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Resurrection of Dormant Daphnia magna: Protocol and Applications
Published on: January 19, 2018
大西洋翻转对晚期普莱斯托纪气候强迫的反应
Lorraine E Lisiecki1, Maureen E Raymo, William B Curry
1Department of Earth Sciences, Boston University, 675 Commonwealth Avenue, Boston, Massachusetts 02215, USA. lisiecki@alumni.brown.edu
Nature
|November 7, 2008
概括
冰川时期的海洋循环变化是复杂的. 新的研究表明,大西洋翻转是敏感的多个因素超越米兰科维奇强迫,影响气候模型.
科学领域:
- 古海洋学是古海洋学.
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 该SPECMAP项目假设高度夏季阳光照射 (米兰科维奇强迫) 驱动海洋循环和气候反应跨轨道周期.
- 之前对海洋循环对轨道强迫反应的分析仅限于几个大西洋地点,并没有完全捕捉特定地点的相位变化.
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