海洋最大缺氧区域的十年振荡
N N Duprey1, A D Foreman1, J D Carriquiry2
1Max Planck Institute for Chemistry (Otto Hahn Institute), Mainz, Germany.
概括
海洋变暖影响缺氧区域 (ODZ). 珊瑚同位素揭示了东部热带北太平洋脱的十年变化,与太平洋十年变化有关,而不仅仅是长期的全球变暖趋势.
科学领域:
- 海洋化学
- 古代海洋学
- 气候科学
背景情况:
- 由于历史数据有限,对缺氧区域 (ODZ) 的海洋变暖影响尚不清楚.
- 了解过去的ODZ变化对于预测未来的海洋脱氧至关重要.
研究的目的:
- 在东部热带北太平洋 (ETNP) ODZ重建过去的脱.
- 研究十年气候变化对ODZ动态的影响.
主要方法:
- 使用珊瑚骨架结合的同位素 (CS-δ15N) 进行月度解析记录.
- 分析了来自ETNP的80年时间序列.
主要成果:
- 在ETNP脱和缺氧方面观察到显著的十年变化.
- 在太平洋十年变化的凉爽阶段化达到顶峰.
- 在这些阶段更强的上升可能会增加生产力和氧气需求.
结论:
- 十年间的变化,特别是太平洋十年间的变化,对ETNP ODZ的动态有很大影响.
- 之前的ODZ长期趋势评估可能因十年性波动而有偏差.
- 未来的ODZ演变取决于全球变暖和十年气候模式之间的相互作用.
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