Greenhouse Gas Budgets of Central and West Asia (2000–2020): A Significant Net Source to the Atmosphere

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES Global Biogeochemical Cycles Pub Date : 2025-02-27 DOI:10.1029/2024GB008370
Xiaoyu Qin, Hanqin Tian, Josep G. Canadell, Yu Shi, Shufen Pan, Ana Bastos, Philippe Ciais, Monica Crippa, Naiqing Pan, Prabir K. Patra, Benjamin Poulter, Marielle Saunois, Stephen Sitch
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Abstract

This study provides the first comprehensive quantification of three major greenhouse gases (GHGs, including CO2, CH4, and N2O) budgets for Central and West Asia (CWA) from 2000 to 2020, including contributions from fossil fuels, industry, and managed and unmanaged terrestrial ecosystems. We use bottom-up (BU: inventories and process-based models) and top-down approaches (TD: atmospheric inversions) to elucidate CWA's GHG budget and its changes. BU and TD budgets consistently show that CWA was a significant and growing GHG source during the 2010s: average net emissions were 4,175 (range: 4,055–4,301) Tg CO2eq yr−1 based on BU and using global warming potentials over a 100-year period (GWP100), and slightly higher net emissions of 4,293 (3,760–4,826) Tg CO2eq yr−1 based on TD. BU estimates show that CO2 emissions from fossil fuel combustion and fugitive releases were the dominant source, accounting for 61% of the total budget in the 2010s, with 2,554 (2,526–2,582) Tg CO2eq yr−1. Terrestrial natural ecosystems were a weak CO2 sink and sources of CH4 and N2O, which together resulted in a decadal mean net GHG emission of 220.5 (114.5–332.8) Tg CO2eq yr−1. Non-CO2 gases, primarily CH4, contributed significantly to the region's GHG emissions, accounting for 32% (BU) and 24% (TD) of CWA's total GHG budget under GWP100, and increasing to 57% (BU) and 49% (TD) with GWP20, highlighting CH4 stronger warming impact over shorter timescales. Overall, CWA contributed about 8% of global net GHG emissions in the 2010s, with about 10% of global CO2, 7% of CH4, and 3% of N2O.

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本研究首次全面量化了 2000 年至 2020 年中亚和西亚(CWA)的三大温室气体(GHGs,包括 CO2、CH4 和 N2O)预算,包括化石燃料、工业以及受管理和未受管理的陆地生态系统的贡献。我们采用自下而上(BU:清单和基于过程的模型)和自上而下(TD:大气反演)的方法来阐明中亚和西亚的温室气体预算及其变化。BU和TD预算一致表明,在2010年代,CWA是一个重要且不断增长的温室气体源:根据BU并使用100年期间的全球升温潜能值(GWP100),平均净排放量为每年4,175(范围:4,055-4,301)兆吨二氧化碳当量,而根据TD,净排放量略高,为每年4,293(3,760-4,826)兆吨二氧化碳当量。BU估算表明,化石燃料燃烧和逃逸释放产生的二氧化碳排放量是主要来源,占2010年代总预算的61%,为2,554 (2,526-2,582) Tg CO2eq yr-1。陆地自然生态系统是一个微弱的二氧化碳吸收汇,也是甲烷和氧化亚氮的来源,两者共同导致十年平均温室气体净排放量为 220.5 (114.5-332.8) Tg CO2eq yr-1。非二氧化碳气体,主要是甲烷(CH4),对该区域的温室气体排放贡献巨大,在 GWP100 下分别占 CWA 温室气体总预算的 32% (BU) 和 24% (TD),在 GWP20 下分别增至 57% (BU) 和 49% (TD),凸显了甲烷在更短的时间尺度上更强的变暖影响。总体而言,在 2010 年代,CWA 占全球温室气体净排放量的 8%,其中二氧化碳占全球排放量的 10%,甲烷占 7%,一氧化二氮占 3%。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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