区域触发的地磁逆转是由区域触发的地磁逆转
Filipe Terra-Nova1, Hagay Amit2
1Nantes Université, Univ Angers, Le Mans Université, CNRS, Laboratoire de Planétologie et Géosciences, LPG UMR 6112, 44000, Nantes, France. filipe.terranova@univ-nantes.fr.
Scientific reports
|April 26, 2024
概括
地磁场逆转与核心-地幔边界的热流变化有关. 增加的热流异质性通过增强数值动力模的惯性力来驱动反转.
科学领域:
- 地质物理学 地质物理学
- 计算物理学的计算物理.
- 地球科学 地球科学
背景情况:
- 数字动力模拟将场逆转与强烈的惯性效应联系起来.
- 在理论上,惯性力在地球外核动力学中是次要的.
研究的目的:
- 研究不同质的核心-地幔边界热流对地磁反转的作用.
- 将数值发现与对惯力力重要性的理论预期相协调.
主要方法:
- 使用了数值动力模拟器.
- 从地震数据推断的内置异质外界热量流.
- 分析了不同热流异质幅度的影响.
主要成果:
- 地磁逆转随着热流异质性的增加而发生.
- 逆转在高热量流区域和强大的小规模惯性力中被触发.
- 增加的异质性导致亚阴性状况抑制逆转.
结论:
- 核心-地幔边界的异质热流可以驱动地磁反转.
- 这使得模拟中的惯性需要与其在理论中的次要作用相协调.
- 地力发电机的行为表现出对热流异质性的非单调反应.
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