在普莱斯托时代的冰川时期,加剧了太平洋深层的进入和通风
I R Hall1, I N McCave, N J Shackleton
1Department of Earth Sciences, Cardiff University, PO Box 914, Cardiff CF10 3YE, UK. Hall@cardiff.ac.uk
Nature
|August 24, 2001
概括
南大洋的深水产量对地球的热量预算产生了重大影响. 冰川时期看到太平洋深层的涌入加剧,可能是由于南极底部水形成的增加.
科学领域:
- * 古海洋学 古代海洋学
- * 气候科学 气候科学
- * 南洋动力学公司
背景情况:
- * 南洋深水产量影响全球热量分布.
- * 太平洋的深水供应主要来自新西兰东部的西部边界深流.
研究的目的:
- *重建平纪时期太平洋的深水特性和流速变化.
- * 调查太平洋深层流入和南极地底水产量之间的关系.
主要方法:
- *对沉积物核心的分析受到深度西部边界电流的影响.
- * 应用物理和同位素代理来重建过去的深水条件.
主要成果:
- * 证据表明,在过去120万年的冰川时期,太平洋深海的进入和通风加剧了.
- * 观察到的深水流量变化与冰川时期南极地底水产量的增加有关.
- * 在普莱斯托时代中期气候过渡 (0.860.45万年前) 期间发现的全球热环流中的重大扰动.
结论:
- *在冰川时期加剧的太平洋深海流入可能是由南洋风力增加或海冰形成所驱动的.
- *南极地底水的生产是调节深太平洋循环的关键因素.
- * 普莱斯托时代中期的气候转变标志着全球海洋循环模式的重大转变.
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