首页> 外文会议>ISPRS Congress >VALIDATION OF THE ASTER GLOBAL DIGITAL ELEVATION MODEL VERSION 3 OVER THE CONTERMINOUS UNITED STATES
【24h】

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

机译:验证雅斯特全球数字高程模型版本3在孔雀石美国

获取原文

摘要

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)的验证。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地面控制点来计算GDEM V3的垂直准确度。测量的GDEM V3测量的根均方误差(RMSE)为8.52米。这与GDEM V2的RMSE相比。垂直精度的另一个重要描述符是平均误差或偏置,指示DEM是否具有从真实地面级别的整体垂直偏移量。 GDEM V3平均误差为-1.20米反映了GDEM V3中的整体负偏差。绝对垂直精度评估结果,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,在存在内置或自然的地上特征的区域中,GDEM V3测量了地面上方的高度,在先前的GDEM版本(V1和V2)的评估中指出的条件和给定立体光学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的凸起高于冠层高于SRTM。整体验证努力还包括对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。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号