TY - JOUR
T1 - Global nitrous oxide budget (1980-2020)
AU - Tian, Hanqin
AU - Pan, Naiqing
AU - Thompson, Rona L.
AU - Canadell, Josep G.
AU - Suntharalingam, Parvadha
AU - Regnier, Pierre
AU - Davidson, Eric A.
AU - Prather, Michael
AU - Ciais, Philippe
AU - Muntean, Marilena
AU - Pan, Shufen
AU - Winiwarter, Wilfried
AU - Zaehle, Sönke
AU - Zhou, Feng
AU - Jackson, Robert B.
AU - Bange, Hermann W.
AU - Berthet, Sarah
AU - Bian, Zihao
AU - Bianchi, Daniele
AU - Bouwman, Alexander F.
AU - Buitenhuis, Erik T.
AU - Dutton, Geoffrey
AU - Hu, Minpeng
AU - Ito, Akihiko
AU - Jain, Atul K.
AU - Jeltsch-Thömmes, Aurich
AU - Joos, Fortunat
AU - Kou-Giesbrecht, Sian
AU - Krummel, Paul B.
AU - Lan, Xin
AU - Landolfi, Angela
AU - Lauerwald, Ronny
AU - Li, Ya
AU - Lu, Chaoqun
AU - Maavara, Taylor
AU - Manizza, Manfredi
AU - Millet, Dylan B.
AU - Mühle, Jens
AU - Patra, Prabir K.
AU - Peters, Glen P.
AU - Qin, Xiaoyu
AU - Raymond, Peter
AU - Resplandy, Laure
AU - Rosentreter, Judith A.
AU - Shi, Hao
AU - Sun, Qing
AU - Tonina, Daniele
AU - Tubiello, Francesco N.
AU - Van Der Werf, Guido R.
AU - Vuichard, Nicolas
AU - Wang, Junjie
AU - Wells, Kelley C.
AU - Western, Luke M.
AU - Wilson, Chris
AU - Yang, Jia
AU - Yao, Yuanzhi
AU - You, Yongfa
AU - Zhu, Qing
N1 - This paper is the result of a collaborative international effort under the umbrella of the Global Carbon Project (a project of Future Earth and a research partner of the World Climate Research Programme) in partnership with the International Nitrogen Initiative (INI). We acknowledge all of the people and institutions who provided the data used in the global nitrous oxide budget as well as the institutions funding parts of this effort (see Table A4). We acknowledge the modeling groups for making their simulations available for this analysis. The PyVAR-CAMS modeling results were funded through the Copernicus Atmosphere Monitoring Service, implemented by ECMWF on behalf of the European Commission, and were generated using computing resources from LSCE. Hanqin Tian and Shufen Pan acknowledge computational and administrative support from the Center for Earth System Science and Global Sustainability, Schiller Institute for Integrated Science and Society at Boston College. Josep G. Canadell thanks the Australian National Environmental Science Program \u2013 Climate Systems Hub for supporting the GHG budget activities of the Global Carbon Project (GCP), including the global and regional NO budget work. We are grateful to the EDGAR team (Monica Crippa, Diego Guizzardi, Edwin Schaaf, Marilena Muntean, Efisio Solazzo, Federico Pagani, and Manjola Banja) for the work needed to publish the EDGARv7.0 Global Greenhouse Gas Emissions dataset ( https://edgar.jrc.ec.europa.eu/dataset_ghg70 , last access: 10 February 2022). Atul K. Jain thanks Shijie Shu and Tzu-Shun Lin for their involvement in developing and analyzing the ISAM model products used here. Giulia Conchedda, Griffiths Obli-Layrea, and Nathan Wanner contributed significant efforts to the generation of fertilizer, livestock, and soil nutrient data that underlie FAO's estimates of NO data.
This paper is the result of a collaborative international effort under the umbrella of the Global Carbon Project (a project of Future Earth and a research partner of the World Climate Research Programme) in partnership with the International Nitrogen Initiative (INI). We acknowledge all of the people and institutions who provided the data used in the global nitrous oxide budget as well as the institutions funding parts of this effort (see Table A4). We acknowledge the modeling groups for making their simulations available for this analysis. The PyVAR-CAMS modeling results were funded through the Copernicus Atmosphere Monitoring Service, implemented by ECMWF on behalf of the European Commission, and were generated using computing resources from LSCE. Hanqin Tian and Shufen Pan acknowledge computational and administrative support from the Center for Earth System Science and Global Sustainability, Schiller Institute for Integrated Science and Society at Boston College. Josep G. Canadell thanks the Australian National Environmental Science Program - Climate Systems Hub for supporting the GHG budget activities of the Global Carbon Project (GCP), including the global and regional N2O budget work. We are grateful to the EDGAR team (Monica Crippa, Diego Guizzardi, Edwin Schaaf, Marilena Muntean, Efisio Solazzo, Federico Pagani, and Manjola Banja) for the work needed to publish the EDGARv7.0 Global Greenhouse Gas Emissions dataset (https://edgar.jrc.ec.europa.eu/dataset_ghg70, last access: 10 February 2022). Atul K. Jain thanks Shijie Shu and Tzu-Shun Lin for their involvement in developing and analyzing the ISAM model products used here. Giulia Conchedda, Griffiths Obli-Layrea, and Nathan Wanner contributed significant efforts to the generation of fertilizer, livestock, and soil nutrient data that underlie FAO's estimates of N2O data.
PY - 2024/6/11
Y1 - 2024/6/11
N2 - Nitrous oxide (N2O) is a long-lived potent greenhouse gas and stratospheric ozone-depleting substance that has been accumulating in the atmosphere since the preindustrial period. The mole fraction of atmospheric N2O has increased by nearly 25 % from 270 ppb (parts per billion) in 1750 to 336 ppb in 2022, with the fastest annual growth rate since 1980 of more than 1.3 ppb yr-1 in both 2020 and 2021. According to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR6), the relative contribution of N2O to the total enhanced effective radiative forcing of greenhouse gases was 6.4 % for 1750-2022. As a core component of our global greenhouse gas assessments coordinated by the Global Carbon Project (GCP), our global N2O budget incorporates both natural and anthropogenic sources and sinks and accounts for the interactions between nitrogen additions and the biogeochemical processes that control N2O emissions. We use bottomup (BU: inventory, statistical extrapolation of flux measurements, and process-based land and ocean modeling) and top-down (TD: atmospheric measurement-based inversion) approaches. We provide a comprehensive quantification of global N2O sources and sinks in 21 natural and anthropogenic categories in 18 regions between 1980 and 2020. We estimate that total annual anthropogenic N2O emissions have increased 40 % (or 1.9 Tg N yr-1) in the past 4 decades (1980-2020). Direct agricultural emissions in 2020 (3.9 Tg N yr-1, best estimate) represent the large majority of anthropogenic emissions, followed by other direct anthropogenic sources, including fossil fuel and industry, waste and wastewater, and biomass burning (2.1 Tg N yr-1), and indirect anthropogenic sources (1.3 Tg N yr-1) . For the year 2020, our best estimate of total BU emissions for natural and anthropogenic sources was 18.5 (lower-upper bounds: 10.6-27.0) Tg N yr-1, close to our TD estimate of 17.0 (16.6-17.4) Tg N yr-1. For the 2010-2019 period, the annual BU decadal-average emissions for both natural and anthropogenic sources were 18.2 (10.6-25.9) Tg N yr-1 and TD emissions were 17.4 (15.8-19.20) Tg N yr-1. The once top emitter Europe has reduced its emissions by 31 % since the 1980s, while those of emerging economies have grown, making China the top emitter since the 2010s. The observed atmospheric N2O concentrations in recent years have exceeded projected levels under all scenarios in the Coupled Model Intercomparison Project Phase 6 (CMIP6), underscoring the importance of reducing anthropogenic N2O emissions. To evaluate mitigation efforts and contribute to the Global Stocktake of the United Nations Framework Convention on Climate Change, we propose the establishment of a global network for monitoring and modeling N2O from the surface through to the stratosphere. The data presented in this work can be downloaded from https://doi.org/10.18160/RQ8P-2Z4R (Tian et al., 2023).
AB - Nitrous oxide (N2O) is a long-lived potent greenhouse gas and stratospheric ozone-depleting substance that has been accumulating in the atmosphere since the preindustrial period. The mole fraction of atmospheric N2O has increased by nearly 25 % from 270 ppb (parts per billion) in 1750 to 336 ppb in 2022, with the fastest annual growth rate since 1980 of more than 1.3 ppb yr-1 in both 2020 and 2021. According to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC AR6), the relative contribution of N2O to the total enhanced effective radiative forcing of greenhouse gases was 6.4 % for 1750-2022. As a core component of our global greenhouse gas assessments coordinated by the Global Carbon Project (GCP), our global N2O budget incorporates both natural and anthropogenic sources and sinks and accounts for the interactions between nitrogen additions and the biogeochemical processes that control N2O emissions. We use bottomup (BU: inventory, statistical extrapolation of flux measurements, and process-based land and ocean modeling) and top-down (TD: atmospheric measurement-based inversion) approaches. We provide a comprehensive quantification of global N2O sources and sinks in 21 natural and anthropogenic categories in 18 regions between 1980 and 2020. We estimate that total annual anthropogenic N2O emissions have increased 40 % (or 1.9 Tg N yr-1) in the past 4 decades (1980-2020). Direct agricultural emissions in 2020 (3.9 Tg N yr-1, best estimate) represent the large majority of anthropogenic emissions, followed by other direct anthropogenic sources, including fossil fuel and industry, waste and wastewater, and biomass burning (2.1 Tg N yr-1), and indirect anthropogenic sources (1.3 Tg N yr-1) . For the year 2020, our best estimate of total BU emissions for natural and anthropogenic sources was 18.5 (lower-upper bounds: 10.6-27.0) Tg N yr-1, close to our TD estimate of 17.0 (16.6-17.4) Tg N yr-1. For the 2010-2019 period, the annual BU decadal-average emissions for both natural and anthropogenic sources were 18.2 (10.6-25.9) Tg N yr-1 and TD emissions were 17.4 (15.8-19.20) Tg N yr-1. The once top emitter Europe has reduced its emissions by 31 % since the 1980s, while those of emerging economies have grown, making China the top emitter since the 2010s. The observed atmospheric N2O concentrations in recent years have exceeded projected levels under all scenarios in the Coupled Model Intercomparison Project Phase 6 (CMIP6), underscoring the importance of reducing anthropogenic N2O emissions. To evaluate mitigation efforts and contribute to the Global Stocktake of the United Nations Framework Convention on Climate Change, we propose the establishment of a global network for monitoring and modeling N2O from the surface through to the stratosphere. The data presented in this work can be downloaded from https://doi.org/10.18160/RQ8P-2Z4R (Tian et al., 2023).
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U2 - 10.5194/essd-16-2543-2024
DO - 10.5194/essd-16-2543-2024
M3 - Article
AN - SCOPUS:85196431315
SN - 1866-3508
VL - 16
SP - 2543
EP - 2604
JO - Earth System Science Data
JF - Earth System Science Data
IS - 6
ER -