北极湖泊和河流作为气体导管进入大气层:对原碳预算的影响
概括
北极原的水生生态系统将二氧化碳 (CO2) 释放到大气中,这挑战了纯粹陆地碳汇的假设. 这一发现表明,目前的碳汇估计可能被高估了.
科学领域:
- 环境科学 环境科学
- 生态生态学 生态生态学
- 气候科学 气候科学
背景情况:
- 北极原储存了大量的碳,被认为是大气中的二氧化碳 (CO2) 的沉积点.
- 以前的碳平衡估计仅集中在陆地生态系统上,可能忽略了水生贡献.
研究的目的:
- 研究北极和阿拉斯加水生生态系统中的二氧化碳 (CO2) 流量.
- 评估水生系统在整个北极碳预算中的作用.
主要方法:
- 在29个不同的水生生态系统中测量二氧化碳 (CO2) 部分压力.
- 从地表水中释放到大气中的二氧化碳的分析.
主要成果:
- 在29个水生生态系统中,有27个显示出二氧化碳净释放到大气中的情况.
- 从水生系统中释放的二氧化碳很可能源于陆地原环境,通过侵蚀和地下水运输.
- 这种水中二氧化碳的流量表明,目前对北极陆地碳汇的估计可能高达20%的高估.
结论:
- 北极水生生态系统是大气二氧化碳的重要来源,而不是沉.
- 北极原的陆地碳汇估计需要修订,以包括水生系统的贡献.
- 要了解北极碳循环的全部过程,就必须考虑陆地和水域的碳流.
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