自1998年以来,在陆地系统中检测到大规模的质量再分配
Christopher M Cox1, Benjamin F Chao
1Raytheon Information Technology and Scientific Services (ITSS), Space Geodesy Branch, NASA Goddard Space Flight Center, Code 926, Greenbelt, MD 20771, USA.
概括
地球的平坦度 (J2) 意外地在1998年左右从下降转变为增加. 这种由不确定的地质物理原因驱动的全球质量分布的变化,现在掩盖了冰期后反弹的影响.
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
- 地质测量是指地质测量.
背景情况:
- 地球的动态平坦度 (J2) 显示了25年的下降趋势,这是由于后冰期的反弹.
- 大约在1998年,人们观察到J2增长趋势的突然逆转.
- 最近这种增长的地质物理驱动因素仍然不确定.
研究的目的:
- 分析地球平度 (J2) 趋势的变化.
- 调查全球质量分布变化的影响.
- 了解所观察到的J2增长背后的地质物理原因.
主要方法:
- 过去25年来太空地质观测的分析.
- 地理物理建模以评估质量再分配.
- 来自不同来源的J2效应的比较.
主要成果:
- 观察到1998年左右的J2趋势出现了显著的逆转.
- 目前的J2增长趋势主要是由全球质量分布的变化驱动的.
- 来自当前质量再分配的J2效应的大小明显超过了来自地幔反弹的影响.
结论:
- 最近地球平坦度的增加 (J2) 表明全球质量分布的实质性变化.
- 这种转变的地质物理原因需要进一步调查.
- 当前质量再分配对J2的影响比后冰期反弹更为主导.
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