沿海海洋中的碳通量:综合、边界过程和未来趋势

IF 11.3 1区 地球科学 Q1 ASTRONOMY & ASTROPHYSICS
M. Dai, Jianzhong Su, Yangyang Zhao, E. Hofmann, Zhimian Cao, W. Cai, J. Gan, Fabrice Lacroix, G. Laruelle, Feifei Meng, J. Müller, P. Régnier, Guizhi Wang, Zhixuan Wang
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引用次数: 30

摘要

本文综述了目前对全球沿海海洋碳循环的认识,并提供了一种新的海气二氧化碳交换定量合成方法。这一再分析得出全球综合沿海海洋CO2通量的估计值为- 0.25±0.05 Pg C年- 1,其中极地和亚极地地区占CO2去除的大部分(>90%)。将河流主导的海洋边缘(RiOMar)和海洋主导的边缘(OceMar)系统分类的框架用于概念化沿海碳循环过程。对比了波罗的海、中大西洋湾和南海3个不同区域的地表pCO2的时空变化特征。从模拟关键过程和预测不同大陆架区域未来变化的能力方面,综述了从箱型模式到三维耦合循环-生物地球化学模式的海洋碳模型。在RiOMar和OceMar系统中实现这些模型仍然存在一些未解决的挑战。强调了在观测和数值模拟中出现的不同海岸系统在人为压力下沿海海洋碳通量的长期趋势。在陆地-海洋-大气耦合系统同步变化的背景下,预测与净零二氧化碳排放前后相关的未来扰动方面的知识缺口构成了一个关键挑战。■一项新的合成估算出全球综合沿海海洋碳汇的年- 1为- 0.25 Pg C,其中90%以上的大气二氧化碳清除发生在极地和亚极地地区。■沿海和开放海洋的持续碳汇对于减缓气候变化和实现《巴黎协定》设定的目标至关重要。▪未来沿海海洋碳循环的不确定性与陆地-海洋-大气耦合系统的同步趋势和变化有关。▪为目前沿海海洋碳研究确定的主要差距和挑战对气候和可持续性政策具有重要影响。《地球与行星科学年度评论》第50卷的最终在线出版日期预计为2022年5月。修订后的估计数请参阅http://www.annualreviews.org/page/journal/pubdates。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Carbon Fluxes in the Coastal Ocean: Synthesis, Boundary Processes and Future Trends
This review examines the current understanding of the global coastal ocean carbon cycle and provides a new quantitative synthesis of air-sea CO2 exchange. This reanalysis yields an estimate for the globally integrated coastal ocean CO2 flux of −0.25 ± 0.05 Pg C year−1, with polar and subpolar regions accounting for most of the CO2 removal (>90%). A framework that classifies river-dominated ocean margin (RiOMar) and ocean-dominated margin (OceMar) systems is used to conceptualize coastal carbon cycle processes. The carbon dynamics in three contrasting case study regions, the Baltic Sea, the Mid-Atlantic Bight, and the South China Sea, are compared in terms of the spatio-temporal variability of surface pCO2. Ocean carbon models that range from box models to three-dimensional coupled circulation-biogeochemical models are reviewed in terms of the ability to simulate key processes and project future changes in different continental shelf regions. Common unresolved challenges remain for implementation of these models across RiOMar and OceMar systems. The long-term trends in coastal ocean carbon fluxes for different coastal systems under anthropogenic stress that are emerging in observations and numerical simulations are highlighted. Knowledge gaps in projecting future perturbations associated with before and after net-zero CO2 emissions in the context of concurrent changes in the land-ocean-atmosphere coupled system pose a key challenge. ▪ A new synthesis yields an estimate for globally integrated coastal ocean carbon sink of −0.25 Pg C year−1, with greater than 90% of atmospheric CO2 removal occurring in polar and subpolar regions. ▪ The sustained coastal and open ocean carbon sink is vital in mitigating climate change and meeting the target set by the Paris Agreement. ▪ Uncertainties in the future coastal ocean carbon cycle are associated with concurrent trends and changes in the land-ocean-atmosphere coupled system. ▪ The major gaps and challenges identified for current coastal ocean carbon research have important implications for climate and sustainability policies. Expected final online publication date for the Annual Review of Earth and Planetary Sciences, Volume 50 is May 2022. Please see http://www.annualreviews.org/page/journal/pubdates for revised estimates.
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来源期刊
Annual Review of Earth and Planetary Sciences
Annual Review of Earth and Planetary Sciences 地学天文-地球科学综合
CiteScore
25.10
自引率
0.00%
发文量
25
期刊介绍: Since its establishment in 1973, the Annual Review of Earth and Planetary Sciences has been dedicated to providing comprehensive coverage of advancements in the field. This esteemed publication examines various aspects of earth and planetary sciences, encompassing climate, environment, geological hazards, planet formation, and the evolution of life. To ensure wider accessibility, the latest volume of the journal has transitioned from a gated model to open access through the Subscribe to Open program by Annual Reviews. Consequently, all articles published in this volume are now available under the Creative Commons Attribution (CC BY) license.
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