关于"海底浴度对中海岩供应气候驱动的波动的敏感性"的评论
1Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.
概括
海洋底层的米兰科维奇循环得到了新发现的支持. 南东太平洋上升被认为是检测这些地质信号的最佳位置.
科学领域:
- 地质学
- 海洋学
- 气候科学
背景情况:
- 最近的研究报告发现了海底浴度数据中的米兰科维奇周期.
- 有关Olive等初步发现的担忧和批评. 和戈夫.
研究的目的:
- 为了解决有关海底浴度的米兰科维奇周期的问题.
- 评估东南太平洋上升作为观察这些周期的关键区域.
主要方法:
- 分析海底水位数据.
- 观察数据与预测模型的比较.
主要成果:
- 尽管受到批评,但这项研究的结果强化了南东太平洋上升对于米兰科维奇周期检测的重要性.
- 模型与该地区观察到的度数据密切一致.
结论:
- 东南太平洋上升仍然是研究海底地形的米兰科维奇周期的首选地点.
- 这些发现支持海洋地质记录中这些长期气候强迫信号的存在和检测能力.
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