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Bridging Carbon Cycling and Air Quality Studies using 14 CO 2 John B. Miller, Scott Lehman, Steve Montzka, Colm Sweeney, Pieter Tans, Jocelyn Turnbull Fossil Fuel and 14 C IPCC 95 th %ile! USA Global QuickTime and a decompressor are


  1. Bridging Carbon Cycling and Air Quality Studies using 14 CO 2 John B. Miller, Scott Lehman, Steve Montzka, Colm Sweeney, Pieter Tans, Jocelyn Turnbull

  2. Fossil Fuel and Δ 14 C IPCC 95 th %ile! USA Global QuickTime™ and a decompressor are needed to see this picture. + CarbonTracker • 14 C is, by definition, absent from fossil fuels, and thus an excellent tracer for Fossil Fuel emissions.

  3. Isotopic Notation ⎡ ⎤ 14 C = ( 14 C / C ) sam Δ − 1 ⎥ × 1000 ⎢ ⎣ ⎦ ( 14 C / C ) std Δ ff = -1000 per mil; Δ atm ~ +55 per mil

  4. Simulated Fossil Fuel CO 2 and Δ 14 C

  5. Airborne sampling QuickTime™ and a decompressor QuickTime™ and a are needed to see this picture. decompressor are needed to see this picture.

  6. CO 2 v. Anthropogenic Tracers Hypotheses H1: Lack of summer correlation due to CO 2 NEE. Using 14 CO 2 instead of CO 2 will improve correlation. H2: NEE also non-zero in winter. Using 14 CO 2 will change the slope.

  7. East Coast CO 2 and Δ 14 C (NHA + CMA) 2004 2008 C obs = C bg + C fos + C bio ( Δ C) obs = ( Δ C) bg + ( Δ C) fos QuickTime™ and a decompressor are needed to see this picture.

  8. PBL and Free Troposphere CO C obs = C bg + C net_source C ff v. C net_source

  9. m=19 ppb/ppm m=12 ppb/ppm m=7.2 ppt/ppm m=3.0 ppt/ppm m=1.2 ppt/ppm m=1.2 ppt/ppm m=4.0 ppb/ppm m=2.3 ppb/ppm Red=Summer; Blue=Winter

  10. m=6.2 ppb/ppm m=1.6 ppt/ppm m=0.7 ppt/ppm m=1.2 ppb/ppm H1 and H2 confirmed! Red=Summer; Blue=Winter

  11. m=19 ppb/ppm m=12 ppb/ppm m=7.2 ppt/ppm m=3.0 ppt/ppm m=1.2 ppt/ppm m=1.2 ppt/ppm m=4.0 ppb/ppm m=2.3 ppb/ppm m gas x E ff = E gas Red=Summer; Blue=Winter

  12. USA Emission Estimates 400 350 14CO2 EPA Gg; Tg CO; 0 .1 Gg SF6 300 250 200 150 100 50 0 CO SF6 HFC134a HCFC22 HCFC142b PCE CH2Cl2 C6H6 51 59 38 49 % of Global

  13. Caveats • Relatively few 14 C data • Some old emission inventories • Seasonal covariance between FF and tracer emissions ⇒ ~5% high bias • Limited domain with high S:N – Evidence for spatial emission ratio variability.

  14. NHA+CMA ‘Footprint’ PBL Residence Time QuickTime™ and a decompressor are needed to see this picture.

  15. Future Calculations Inventory QuickTime™ and a decompressor are needed to see this picture. Bottom-up Estimate ? Footprint QuickTime™ and a decompressor are needed to see this picture. Top-down Estimate Fossil Fuel Emissions

  16. Conclusions • 14 CO 2 allows the partitioning of CO 2 into fossil fuel and biological components. • 14 CO 2 offers great promise as a tool to calculate regional and seasonal emissions of anthropogenic gases. • At low ranges, correlating with total CO 2 appears to result in a low bias. • Many species appear to exhibit significant seasonal emission cycles.

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