Schematic illustration of the natural sources and sinks for remote sensing of OCS, SIF, and CO2. The natural carbon cycle (red) is dominated by exchanges between terrestrial photosynthesis (GPP), ecosystem respiration (Re), and the surface and deep oceans. The dominant global OCS fluxes (green) are the plant sink and surface ocean source. SIF is directly emitted from leaves. These three signals provide highly complementary views into net ecosystem exchange (CO2) and controls on photosynthesis that are biophysical (OCS) and biogeochemical (SIF).
Image credit: Keck Institute for Space Studies / Chuck Carter.