14
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: not found

      Recent global decline of CO2 fertilization effects on vegetation photosynthesis

      1 , 2 , 1 , 2 , 3 , 1 , 2 , 1 , 4 , 5 , 6 , 7 , 8 , 9 , 1 , 2 , 10 , 11 , 9 , 6 , 12 , 13 , 14 , 15 , 1 , 2 , 16 , 17 , 5 , 18 , 19 , 20 , 21 , 21 , 22 , 23 , 24 , 25 , 5 , 26 , 12 , 27 , 5 , 28 , 7 , 8
      Science
      American Association for the Advancement of Science (AAAS)

      Read this article at

      ScienceOpenPublisherPubMed
      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          The enhanced vegetation productivity driven by increased concentrations of carbon dioxide (CO 2) [i.e., the CO 2 fertilization effect (CFE)] sustains an important negative feedback on climate warming, but the temporal dynamics of CFE remain unclear. Using multiple long-term satellite- and ground-based datasets, we showed that global CFE has declined across most terrestrial regions of the globe from 1982 to 2015, correlating well with changing nutrient concentrations and availability of soil water. Current carbon cycle models also demonstrate a declining CFE trend, albeit one substantially weaker than that from the global observations. This declining trend in the forcing of terrestrial carbon sinks by increasing amounts of atmospheric CO 2 implies a weakening negative feedback on the climatic system and increased societal dependence on future strategies to mitigate climate warming.

          Related collections

          Most cited references124

          • Record: found
          • Abstract: found
          • Article: not found

          A biochemical model of photosynthetic CO2 assimilation in leaves of C 3 species.

          Various aspects of the biochemistry of photosynthetic carbon assimilation in C3 plants are integrated into a form compatible with studies of gas exchange in leaves. These aspects include the kinetic properties of ribulose bisphosphate carboxylase-oxygenase; the requirements of the photosynthetic carbon reduction and photorespiratory carbon oxidation cycles for reduced pyridine nucleotides; the dependence of electron transport on photon flux and the presence of a temperature dependent upper limit to electron transport. The measurements of gas exchange with which the model outputs may be compared include those of the temperature and partial pressure of CO2(p(CO2)) dependencies of quantum yield, the variation of compensation point with temperature and partial pressure of O2(p(O2)), the dependence of net CO2 assimilation rate on p(CO2) and irradiance, and the influence of p(CO2) and irradiance on the temperature dependence of assimilation rate.
            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            The ERA-Interim reanalysis: configuration and performance of the data assimilation system

              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2)

              The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2) is the latest atmospheric reanalysis of the modern satellite era produced by NASA’s Global Modeling and Assimilation Office (GMAO). MERRA-2 assimilates observation types not available to its predecessor, MERRA, and includes updates to the Goddard Earth Observing System (GEOS) model and analysis scheme so as to provide a viable ongoing climate analysis beyond MERRA’s terminus. While addressing known limitations of MERRA, MERRA-2 is also intended to be a development milestone for a future integrated Earth system analysis (IESA) currently under development at GMAO. This paper provides an overview of the MERRA-2 system and various performance metrics. Among the advances in MERRA-2 relevant to IESA are the assimilation of aerosol observations, several improvements to the representation of the stratosphere including ozone, and improved representations of cryospheric processes. Other improvements in the quality of MERRA-2 compared with MERRA include the reduction of some spurious trends and jumps related to changes in the observing system, and reduced biases and imbalances in aspects of the water cycle. Remaining deficiencies are also identified. Production of MERRA-2 began in June 2014 in four processing streams, and converged to a single near-real time stream in mid 2015. MERRA-2 products are accessible online through the NASA Goddard Earth Sciences Data Information Services Center (GES DISC).
                Bookmark

                Author and article information

                Contributors
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                (View ORCID Profile)
                Journal
                Science
                Science
                American Association for the Advancement of Science (AAAS)
                0036-8075
                1095-9203
                December 10 2020
                December 11 2020
                December 10 2020
                December 11 2020
                : 370
                : 6522
                : 1295-1300
                Affiliations
                [1 ]International Institute for Earth System Science, Nanjing University, Nanjing, Jiangsu 210023, China.
                [2 ]Jiangsu Provincial Key Laboratory of Geographic Information Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing, Jiangsu 210023, China.
                [3 ]Huangshan Park Ecosystem Observation and Research Station, Ministry of Education, Huangshan, China.
                [4 ]Department of Geography and Planning, University of Toronto, Toronto, Ontario, Canada.
                [5 ]Laboratoire des Sciences du Climat et de l’Environnement, CEA CNRS UVSQ, Gif-sur-Yvette, France.
                [6 ]European Commission, Joint Research Centre (JRC), Ispra, Italy.
                [7 ]CSIC, Global ecology Unit CREAF-CSIC-UAB, Bellaterra 08193, Catalonia, Spain.
                [8 ]CREAF, Cerdanyola del Vallès 08193, Catalonia, Spain.
                [9 ]Department of Biology, Centre of Excellence PLECO (Plant and Vegetation Ecology), University of Antwerp, Wilrijk, Belgium.
                [10 ]Department of Global Ecology, Carnegie Institution for Science, Stanford, CA 94305, USA.
                [11 ]Sierra Nevada Research Institute, University of California, Merced, CA 95343, USA.
                [12 ]College of Life and Environmental Sciences, University of Exeter, Exeter, UK.
                [13 ]College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, UK.
                [14 ]School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, USA.
                [15 ]School of Atmospheric Sciences, Center for Monsoon and Environment Research, Sun Yat-Sen University, Guangzhou, China.
                [16 ]Terrestrial Sciences Section, National Center for Atmospheric Research, Boulder, CO, USA.
                [17 ]Forest Research Institute Baden-Württemberg, Freiburg, Germany.
                [18 ]Climate and Environmental Physics, Physics Institute, and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland.
                [19 ]Institute of Applied Energy, Tokyo, Japan.
                [20 ]NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.
                [21 ]Thünen Institute of Forest Ecosystems, Alfred-Möller-Str. 1, 16225 Eberswalde, Germany.
                [22 ]Department of Environmental Science and Engineering, Fudan University, Shanghai, 200433, China.
                [23 ]Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD 20742, USA.
                [24 ]LASG, Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029, China.
                [25 ]International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL, USA.
                [26 ]Department of Atmospheric Sciences, University of Illinois, 105 South Gregory Street, Urbana, IL 61801-3070, USA.
                [27 ]CSIRO Oceans and Atmosphere, Canberra, ACT 2601, Australia.
                [28 ]Institute of Geography, University of Augsburg, Augsburg, Germany.
                Article
                10.1126/science.abb7772
                33303610
                90fabd7a-c221-4c00-9f63-272e888d4bac
                © 2020

                https://www.sciencemag.org/about/science-licenses-journal-article-reuse

                History

                Comments

                Comment on this article