北极海洋的阿拉贡石不和:海洋酸化和海冰融化的影响
Michiyo Yamamoto-Kawai1, Fiona A McLaughlin, Eddy C Carmack
1Department of Fisheries and Oceans, Institute of Ocean Sciences, 9860 West Saanich Road, Sidney, British Columbia V8L 4B2, Canada. michiyo.kawai@dfo-mpo.gc.ca
概括
由于二氧化碳排放量增加和海冰融化,北冰洋水域的碳酸含量越来越低. 这种酸化威胁到海洋生物,影响整个北极生态系统.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋生物学 海洋生物学
- 气候科学 气候科学
背景情况:
- 人为二氧化碳排放量的增加正在推动海洋酸化.
- 北极海冰融化正在改变海洋化学和循环模式.
研究的目的:
- 调查海洋酸化和海冰融化对加拿大盆地碳酸和度状态的影响.
- 评估这些变化对北极海洋生态系统的影响.
主要方法:
- 在加拿大盆地地表水化学分析.
- 评估海冰面积与阿拉贡石和度状态之间的关系.
主要成果:
- 2008年,加拿大盆地的地表水被发现在阿拉贡石方面不和.
- 广泛的海冰融化被确定为这种低和的主要原因.
- 退缩的海冰增加了低和地下水的上游到大陆架上.
结论:
- 海洋酸化和海冰融化在北冰洋中造成了不和的条件.
- 这些变化对化浮游生物和无脊椎动物构成重大威胁.
- 北极生态系统的组成很可能会因这些持续的环境变化而改变.
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