 1970 – 1979: 1.3 ppm y-1 1980 – 1989: 1.6 ppm y1 1990 – 1999: 1.5 ppm y-1 2000 - 2007: 2.0 ppm y-1 2007: 2.2 ppm y-1 Data Source: Pieter Tans and Thomas Conway, NOAA/ESRL 2. Emissions from Fossil Fuel and Cement Emissions from Fossil Fuel + Cement Atmoapheric [CO2] (ppmv) Fossil Fuel Emission (GtC/y) 2007 Fossil Fuel: 8.5 Pg C 9 8 Emissions 7 6 5 4 3 2 1 0 1850 4001850 380 360 340 320 300 Data Source: G. Marland, T.A. Boden, R.J. Andres, and J. Gregg at CDIAC 280 1870 1870 1890 1890 1910 1910 1930 1930 1950 1950 1970 1970 1990 1990 2010 2010 [CO2] 1990 - 1999: 0.9% y-1 2000 - 2007: 3.5% y-1 2 ppm/year Fossil Fuel Emissions: Actual vs. IPCC Scenarios 0 1850 1900 1950 2000 2050 2100 10 Fossil Fuel Emission (GtC/y) 9.5 9 8.5 8 7.5 CDIAC IEAall A1B(Av) A1FI(Av) A1T(Av) A2(Av) B1(Av) B2(Av) 7 6.5 6 5.5 5 1990 1995 2000 Raupach et al 2007, PNAS (updated) 2005 2010 Percentage of Global Annual Emissions Regional Shift in Emissions Share 62% 57% 49.7% 43% 38% FCCC Kyoto Protocol Adopted Kyoto Reference Year J. Gregg and G. Marland, 2008, personal communication 50.3% 53% 47% Kyoto Protocol Enter into Force Current Regional Share of Fossil Fuel Emissions 100% D3-Least Developed Countries 80% D2-Developing Countries 60% India 40% China FSU 20% 0% Cumulative Flux Emissions in 2004 [1751-2004] Raupach et al. 2007, PNAS Flux Growth in 2004 Japan EU Population USA in 2004 D1-Developed Countries 3. Drivers of fossil fuel emissions Human and Biophysical Drivers of Accelerating AtmCO2 Kaya Identity C Emissions = Population x Per Capita GDP x C intensity of GDP Per Capital GDP C intensity of GDP Population C Emissions Raupach, Canadell, Le Quere, 2008, Biogeoscience Regional Emission Pathways C emissions Wealth per capita Population C Intensity Developed Countries (-) Developing Countries Raupach et al 2007, PNAS Least Developed Countries 4. Emissions from Land Use Change Carbon Emissions from Land Use Change Borneo, Courtesy: Viktor Boehm Tropical deforestation 13 Million hectares each year 2000-2007 Tropical Americas 0.6 Pg C y-1 Tropical Asia 0.6 Pg C y-1 Tropical Africa 0.3 Pg C y-1 1.5 Pg C y-1 [2007-Total Anthropogenic Emissions:8.5+1.5 = 10 Pg] Canadell et al. 2007, PNAS; FAO-Global Resources Assessment 2005 Historical Emissions from Land Use Change Carbon Emissions from Tropical Deforestation 2000-2007 1.5 Pg C y-1 1.60 Africa 1.40 Latin America 1.20 S. & SE Asia 1.00 SUM (16% total emissions) 0.80 0.60 0.40 0.20 R.A. Houghton, unpublished 2000 1990 1980 1970 1960 1950 1940 1930 1920 1910 1900 1890 1880 1870 1860 0.00 1850 Pg C yr-1 1.80 Regional Share of Emissions from Land Use Change Canadell, Raupach, Houghton, 2008, Biogeosciences, submitted 5. Natural CO2 sinks Fate of Anthropogenic CO2 Emissions (2000-2007) 1.5 Pg C y-1 4.2 Pg y-1 Atmosphere 46% 2.6 Pg y-1 Land 29% + 7.5 Pg C y-1 2.3 Pg y-1 Oceans 26% Canadell et al. 2007, PNAS (updated) Climate Change at 55% Discount Natural CO2 sinks absorb 55% of all anthropogenic carbon emissions slowing down climate change significantly. They are in effect a huge subsidy to the global economy worth half a trillion US$ annually if an equivalent sink had to be created using other climate mitigation options (based on the cost of carbon in the EU-ETS). Factors that Influence the Airborne Fraction 1. The rate of CO2 emissions. 2. The rate of CO2 uptake and ultimately the total amount of C that can be stored by land and oceans: – – Land: CO2 fertilization effect, soil respiration, N deposition fertilization, forest regrowth, woody encroachment, … Oceans: CO2 solubility (temperature, salinity),, ocean currents, stratification, winds, biological activity, acidification, … Springer; Gruber et al. 2004, Island Press Decline in the Efficiency of CO2 Natural Sinks % CO2 Emissions in Atmosphere Fraction of all anthropogenic emissions that stay in the atmosphere Emissions 1 tCO2 400Kg stay Emissions 1 tCO2 1960 1970 1980 Canadell et al. 2007, PNAS 1990 2000 2006 450Kg stay Efficiency of Natural Sinks Land Fraction Ocean Fraction Canadell et al. 2007, PNAS Causes of the Declined in the Efficiency of the Ocean Sink • 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. Credit: N.Metzl, August 2000, oceanographic cruise OISO-5 • 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. Le Quéré et al. 2007, Science 6. Summary of the global carbon budget Human Perturbation of the Global Carbon Budget Source deforestation tropics extra-tropics 1.5 Sink CO2 flux (Pg C y-1) 2000-2007 Time (y) Global Carbon Project (2008) Human Perturbation of the Global Carbon Budget Source 7.5 deforestation Sink CO2 flux (Pg C y-1) fossil fuel emissions 2000-2007 Time (y) Global Carbon Project (2008) 1.5 Human Perturbation of the Global Carbon Budget Source 7.5 deforestation Sink CO2 flux (Pg C y-1) fossil fuel emissions 2000-2007 Time (y) Global Carbon Project (2008) 1.5 Human Perturbation of the Global Carbon Budget Source 7.5 deforestation atmospheric CO2 Sink CO2 flux (Pg C y-1) fossil fuel emissions 2000-2007 Time (y) Global Carbon Project (2008) 1.5 4.2 Human Perturbation of the Global Carbon Budget Source 7.5 deforestation atmospheric CO2 Sink CO2 flux (Pg C y-1) fossil fuel emissions 2000-2007 ocean Time (y) Global Carbon Project (2008) 1.5 4.2 2.3 Human Perturbation of the Global Carbon Budget 2000-2007 Source 7.5 deforestation atmospheric CO2 Sink CO2 flux (Pg C y-1) fossil fuel emissions land ocean Time (y) Global Carbon Project (2008) 1.5 4.2 2.6 2.3 Human Perturbation of the Global Carbon Budget Canadell et al. 2007, PNAS (updated to 2007) Drivers of Accelerating Atmospheric CO2 1970 – 1979: 1.3 ppm y-1 1980 – 1989: 1.6 ppm y1 1990 – 1999: 1.5 ppm y-1 2000 - 2007: 2.0 ppm y-1 To: • Economic growth • Carbon intensity • Efficiency of natural sinks 65% - Increased activity of the global economy 17% - Deterioration of the carbon intensity of the global economy 18% - Decreased efficiency of natural sinks (calculations based on the period 2000-2006) Canadell et al. 2007, PNAS Conclusions (i) • Anthropogenic CO2 emissions are growing x4 faster since 2000 than during the previous decade, and above the worst case emission scenario of the Intergovernmental Panel on Climate Change (IPCC). • Less Developed Countries are now emitting more carbon than Developed Countries. • The carbon intensity of the world’s economy is improving slower than previous decades. Conclusions (ii) • The efficiency of natural sinks has decreased by 5% over the last 50 years (and will continue to do so in the future), implying that the longer it takes to begin reducing emissions significantly, the larger the cuts needed to stabilize atmospheric CO2. • All these changes have led to an acceleration of atmospheric CO2 growth 33% faster since 2000 than in the previous two decades, implying a stronger climate forcing and sooner than expected. www.globalcarbonproject.org [email protected]