概括
1988年,北大西洋的二氧化碳 (CO2) 净流量惊人地小,这与预期相反. 这项研究揭示了海洋是氧气 (O(2) 的更大的沉池,而不是大气中的CO(2).
科学领域:
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
- 气候科学 气候科学
背景情况:
- 北大西洋传统上被视为大气中二氧化碳 (CO2) 的重要沉点.
- 了解海洋气体交换对于气候建模和预测未来大气CO2度至关重要.
研究的目的:
- 量化二氧化碳 (CO2) 和氧气 (O2) 通过佛罗里达海峡和大约在北方25度处进入大西洋的总和净运输量.
- 评估1988年大气和北大西洋之间的CO2净流量.
主要方法:
- 测量了CO2和O2的度,以及相关的化学物种.
- 结合化学测量与海洋质量运输的估计.
- 计算了CO2和O2的北向和南向流量.
主要成果:
- 1988年,在北极25度的南方观测到每秒0.7 x 10 6的净CO2流量 (每年0.26 +/- 0.03千兆的碳).
- 在北方,O2的净输送量为2.08×106摩尔/秒,是CO2净流量的3倍.
- 北大西洋作为二氧化碳吸收的作用小于预期,尽管热量损失很大.
结论:
- 在1988年,北大西洋是大气中二氧化碳的相对较小的沉积点.
- 在这个度上,海洋是O2比CO2更大的沉池.
- 热和化学效应对CO2和O2循环有不同的影响,影响净气体交换.
相关概念视频
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