与轨道相关的长期气候周期在贝加尔湖的12Myr大陆记录中揭示了
K Kashiwaya1, S Ochiai, H Sakai
1Department of Earth Sciences, Kanazawa University, Kakuma, Japan. kashi@kenroku.kanazawa-u.ac.jp
Nature
|March 10, 2001
概括
贝加尔湖是贝加尔湖的一个.
科学领域:
- 古气候学 古气候学
- 地质地质地质地质地质地
- 气候科学 气候科学
背景情况:
- 陆地气候记录经常与海洋数据保持一致.
- 长期连续的气候记录 (>100万年) 很少.
- 贝加尔湖提供了一个独特的,没有冰的,高沉积率的档案.
研究的目的:
- 为了重建过去1200万年的亚洲大陆内部气候.
- 调查阳光照射和长期环境变化之间的关系.
主要方法:
- 来自贝加尔湖的长沉积物核心的分析.
- 频谱分析以确定周期性模式.
主要成果:
- 观察到亚洲内陆的逐渐冷却趋势.
- 发现了冷却趋势中的波动.
- 频谱分析显示了潜在的米兰科维奇周期 (400,600,1000年).
结论:
- 阳光照射变化对长期的大陆气候产生了重大影响.
- 贝加尔湖为了解过去的气候动态提供了一个至关重要的档案.
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