沿岸域の人為起源炭素(Coastal anthropogenic carbon)

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2024-08-20 デラウェア大学 (UD)

人間活動による二酸化炭素(CO2)が沿岸海域にどのように影響を与えているかを明らかにするため、デラウェア大学の研究チームが米国東海岸のデータを分析しました。表層水は大気中のCO2を直接吸収し、最も高い人為的CO2濃度を示しましたが、深層水では自然由来のCO2が優勢でした。また、沿岸から沖合への人為的CO2の輸送はほとんどなく、主に沖合の水塊と大気からの混合が原因とされています。この研究は、沿岸海域の炭素循環に対する理解を深めるものです。

<関連情報>

米国東海岸における人為起源炭素の発生源と蓄積 The source and accumulation of anthropogenic carbon in the U.S. East Coast

Xinyu Li, Zelun Wu, Zhangxian Ouyang, and Wei-Jun Cai
Science Advances  Published:9 Aug 2024
DOI:https://doi.org/10.1126/sciadv.adl3169

沿岸域の人為起源炭素(Coastal anthropogenic carbon)

Abstract

The ocean has absorbed anthropogenic carbon dioxide (Canthro) from the atmosphere and played an important role in mitigating global warming. However, how much Canthro is accumulated in coastal oceans and where it comes from have rarely been addressed with observational data. Here, we use a high-quality carbonate dataset (1996–2018) in the U.S. East Coast to address these questions. Our work shows that the offshore slope waters have the highest Canthro accumulation changes (ΔCanthro) consistent with water mass age and properties. From offshore to nearshore, ΔCanthro decreases with salinity to near zero in the subsurface, indicating no net increase in the export of Canthro from estuaries and wetlands. Excesses over the conservative mixing baseline also reveal an uptake of Canthro from the atmosphere within the shelf. Our analysis suggests that the continental shelf exports most of its absorbed Canthro from the atmosphere to the open ocean and acts as an essential pathway for global ocean Canthro storage and acidification.

1702地球物理及び地球化学
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