格雷斯 (GRACE) 的重力数据限制了洛伦西亚上空的古老冰层几何和大陆动态
M E Tamisiea1, J X Mitrovica, J L Davis
1Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Mail Stop 42, Cambridge, MA 02143, USA. mtamisiea@cfa.harvard.edu
重力恢复和气候实验 (GRACE) 卫星数据揭示了加拿大的冰川静态调整 (GIA) 和冰盖结构. 这种GIA模型提供了关于大陆地质层浮力的关键数据.
科学领域:
- 地质物理学 地质物理学
- 卫星地质测量 卫星地质测
- 冰川学的冰川学
背景情况:
- 了解冰川静态调整 (GIA) 对于解释地球的重力场至关重要.
- 以前对劳伦西亚冰层复合物的重建缺乏明确的证据.
- GIA对大陆构造层的影响需要精确的建模.
研究的目的:
- 用GRACE卫星数据隔离和分析GIA在加拿大的重力信号.
- 为了确定古老的劳伦斯海冰综合体的结构.
- 为了限制地幔对流和大陆地板层浮力模型.
主要方法:
- 来自GRACE卫星任务数据的自由空气重力趋势的分析.
- 观察到的重力场与冰川静态调整 (GIA) 模型的比较.
- 峰值GIA速率与观察到的静态重力场的调和.
主要成果:
- 格雷斯数据强大地将GIA重力信号与地幔对流隔离起来.
- 证据支持劳伦西亚冰层复合体,其中有两个大圆顶,位于哈德逊湾的西和东.
- GIA模型占观察到的静态重力场的25-45%.
结论:
- GRACE数据提供了GIA和劳伦斯冰盖配置的清晰图像.
- 这些发现为了解大陆地质层浮力提供了关键的边界条件.
- 这项研究完善了冰川后反弹和地幔动态的地球物理模型.
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