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首页> 外文期刊>Journal of applied geodesy >A Spatial Analysis of GEOID03 and GEOID09 in Connecticut
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A Spatial Analysis of GEOID03 and GEOID09 in Connecticut

机译:康涅狄格州的GEOID03和GEOID09空间分析

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摘要

The National Geodetic Survey (NGS) recommends using a hybrid geoid model to derive orthometric heights from ellipsoid heights. The accuracy of GE0ID03 and GE0ID09 were assessed independently in Connecticut. The present research analyses the spatial behavior of residuals derived from the comparison of differential levelled NAVD 88 orthometric heights and GPS-derived orthometric heights (using GEOID03 & GEOID09) at 72 benchmarks in Connecticut. Both geometrical and geosta-tistical analyses were performed on the residuals. A planar regression model indicates a weak spatial relation for residuals derived from GEOID03. This weakness was not noted in the analysis of residuals derived from GEOID09. Results of a four-parameter regression model does not indicate any need for a correction surface. A kriging surface was created with a fitted spherical semivariogram model and suggests GEOID09 captures more spatial variability of geoid undulation than GEOID03 in Connecticut.
机译:美国国家大地测量局(NGS)建议使用混合大地水准面模型从椭球高度中得出正高。在康涅狄格州独立评估了GE0ID03和GE0ID09的准确性。本研究分析了康涅狄格州72个基准点的差分水平NAVD 88正交高度与GPS衍生的正交高度(使用GEOID03和GEOID09)的比较得出的残差的空间行为。对残差进行了几何和地质统计分析。平面回归模型表明派生自GEOID03的残差的空间关系很弱。分析来自GEOID09的残差时未注意到此弱点。四参数回归模型的结果并不表示需要任何校正表面。使用拟合的球面半变异函数模型创建了克里金表面,这表明与康涅狄格州的GEOID03相比,GEOID09捕获的大地水准面波动的空间变异性更大。

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