北大西洋碳汇的年间变化
Nicolas Gruber1, Charles D Keeling, Nicholas R Bates
1Institute of Geophysics and Planetary Physics and Department of Atmospheric Sciences, University of California, Los Angeles, CA 90095, USA. ngruber@igpp.ucla.edu
概括
北大西洋的北大西洋.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 碳循环研究 碳循环研究
背景情况:
- 北大西洋是大气中二氧化碳的重要海洋沉点.
- 这种碳汇的时间变化不太清楚.
- 了解碳汇对于减缓气候变化至关重要.
研究的目的:
- 为了研究北大西洋海洋碳汇的时间变化.
- 确定海洋上层碳变化的关键驱动因素.
- 评估观察到的变异性对盆地范围的潜在影响.
主要方法:
- 对上海无机碳观测18年时间序列的分析.
- 利用来自百慕大附近西北亚热带北大西洋的数据.
- 与冬季混合层深度和海面温度异常相关联的碳变化.
主要成果:
- 在北大西洋碳汇中观察到相当大的年比年变化.
- 确定了冬季混合层深度和海面温度异常作为主要驱动因素.
- 变化表现出一个与北大西洋振荡 (NAO) 相关的盆地范围的模式.
结论:
- 北大西洋碳汇的强度显示出显著的时间变化.
- 北大西洋振荡 (NAO) 可能协调了整个盆地的这种变化.
- 碳汇强度的估计变化大约为每年+/-0.3倍克的碳,几乎是+/-50%.
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