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调和南大洋前沿的赤道向上的迁移与小的南极冰的体积变化在米奥生冷却期间的冰冷
Suning Hou1, Lennert B Stap2, Ryan Paul3
1Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands. s.hou@uu.nl.
Nature communications
|November 9, 2023
概括
苗代气候冷却并没有增加南极冰的数量. 相反,南极冰盖降低并向海扩展,挑战了以前对冰 - 海洋 - 气候相互作用的理解.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 冰川学的冰川学
背景情况:
- 苗代气候冷却和二氧化碳减少传统上与南极冰川扩张有关.
- 最近的研究挑战了这个范式,显示在这段时间内冰块体积没有大幅增加.
研究的目的:
- 调查米奥森冰洋气候相互作用.
- 重建亚热带前线迁移,海洋温度和全球冰体积.
- 调和关于气候冷却而没有冰川膨胀的反直觉发现.
主要方法:
- 使用多个代理重建使用dinoflagellate囊和底形形块化同位素.
- 分析了来自塔斯马尼亚海域的数据.
- 冰盖建模包括降水和冰洋动态.
主要成果:
- 向赤道的迁移和亚热带阵线的加强.
- 观察到同时发生的表面和深海冷却.
- 缺少显著的全球冰的体积变化在中后期的米奥纪.
结论:
- 南极冰盖的高度下降,同时向海扩大,以保持稳定的体积.
- 这种动态可以通过特定的降水模式和冰引起的海洋冷却来实现.
- 需要重新思考米奥世时期的冰 - 海洋 - 气候相互作用.
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