通过卫星高度计检测到的潮标参考水平的抵消:十个案例研究
R D Ray1, M J Widlansky2, A S Genz3
1NASA Goddard Space Flight Center, Greenbelt, MD USA.
概括
卫星高度计和潮计可以检测小型垂直陆地运动 (VLM) 和数据错误. 将这些海平面测量结果进行比较有助于确保数据的准确性,特别是对于岛屿的潮计.
科学领域:
- 地质测量是指地质测量.
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 海平面测量对于了解气候变化至关重要.
- 卫星高度计和潮计提供了补充数据.
- 潮表的稳定性对于准确的相对海平面记录至关重要.
研究的目的:
- 评估卫星高度计对于潮计质量控制的实用性.
- 为了检测潮尺测量中的小,不连续的垂直偏移.
- 在潮表位置确定垂直陆地运动 (VLM).
主要方法:
- 从卫星高度测量的绝对海平面数据与来自潮表的相对海平面数据的比较.
- 分析了十个可能经历垂直偏移的潮计案例研究.
- 使用来自地标站的独立VLM测量进行验证.
主要成果:
- 检测到潮仪中的小 (<1-2厘米) 不连续的垂直偏移.
- 卫星高度计在潮计质量控制方面被证明是有效的.
- 开放海洋岛屿的潮计为VLM检测提供了更清晰的信号.
结论:
- 卫星高度计是识别潮计数据错误的宝贵工具.
- 通过结合卫星和潮计数据,可以确定VLM.
- 精确的海平面上升监测需要强大的潮表稳定性和数据验证.
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