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Oral Presentation ID: 493 Topics: Keywords: Theme 1.1: The Contemporary Carbon Cycle - Trends, Variability and Time of Emergence of Human Impacts carbon cycle, carbon sources and sinks State, Trends and Uncertainties of the Contemporary Global Carbon Budget Josep G Canadell1, Corinne Le Quere2, Philippe Ciais3, Glen Peters4, Rob Jackson5, Vanessa Haverd6, Anders Ahlstrom7 1 Global Carbon Project/CSIRO, Australia; 2University of East Anglia and Tyndall Centre, UK; 3LSCE, Paris; 4CICERO, Norway; 5Stanord University, USA; 6CSIRO, Australia; 7Lund University, Sweden Long-term redistribution of carbon among fossil fuel reserves, the atmosphere, oceans and land largely determines the degree of human-driven climate change and future carbon-climate feedbacks. Here we provide an update on the state and trends of the carbon budged as assessed by a large research community effort driven by the Global Carbon Project*. Key trends are 1) the apparent stabilization in the growth of fossil fuel emissions and the likely emissions decline from land use change; 2) the continued growth in atmospheric CO2; and 3) the growth in the land and ocean sinks in response to the growth in excess atmospheric CO 2 with large annual and decadal variability. Efforts to attribute driving processes to the growing sinks require a strong CO 2 fertilization effect on vegetation growth and emerging trends show an under realized role of semiarid regions in contributing to the mean, trend and variability of the global land sink. Climate variability, including ENSO and the 2000’s slowdown in terrestrial global warming, has produced opportunities to explore the drivers of global carbon fluxes as they take large departures from mean states (e.g., high rates of atmospheric CO2 accumulation along with no growth in fossil fuel emissions and strong land greening trends in recent years). Process attribution shows the strong interplay between gross primary productivity and heterotrophic respiration in response to warming, and the role of tropical and sub-tropical systems to the overall sink. Key uncertainties remain on 1) the role of anthropogenic lateral flows of carbon and their ultimate fate in inland waters and costal zones; 2) the emissions from land use change and forestry, particularly the effects of forest degradation (e.g., harvest, fires, erosion) and regrowth on land carbon stocks; and 3) the drivers of multi-year to decadal variability that limits our capacity to identify large carbon-cycle feedbacks and independently verify reported emissions in the short term. New advances in observations and data handling are critical in reducing uncertainties including 1) Bayesian fusion approaches to optimally combine multiple data streams of ocean and land uptake, and fossil fuel and land use change emissions; 2) continuous landscape carbon density measurements and column CO2 from remotely sensed platforms; and 3) improved ocean circulation and CO2 uptake at the decadal scales; among others. *Le Quéré, C. et al. Global Carbon Budget 2016, Earth Syst. Sci. Data, 8, 605-649, 2016; Li W et al. Reducing uncertainties in decadal variability of the global carbon budget with multiple datasets, PNAS, 2016