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Eldering, A.; Wennberg, P. O.; Crisp, D.; Schimel, D. S.; Gunson, M. R.; Chatterjee, A.; Liu, J.; Schwandner, F. M.; Sun, Y.; O’Dell, C. W.; Frankenberg, C.; Taylor, T.; Fisher, B.; Osterman, G. B.; Wunch, D.; Hakkarainen, J.; Tamminen, J.; Weir, B.
Science (American Association for the Advancement of Science), 10/2017, Volume: 358, Issue: 6360Journal Article
NASA's Orbiting Carbon Observatory-2 (OCO-2) mission was motivated by the need to diagnose how the increasing concentration of atmospheric carbon dioxide (CO ) is altering the productivity of the biosphere and the uptake of CO by the oceans. Launched on 2 July 2014, OCO-2 provides retrievals of the column-averaged CO dry-air mole fraction (Formula: see text) as well as the fluorescence from chlorophyll in terrestrial plants. The seasonal pattern of uptake by the terrestrial biosphere is recorded in fluorescence and the drawdown of Formula: see text during summer. Launched just before one of the most intense El Niños of the past century, OCO-2 measurements of Formula: see text and fluorescence record the impact of the large change in ocean temperature and rainfall on uptake and release of CO by the oceans and biosphere.
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