不对称的气泡介导气体转移增强了全球海洋的二氧化碳吸收
Yuanxu Dong1,2, Mingxi Yang3, Thomas G Bell3
1Marine Biogeochemistry Research Division, GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany. ydong@geomar.de.
Nature communications
|November 25, 2025
概括
海洋二氧化碳 (CO2) 的吸收高于估计,这是由于气泡介导的气体交换有利于CO2的入侵. 这项研究为这种不对称性提供了实地证据,改善了CO2流量评估.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 地质化学 地质化学
背景情况:
- 海洋空气二氧化碳 (CO2) 流对于气候调节至关重要.
- 目前的模型假定气体转移是对称的,忽视了泡效应.
- 缺乏非对称的气泡介导CO2转移的现场证据.
研究的目的:
- 提供非对称气泡介导的二氧化碳转移的直接现场证据.
- 开发一个不对称的二氧化碳流量方程.
- 重新评估全球海洋二氧化碳吸收.
主要方法:
- 气体转移速度 (K) 的现场测量.
- 开发一种包含泡效应的不对称流量方程.
- 将新估计与传统模型进行比较.
主要成果:
- 直接的实地证据证实,气泡介导的二氧化碳转移有利于入侵.
- 不对称方程减少了K估计中的偏差.
- 全球海洋二氧化碳的吸收增加了0.3-0.4 Pg C yr-1 (约为0.4 Pg C yr-1). 15%) 从1991年到2020年.
结论:
- 海洋可能吸收的二氧化碳比以前想象的要多.
- 对于准确的二氧化碳吸收评估,需要一个不对称的流量方程.
- 需要更多关于二氧化碳逃逸的数据来完善不对称性量化.
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