日间长度十年内变化的表征和含义
1School of Environmental Sciences, University of Liverpool, Liverpool L69 3GP, UK. holme@liv.ac.uk
Nature
|July 13, 2013
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 地力学是什么?地力学是什么?
背景情况:
- 地球的旋转因外部扭矩和内部角运动量交换而变化.
- 大气层主导短期变化,而地幔核心交换影响了十年变化.
- 地球自转的十年内变化是复杂的,不太了解.
研究的目的:
- 为了澄清驱动地球旋转在十年内时间尺度上的非潮变化的组成部分.
- 为了研究日长变化和地磁震动之间的关系.
- 为了限制下层地幔的电导率和组成.
主要方法:
- 在时间域中分析地球的旋转 (一天的长度),而不是频率域.
- 非大气角度运动量交换的分解成不同的组成部分.
- 一天长度变化与地磁震事件的相关性.
主要成果:
- 地球旋转变化的非大气组成部分被分为三个不同的信号:十年趋势,5.9年振荡和与地磁震动同步跳跃.
- 这些日长跳跃的性质为导致地磁震动的现象提供了新的见解.
- 这些发现对下层地幔的电导率施加了显著的约束.
结论:
- 地磁冲动与地球自转中的特定,可识别的跳跃有关.
- 这项研究为了解下层地幔电导率,结构和组成提供了关键的约束.
- 时间域分析为地球的旋转动力学和核心-地幔相互作用提供了更清晰的图像.
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