内部水域的全球二氧化碳排放来自内陆水域
Peter A Raymond1, Jens Hartmann, Ronny Lauerwald
1Yale School of Forestry and Environmental Studies, 195 Prospect Street, New Haven, Connecticut 06511, USA.
Nature
|November 22, 2013
概括
全球从内陆水域逃逸的二氧化碳 (CO2) 比以前估计的要高. 这项研究揭示了显著的区域差异,并确定了来自河流和溪流的二氧化碳流的热点.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 气候科学 气候科学
背景情况:
- 从内陆水域逃逸的二氧化碳 (CO2) 是全球碳循环的关键但量化不足的组成部分.
- 以前的全球估计受到表面积,气体转移速度和全面的二氧化碳数据库缺乏标准化的框架的限制.
研究的目的:
- 建立一个全球框架来估计内陆水域的二氧化碳逃逸.
- 分析内陆水面积,溶解的二氧化碳和气体转移速度的区域变化.
- 为提供最新的全球二氧化碳逃逸率.
主要方法:
- 开发一个框架来估计内陆水面积和气体转移速度.
- 为内陆水域编制全球二氧化碳数据库.
- 从溪流,河流,湖泊和水库中脱离二氧化碳的区域分析.
主要成果:
- 全球二氧化碳逃逸率估计为每年从溪流/河流流出1.8 Pg C,从湖泊/水库出0.32 Pg C.
- 全球总二氧化碳逃逸率为每年2.1 Pg C,高于之前的估计,这是由于河流流量增加所致.
- 确定全球热点的溪流和河流二氧化碳逃逸,70%的流量来自陆地表面的20%.
结论:
- 从内陆水域的全球二氧化碳逃逸是相当大且被低估的碳流.
- 在二氧化碳逃逸方面存在显著的区域差异,河流系统中集中了"热点".
- 需要进一步的研究,以阐明推动全球内陆水域二氧化碳逃逸的来源和机制.
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