概括
从1970年到1990年,太平洋每年吸收2.1亿二氧化碳 (CO2),主要来自化石燃料. 这表明海洋是主要的二氧化碳 (CO2) 沉积点,生物圈没有显著的释放.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 1970年至1990年间,太平洋表面水中溶解无机碳的三角洲值下降了0.4每毫米.
- 这种同位素转移归因于从化石燃料燃烧和森林砍伐中产生的大气二氧化碳 (CO2) 的吸收.
研究的目的:
- 量化1970年至1990年间海洋吸收和生物圈释放的CO2净量.
- 确定海洋作为碳汇的作用,并评估生物圈在此期间释放的二氧化碳.
主要方法:
- 对大气中CO2度变化的分析.
- 测量大气中CO2的三角洲值.
- 评估海洋中溶解的无机碳的三角洲值.
主要成果:
- 计算的平均海洋净CO2吸收量为每年2.1千兆的碳.
- 同位素数据表明,海洋是人类产生的二氧化碳的主要净沉积点.
结论:
- 海洋在减轻大气中的CO2增加方面发挥着至关重要的作用.
- 在20年的研究期间,没有从生物圈中检测到任何显著的净CO2排放.
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