Global nitrous oxide budget (1980–2020)

IF 11.2 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Earth System Science Data Pub Date : 2024-06-11 DOI:10.5194/essd-16-2543-2024
Hanqin Tian, Naiqing Pan, Rona L. Thompson, Josep G. Canadell, Parvadha Suntharalingam, Pierre Regnier, Eric A. Davidson, Michael Prather, Philippe Ciais, Marilena Muntean, Shufen Pan, Wilfried Winiwarter, Sönke Zaehle, Feng Zhou, Robert B. Jackson, Hermann W. Bange, Sarah Berthet, Zihao Bian, Daniele Bianchi, Alexander F. Bouwman, Erik T. Buitenhuis, Geoffrey Dutton, Minpeng Hu, Akihiko Ito, Atul K. Jain, Aurich Jeltsch-Thömmes, Fortunat Joos, Sian Kou-Giesbrecht, Paul B. Krummel, Xin Lan, Angela Landolfi, Ronny Lauerwald, Ya Li, Chaoqun Lu, Taylor Maavara, Manfredi Manizza, Dylan B. Millet, Jens Mühle, Prabir K. Patra, Glen P. Peters, Xiaoyu Qin, Peter Raymond, Laure Resplandy, Judith A. Rosentreter, Hao Shi, Qing Sun, Daniele Tonina, Francesco N. Tubiello, Guido R. van der Werf, Nicolas Vuichard, Junjie Wang, Kelley C. Wells, Luke M. Western, Chris Wilson, Jia Yang, Yuanzhi Yao, Yongfa You, Qing Zhu
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Abstract

Abstract. 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 bottom-up (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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全球一氧化二氮预算(1980-2020 年)
摘要一氧化二氮(N2O)是一种长寿命的强效温室气体和平流层臭氧消耗物质,自前工业化时期以来一直在大气中累积。大气中氧化亚氮的摩尔分数从 1750 年的 270 ppb(十亿分之一)增加到 2022 年的 336 ppb,增加了近 25%,其中 2020 年和 2021 年的年增长率超过 1.3 ppb-1,是自 1980 年以来最快的年增长率。根据《政府间气候变化专门委员会第六次评估报告》(IPCC AR6),1750-2022 年期间,一氧化二氮对温室气体总的增强有效辐射强迫的相对贡献率为 6.4%。作为全球碳项目(GCP)协调的全球温室气体评估的核心组成部分,我们的全球一氧化二氮预算包含了自然和人为源和汇,并考虑了氮添加和控制一氧化二氮排放的生物地球化学过程之间的相互作用。我们采用了自下而上(BU:清单、通量测量的统计外推法以及基于过程的陆地和海洋建模)和自上而下(TD:基于大气测量的反演)的方法。我们对 1980-2020 年间全球 18 个地区 21 个自然和人为类别的一氧化二氮源和汇进行了全面量化。我们估计,在过去 40 年(1980-2020 年)中,每年的人为一氧化二氮排放总量增加了 40%(或每年 1.9 兆吨氮)。2020 年的直接农业排放(3.9 Tg N yr-1,最佳估计值)占人为排放的绝大部分,其次是其他直接人为排放源,包括化石燃料和工业、废物和废水以及生物质燃烧(2.1 Tg N yr-1),以及间接人为排放源(1.3 Tg N yr-1)。对于 2020 年,我们对自然源和人为源的生物量总排放量的最佳估计值为 18.5(下限-上限:10.6-27.0)兆吨氮年-1,接近于我们的技术发展估算值 17.0(16.6-17.4)兆吨氮年-1。2010-2019 年期间,自然源和人为源的年均 BU 排放量为 18.2(10.6-25.9)兆吨氮年-1,TD 排放量为 17.4(15.8-19.20)兆吨氮年-1。曾经的最大排放国欧洲自 20 世纪 80 年代以来已减少了 31%的排放量,而新兴经济体的排放量却在增加,中国自 2010 年代以来已成为最大排放国。近年来观测到的大气中一氧化二氮浓度超过了耦合模式相互比较项目第六阶段(CMIP6)中所有情景下的预测水平,这凸显了减少人为一氧化二氮排放的重要性。为了评估减排工作并为《联合国气候变化框架公约》的全球评估做出贡献,我们建议建立一个全球网络,对从地表到平流层的一氧化二氮进行监测和建模。本研究中的数据可从 https://doi.org/10.18160/RQ8P-2Z4R 下载(Tian 等人,2023 年)。
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来源期刊
Earth System Science Data
Earth System Science Data GEOSCIENCES, MULTIDISCIPLINARYMETEOROLOGY-METEOROLOGY & ATMOSPHERIC SCIENCES
CiteScore
18.00
自引率
5.30%
发文量
231
审稿时长
35 weeks
期刊介绍: Earth System Science Data (ESSD) is an international, interdisciplinary journal that publishes articles on original research data in order to promote the reuse of high-quality data in the field of Earth system sciences. The journal welcomes submissions of original data or data collections that meet the required quality standards and have the potential to contribute to the goals of the journal. It includes sections dedicated to regular-length articles, brief communications (such as updates to existing data sets), commentaries, review articles, and special issues. ESSD is abstracted and indexed in several databases, including Science Citation Index Expanded, Current Contents/PCE, Scopus, ADS, CLOCKSS, CNKI, DOAJ, EBSCO, Gale/Cengage, GoOA (CAS), and Google Scholar, among others.
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