在地球系统中测量质量变化的GRACE测量
Byron D Tapley1, Srinivas Bettadpur, John C Ries
1Center for Space Research, University of Texas, Austin, TX 78712, USA.
概括
重力恢复和气候实验 (GRACE) 卫星提供精确的每月地质高度测量. 这些观测揭示了南美洲的季节性水质变化,有助于水文研究.
科学领域:
- 地质测量是指地质测量.
- 水文学的水文学
- 气候科学 气候科学
背景情况:
- 双重重力恢复和气候实验 (GRACE) 卫星提供每月重力场估计.
- 这些估计可以在400公里的空间分辨率下实现高地理高度精度 (2-3毫米).
研究的目的:
- 分析年度地形变化及其与水文过程的相关性.
- 为了区分亚马逊流域和邻近较小的流域之间的水文信号.
主要方法:
- 利用来自GRACE卫星的每月重力场数据.
- 分析地形高度变化及其季节性模式.
- 通过比较南美不同流域的水文信号.
主要成果:
- 观测到的年度地质变化高达10毫米,在春季和秋季达到顶峰.
- 将南美洲的显著地质变化归因于表面和地下水的变化.
- 在亚马逊和北方流域之间的水文信号中显示出明显的区别.
结论:
- GRACE卫星数据有效地捕捉了大规模的水文变化.
- 这些发现使得当地水文过程与区域和全球规模的联系成为可能.
- 这项研究增强了我们对南美洲水质动态的理解.
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