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      Increased nitrous oxide emissions from global lakes and reservoirs since the pre-industrial era

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          Abstract

          Lentic systems (lakes and reservoirs) are emission hotpots of nitrous oxide (N 2O), a potent greenhouse gas; however, this has not been well quantified yet. Here we examine how multiple environmental forcings have affected N 2O emissions from global lentic systems since the pre-industrial period. Our results show that global lentic systems emitted 64.6 ± 12.1 Gg N 2O-N yr −1 in the 2010s, increased by 126% since the 1850s. The significance of small lentic systems on mitigating N 2O emissions is highlighted due to their substantial emission rates and response to terrestrial environmental changes. Incorporated with riverine emissions, this study indicates that N 2O emissions from global inland waters in the 2010s was 319.6 ± 58.2 Gg N yr −1. This suggests a global emission factor of 0.051% for inland water N 2O emissions relative to agricultural nitrogen applications and provides the country-level emission factors (ranging from 0 to 0.341%) for improving the methodology for national greenhouse gas emission inventories.

          Abstract

          Modeling shows that N 2O emissions from global lakes and reservoirs have doubled since the pre-industrial era, this was mainly caused by widespread agricultural nitrogen application.

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          Most cited references72

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          Matplotlib: A 2D Graphics Environment

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            Nitrous oxide (N2O): the dominant ozone-depleting substance emitted in the 21st century.

            By comparing the ozone depletion potential-weighted anthropogenic emissions of N2O with those of other ozone-depleting substances, we show that N2O emission currently is the single most important ozone-depleting emission and is expected to remain the largest throughout the 21st century. N2O is unregulated by the Montreal Protocol. Limiting future N2O emissions would enhance the recovery of the ozone layer from its depleted state and would also reduce the anthropogenic forcing of the climate system, representing a win-win for both ozone and climate.
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              A comprehensive quantification of global nitrous oxide sources and sinks

              Nitrous oxide (N2O), like carbon dioxide, is a long-lived greenhouse gas that accumulates in the atmosphere. Over the past 150 years, increasing atmospheric N2O concentrations have contributed to stratospheric ozone depletion1 and climate change2, with the current rate of increase estimated at 2 per cent per decade. Existing national inventories do not provide a full picture of N2O emissions, owing to their omission of natural sources and limitations in methodology for attributing anthropogenic sources. Here we present a global N2O inventory that incorporates both natural and anthropogenic sources and accounts for the interaction between nitrogen additions and the biochemical processes that control N2O emissions. We use bottom-up (inventory, statistical extrapolation of flux measurements, process-based land and ocean modelling) and top-down (atmospheric inversion) approaches to provide a comprehensive quantification of global N2O sources and sinks resulting from 21 natural and human sectors between 1980 and 2016. Global N2O emissions were 17.0 (minimum-maximum estimates: 12.2-23.5) teragrams of nitrogen per year (bottom-up) and 16.9 (15.9-17.7) teragrams of nitrogen per year (top-down) between 2007 and 2016. Global human-induced emissions, which are dominated by nitrogen additions to croplands, increased by 30% over the past four decades to 7.3 (4.2-11.4) teragrams of nitrogen per year. This increase was mainly responsible for the growth in the atmospheric burden. Our findings point to growing N2O emissions in emerging economies-particularly Brazil, China and India. Analysis of process-based model estimates reveals an emerging N2O-climate feedback resulting from interactions between nitrogen additions and climate change. The recent growth in N2O emissions exceeds some of the highest projected emission scenarios3,4, underscoring the urgency to mitigate N2O emissions.
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                Author and article information

                Contributors
                hanqin.tian@bc.edu
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                31 January 2024
                31 January 2024
                2024
                : 15
                : 942
                Affiliations
                [1 ]GRID grid.9227.e, ISNI 0000000119573309, State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, , Chinese Academy of Sciences, ; Beijing, 100085 China
                [2 ]International Center for Climate and Global Change Research, Auburn University, ( https://ror.org/02v80fc35) Auburn, AL 36849 USA
                [3 ]University of Chinese Academy of Sciences, ( https://ror.org/05qbk4x57) Beijing, 100049 China
                [4 ]Center for Earth System Science and Global Sustainability, Schiller Institute for Integrated Science and Society, Department of Earth and Environmental Sciences, Boston College, ( https://ror.org/02n2fzt79) Chestnut Hill, MA 02467 USA
                [5 ]School of Geographic Sciences, East China Normal University, ( https://ror.org/02n96ep67) Shanghai, 610000 China
                [6 ]School of Geography, Nanjing Normal University, ( https://ror.org/036trcv74) Nanjing, 210023 China
                [7 ]College of Urban and Environmental Sciences, Peking University, ( https://ror.org/02v51f717) Beijing, 100871 China
                [8 ]School of Geography, University of Leeds, ( https://ror.org/024mrxd33) Leeds, LS2 9JT UK
                [9 ]Université Paris-Saclay, INRAE, AgroParisTech, UMR ECOSYS, ( https://ror.org/03xjwb503) Palaiseau, 91120 France
                [10 ]Department of Engineering, Boston College, ( https://ror.org/02n2fzt79) Chestnut Hill, MA 02467 USA
                Author information
                http://orcid.org/0000-0002-8238-7274
                http://orcid.org/0000-0002-1806-4091
                http://orcid.org/0000-0001-8250-0567
                http://orcid.org/0000-0003-2310-3662
                http://orcid.org/0000-0003-3153-1587
                http://orcid.org/0000-0001-6677-9262
                http://orcid.org/0000-0001-5554-0897
                Article
                45061
                10.1038/s41467-024-45061-0
                10830459
                38296943
                5003e45e-1ced-4424-bc63-1c6c9086350c
                © The Author(s) 2024

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 24 June 2023
                : 11 January 2024
                Funding
                Funded by: FundRef https://doi.org/10.13039/100000001, National Science Foundation (NSF);
                Award ID: 243232
                Award ID: 1922687
                Award Recipient :
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                © Springer Nature Limited 2024

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