A coupled model of the global cycles of carbonyl sulfide and CO<sub>2</sub>: A possible new window on the carbon cycle

  • Joe Berry
    Department of Global Ecology Carnegie Institution Stanford California USA
  • Adam Wolf
    Department of Ecology and Evolutionary Biology Princeton University Princeton New Jersey USA
  • J. Elliott Campbell
    Sierra Nevada Research Institute University of California, Merced Merced California USA
  • Ian Baker
    Department of Atmospheric Science Colorado State University Fort Collins Colorado USA
  • Nicola Blake
    Department of Chemistry University of California, Irvine Irvine California USA
  • Don Blake
    Department of Chemistry University of California, Irvine Irvine California USA
  • A. Scott Denning
    Department of Atmospheric Science Colorado State University Fort Collins Colorado USA
  • S. Randy Kawa
    NASA Goddard Space Flight Center Greenbelt Maryland USA
  • Stephen A. Montzka
    NOAA Earth System Research Laboratory Boulder Colorado USA
  • Ulrike Seibt
    Department of Atmospheric and Oceanic Sciences University of California, Los Angeles Los Angeles California USA
  • Keren Stimler
    Environmental Sciences and Energy Research Weizmann Institute of Science Rehovot Israel
  • Dan Yakir
    Environmental Sciences and Energy Research Weizmann Institute of Science Rehovot Israel
  • Zhengxin Zhu
    NASA Goddard Space Flight Center Greenbelt Maryland USA

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<jats:title>Abstract</jats:title><jats:p>Carbonyl sulfide (COS) is an atmospheric trace gas that participates in some key reactions of the carbon cycle and thus holds great promise for studies of carbon cycle processes. Global monitoring networks and atmospheric sampling programs provide concurrent data on COS and CO<jats:sub>2</jats:sub> concentrations in the free troposphere and atmospheric boundary layer over vegetated areas. Here we present a modeling framework for interpreting these data and illustrate what COS measurements might tell us about carbon cycle processes. We implemented mechanistic and empirical descriptions of leaf and soil COS uptake into a global carbon cycle model (SiB 3) to obtain new estimates of the COS land flux. We then introduced these revised boundary conditions to an atmospheric transport model (Parameterized Chemical Transport Model) to simulate the variations in the concentration of COS and CO<jats:sub>2</jats:sub> in the global atmosphere. To balance the threefold increase in the global vegetation sink relative to the previous baseline estimate, we propose a new ocean COS source. Using a simple inversion approach, we optimized the latitudinal distribution of this ocean source and found that it is concentrated in the tropics. The new model is capable of reproducing the seasonal variation in atmospheric concentration at most background atmospheric sites. The model also reproduces the observed large vertical gradients in COS between the boundary layer and free troposphere. Using a simulation experiment, we demonstrate that comparing drawdown of CO<jats:sub>2</jats:sub> with COS could provide additional constraints on differential responses of photosynthesis and respiration to environmental forcing. The separation of these two distinct processes is essential to understand the carbon cycle components for improved prediction of future responses of the terrestrial biosphere to changing environmental conditions.</jats:p>

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