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VALIDATION OF THE ASTER GLOBAL DIGITAL ELEVATION MODEL VERSION 3 OVER THE CONTERMINOUS UNITED STATES

机译:验证艾斯特全球数字高程模型版本3在孔雀石美国

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The ASTER Global Digital Elevation Model Version 3 (GDEM v3) was evaluated over the conterminous United States in a manner similar to the validation conducted for the original GDEM Version 1 (v1) in 2009 and GDEM Version 2 (v2) in 2011. The absolute vertical accuracy of GDEM v3 was calculated by comparison with more than 23,000 independent reference geodetic ground control points from the U.S. National Geodetic Survey. The root mean square error (RMSE) measured for GDEM v3 is 8.52 meters. This compares with the RMSE of 8.68 meters for GDEM v2. Another important descriptor of vertical accuracy is the mean error, or bias, which indicates if a DEM has an overall vertical offset from true ground level. The GDEM v3 mean error of -1.20 meters reflects an overall negative bias in GDEM v3. The absolute vertical accuracy assessment results, both mean error and RMSE, were segmented by land cover type to provide insight into how GDEM v3 performs in various land surface conditions. While the RMSE varies little across cover types (6.92 to 9.25 meters), the mean error (bias) does appear to be affected by land cover type, ranging from -2.99 to +4.16 meters across 14 land cover classes. These results indicate that in areas where built or natural aboveground features are present, GDEM v3 is measuring elevations above the ground level, a condition noted in assessments of previous GDEM versions (v1 and v2) and an expected condition given the type of stereo-optical image data collected by ASTER. GDEM v3 was also evaluated by differencing with the Shuttle Radar Topography Mission (SRTM) dataset. In many forested areas, GDEM v3 has elevations that are higher in the canopy than SRTM. The overall validation effort also included an evaluation of the GDEM v3 water mask. In general, the number of distinct water polygons in GDEM v3 is much lower than the number in a reference land cover dataset, but the total areas compare much more closely.
机译:艾斯特全球数字高度模型版本3(GDEM V3)以类似于2009年的原始GDEM版本1(v1)的验证和2011年的GDEM版本2(v2)的方式评估了孔雀石美国。绝对通过与来自美国国家大地测量调查的超过23,000个独立参考大地测量控制点进行计算,计算GDEM V3的垂直准确度。 GDEM V3测量的根均方误差(RMSE)为8.52米。这与GDEM V2的RMSE相比为8.68米。垂直精度的另一个重要描述符是平均误差或偏置,这指示DEM具有从真实地面级别的整体垂直偏移量。 -1.20米的GDEM V3平均误差反映了GDEM V3中的整体负偏差。绝对垂直准确性评估结果,均值误差和RMSE都被陆地覆盖类型分段,以了解GDEM V3如何在各种陆地状况中进行。虽然RMSE在覆盖类型(6.92至9.25米)上变化少,但平均误差(偏差)似乎受到陆地覆盖类型的影响,从-2.99到+4.16米,横跨14个陆地覆盖类别。这些结果表明,在存在的内置或自然的地上特征的区域中,GDEM V3正在测量地面上方的升高,在先前的GDEM版本(V1和V2)的评估中指出的条件和给出了立体声的类型的预期条件艾斯特收集的图像数据。还通过使用梭雷达形貌任务(SRTM)数据集的差异来评估GDEM V3。在许多森林区域中,GDEM V3在冠层中具有比SRTM更高的升高。整体验证工作还包括对GDEM V3水面膜的评估。通常,GDEM V3中的不同水多边形的数量远低于参考陆地覆盖数据集中的数量,但总面积比较得更加密切。

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