的循环. 的循环. 在亚波克斯海洋中,氧化的快速循环
Andrew R Babbin1, Daniele Bianchi2, Amal Jayakumar3
1Department of Geosciences, Princeton University, Princeton, NJ 08544, USA. Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. babbin@mit.edu.
概括
海洋的氧化 (N2O) 循环比以前想象的要快,尤其是在亚氧化区. 这种由有机碳和氧气水平驱动的快速循环,表明海洋温室气体排放量正在增加.
科学领域:
- 海洋学 海洋学 海洋学
- 大气化学 大气化学
- 生物地质化学生物地质化学
背景情况:
- 氧化 (N2O) 是一种强有力的温室气体和平流层臭氧破坏物质.
- 海洋N2O的来源和沉积点尚未得到充分了解,这阻碍了准确的气候建模.
- 海洋中的suboxic区域是N2O循环的关键,但量化不足的区域.
研究的目的:
- 直接测量东部热带北太平洋地区的N2O减少率.
- 量化N2O在海洋亚箱性区域的循环速率.
- 了解控制N2O循环的因素及其对大气排放的影响.
主要方法:
- 使用稳定同位素标记器直接测量N2O的减少率.
- 在东部热带北太平洋进行测量.
- 分析了与环境因素相关的N2O循环的空间分布.
主要成果:
- 由于不完全的脱化,在亚箱性区域的N2O循环速率比当前模型预测高出一个数量级.
- N2O循环速率显示出对有机碳和溶解氧度的强烈依赖.
- 二氧化碳的流量是大气净流量的20倍,这表明海洋处理的数量很大.
结论:
- 海洋N2O循环在当前的模型中被严重低估,特别是在亚箱性环境中.
- 快速循环和对环境因素的依赖表明,扩大亚箱性区域将增加N2O排放.
- 准确量化海洋N2O流量对于预测未来的气候变化和臭氧层消耗至关重要.
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