南极环极电流在过去一百万年中的强度在区域不对称的变化
Shuzhuang Wu1,2, Alain Mazaud3, Elisabeth Michel3
1Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland.
概括
南极环极流 (ACC) 在过去一百万年里,在南大洋的强度变化不均. 这些由各种因素影响的动态,可以提供对未来气候变化影响的见解.
科学领域:
- 古代海洋学 古代海洋学 古代海洋学
- 气候科学 气候科学
- 南大洋动力学 南大洋动力学
背景情况:
- 南极环极流 (ACC) 对全球海洋循环,气候调节和南极冰盖稳定性至关重要.
- 了解ACC过去的变异性,特别是普世时期的变异性,至关重要,但仍然受到很小的限制.
- ACC的轨道尺度动态显著影响全球气候模式.
研究的目的:
- 为了重建过去一百万年来ACC的流速变化.
- 为了研究在世时期的ACC的时空变化.
- 了解ACC变化的驱动因素及其对过去和未来气候的影响.
主要方法:
- 来自南洋印度部门的沉积物核心的分析.
- 使用午线截面重建ACC流速.
- 检查轨道时间尺度 (过去100万年).
主要成果:
- 在南大洋中观察到ACC强度的区域不对称变化.
- 在南印度洋,ACC加剧,而在南太平洋,在冰川/低斜率时期,ACC减弱.
- 相反的模式发生在冰川间/高斜率时期,表明反相动态.
结论:
- ACC的动态受 bathymetry,南半球西风,海冰范围,浮力强迫和电流汇合的影响.
- 这些不对称和反相的ACC动态在温暖的普莱斯托时代间隔中持续存在.
- 在温暖时期的过去ACC行为可能作为未来人类变暖场景的有限模拟.
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