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太平洋翻转循环的重新组织,在整个米奥生气候最佳时期
Ann Holbourn1, Wolfgang Kuhnt2, Denise K Kulhanek2
1Institute of Geosciences, Christian-Albrechts-University, D-24118, Kiel, Germany. ann.holbourn@ifg.uni-kiel.de.
Nature communications
|September 17, 2024
概括
海洋翻转的循环转移是由全球变暖和冷却事件驱动的. 南极冰盖和高度的气候变化影响了米奥世时期的深水出口和太平洋循环模式.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 海洋翻转循环对全球变暖的反应受到辩论.
- 了解过去的循环变化可以为未来的气候预测提供信息.
研究的目的:
- 在米奥生气候最佳期 (MCO) 和中米奥生气候过渡期 (MMCT) 期间调查深水循环.
- 分析高度气候和南极冰盖对海洋循环的影响.
主要方法:
- 来自西赤道太平洋 (国际海洋发现计划站点U1490) 的综合多代理记录.
- 综合了来自太平洋,南洋和印度洋的已公布数据.
主要成果:
- 南方来源深水的北方出口与南极冰盖相关.
- 在MCO期间的全球变暖降低了碳酸离子度和增加了分层,将翻转转移到更深的水域.
- 海底鱼类的生产力弥补了西赤道太平洋的溶解,在16亿年后,碳酸盐积累率上升了.
- 在MMCT期间的冷却改善了碳酸盐的保存,并启动了现代太平洋翻转循环.
结论:
- 度热梯度,南洋风应力和分层变化在MCO和MMCT期间驱动了不同的深水形成模式.
- 海洋循环对气候变化和冰盖变化的敏感.
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