海冰通过调节冬季分层来控制海洋净二氧化碳的吸收
Elise S Droste1,2,3, Dorothee C E Bakker1, Hugh J Venables4
1School of Environmental Sciences, University of East Anglia, Norwich, UK.
概括
南大洋的二氧化碳吸收因季节而异. 冬季的海冰持续时间控制了海洋分层,影响了20%的碳吸收,并影响了海洋的碳沉积.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋化学 海洋化学
- 气候科学 气候科学
背景情况:
- 南大洋呈现季节性二氧化碳交换,夏季的吸收被冬季的排气抵消.
- 海冰的动态显著影响了这种平衡,导致南大洋碳汇的跨年变化.
研究的目的:
- 为了研究海水二氧化碳流失的跨年变化的驱动因素.
- 量化海冰状况对南大洋碳汇的影响.
主要方法:
- 利用了十年 (2010-2020年) 的全年海洋碳酸盐化学数据.
- 分析了西南极半岛罗瑟拉时间序列的数据.
主要成果:
- 海水二氧化碳流动性的年间变化与冬季过程有关.
- 那些海冰持续时间较长和冬季分层增加的年份,吸收的二氧化碳增加了约20%.
- 受到海冰影响的海洋分层,控制了进入富含碳的海洋内部的途径.
结论:
- 冬季的海洋观测对于了解海空二氧化碳流动至关重要.
- 海冰的持续时间是调节南大洋碳沉积能力的关键因素.
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