首页|美国NAVD88高程基准与全球高程基准之间的垂直偏差

美国NAVD88高程基准与全球高程基准之间的垂直偏差

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随着空间探测技术的发展,利用地球重力场模型实现全球高程基准统一成为一种有效的方法.本文联合EGM2008、EIGEN-6C4 超高阶地球重力场模型和美国范围内36 578 个GNSS/水准点,基于重力位差法确定NAVD88 高程基准相对于全球高程基准的垂直偏差.首先通过最新发布的CRUST 1.0 地壳密度模型确定美国区域地壳密度,较通常假设地壳密度均匀分布更贴合实际情况;然后根据GNSS/水准点至水准原点的距离划分阈值,实验结果表明阈值取 3 000 km计算结果的标准差达到最小;最后利用最小二乘法对垂直偏差结果进行优化改善,求出美国高程基准NAVD88 相对于全球高程基准的垂直偏差为-0.956 6 m.
The Vertical Shift between North American Vertical Datum of 1988 and Global Vertical Datum
With the development of space exploration technology,it becomes an effective method to unify global vertical datum by using earth gravity field model.In this paper,the vertical shift between NAVD88 datum and global vertical datum is determined by combining the EGM2008,EIGEN-6C4 ultra-high-degree gravity models and 36 578 GNSS/leveling points in the United States by using the potential difference approach.First,CRUST 1.0,the latest crustal density model,is used to determine the regional crustal density of the United States,which is more realistic to the actual situation than the common assumption of the evenly distributed crustal densities.Then the thresholds are divided according to the distance between GNSS/leveling point and leveling origin.The experi-mental results show that the standard deviation of the vertical shift reached the minimum when the threshold is set at 3 000 km.Finally,the least square method is used to optimize and improve the vertical shift results,and the vertical shift between NAVD88 and global vertical datum is calculated to be -0.956 6 m.

vertical datumCRUST 1.0 modelNorth American Vertical Datum of 1988(NAVD88)vertical shiftGNSS/leveling

刘鑫宇、李姗姗、单建晨、范雕、黄炎、王傲明

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75841部队,湖南 长沙 410000

信息工程大学,河南 郑州 450001

高程基准 CRUST 1.0模型 美国高程基准NAVD88 垂直偏差 GNSS/水准

2024

测绘科学技术学报
信息工程大学科研部

测绘科学技术学报

影响因子:0.594
ISSN:1673-6338
年,卷(期):2024.40(6)