概括
从1850年到1950年,生物圈释放出大量的二氧化碳 (CO2),减少了生物质. 海洋吸收了47%的过剩CO2,留下53%的空气.
科学领域:
- 环境科学 环境科学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 自从工业革命以来,大气中的二氧化碳 (CO2) 水平大幅上升.
- 土地利用变化影响陆地生物质和碳循环.
- 海洋吸收是调节大气二氧化碳度的关键因素.
研究的目的:
- 量化1850年至1950年间生物圈到大气中的二氧化碳净排放量.
- 评估土地利用变化对陆地生物质的影响.
- 为了确定从化石燃料中获得的二氧化碳在大气和海洋海底之间的分布.
主要方法:
- 基于历史数据的生物圈净二氧化碳排放估计.
- 量化由于土地利用变化的陆地生物质变化.
- 在热带和深海地区对海洋二氧化碳吸收的分析.
主要成果:
- 从1850年到1950年,生物圈的净二氧化碳排放平均每年为1.2 x 10^9的碳.
- 在此期间,由于土地利用变化,陆地生物量减少了7%.
- 自1850年以来,大气中的二氧化碳含量增加了18%,其中53%仍在空气中传播.
结论:
- 在工业初期,生物圈是大气二氧化碳的净来源.
- 海洋下沉点,特别是热带旋转,在缓解大气二氧化碳上升方面发挥着至关重要的作用.
- 大多数人为产生的二氧化碳仍留在大气中,导致气候变化.
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