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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >A new, high-resolution digital elevation model of Greenland fully validated with airborne laser altimeter data
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A new, high-resolution digital elevation model of Greenland fully validated with airborne laser altimeter data

机译:格陵兰岛的新型高分辨率数字高程模型已通过机载激光高度计数据充分验证

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摘要

A new digital elevation model of the Greenland ice sheet and surrounding rock outcrops has been produced at 1-km postings from a comprehensive suite of satellite remote sensing and cartographic data sets. Height data over the ice sheet were mainly from ERS-1 and Geosat radar altimetry. These data were corrected for a slope-dependent bias that had been identified in a previous study. The radar altimetry was supplemented with stereophotogrammetric data sets, synthetic aperture radar interferometry, and digitized cartographic maps over regions of bare rock and where gaps in the satellite altimeter coverage existed. The data were interpolated onto a regular grid with a spacing of similar to1 km. The accuracy of the resultant digital elevation model over the ice sheet was assessed using independent and spatially extensive measurements from an airborne laser altimeter that had an accuracy of between 10 and 12 cm. In a comparison with the laser altimetry the digital elevation model was found to have a slope-dependent accuracy ranging from -1.04 +/-1.98 m to -0.06 +/- 14.33 m over the ice sheet for a slope range of 0.0-1.0 degrees. The mean accuracy over the whole ice sheet was -0.33 +/-6.97 m. Over the bare rock areas the accuracy ranged from 20 to 200 m, dependent on the data source available. The new digital elevation model was used as an input data set for a positive degree day model of ablation. The new elevation model was found to reduce ablation by only 2% compared with using an older, 2.5-km resolution model, which suggests that resolution-induced errors in estimating ablation are no longer important. [References: 36]
机译:一套全面的卫星遥感和制图数据集以1公里的发布距离产生了格陵兰冰盖和周围岩石露头的新数字高程模型。冰盖上的高度数据主要来自ERS-1和Geosat雷达测高仪。这些数据已针对先前研究中确定的斜率依赖性偏差进行了校正。雷达测高仪还补充了立体摄影测量数据集,合成孔径雷达干涉测量法以及裸岩区域以及卫星高度计覆盖范围内存在空白的数字化地图。将数据插值到规则网格中,间距大约为1 km。使用来自机载激光测高仪的独立且空间上广泛的测量值(其精度在10到12厘米之间)评估了冰盖上所得数字高程模型的精度。在与激光测高仪的比较中,在0.0-1.0度的坡度范围内,数字高程模型在冰面上的坡度相关精度为-1.04 +/- 1.98 m至-0.06 +/- 14.33 m 。整个冰盖的平均精度为-0.33 +/- 6.97 m。在裸露的岩石区域,精度取决于可用的数据源,范围为20至200 m。新的数字高程模型用作消融正度日模型的输入数据集。与使用旧的2.5 km分辨率模型相比,发现新的高程模型只能将消融减少2%,这表明在估计消融时分辨率引起的误差不再重要。 [参考:36]

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