Ailé Selenne Golin, Hugo Ramiro Páez Campos, Cristian Guevara Ochoa, Claudia Fernanda Dávila, Luis Sebastián Vives
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Statistical metrics were calculated for (i) residuals between DEMs and the Ice, Cloud and Land Elevation Satellite-2 (ICESat-2); (ii) the minimum distance between DEM-derived drainage networks and those from the Buenos Aires Provincial Water Authority; and (iii) DEM-derived slopes in shallow water bodies compared with the Joint Research Centre's Global Surface Water Mapping product. Analyses were performed for four elevation and seven slope bands. TanDEM-X had the smallest errors compared to ICESat-2 (median 0.19 m, NMAD 0.38 m), followed by FABDEM (median 0.31 m, NMAD 0.23 m). EDEM performed best in drainage networks (median 99.45 m, NMAD 117.16 m), followed by FABDEM. In general, the vertical error increased with elevation and the accuracy of the drainage network estimates improved. The vertical accuracy decreased with steeper slopes, with FABDEM performing the best across all slope ranges. FABDEM exhibited the best performance in determining seasonally dispersed shallow water bodies, demonstrating its overall usefulness for hydrological applications in large-scale plains characterized by aeolian geoforms of lowland accumulation and erosion. 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引用次数: 0
摘要
本研究评估了阿根廷查科-潘潘亚平原Del Azul Creek盆地的六种开放获取数字高程模型(DEM):航天飞机雷达地形任务、先进陆地观测卫星相相阵l波段合成孔径雷达、TerraSAR-X数字高程测量附加组件(TanDEM-X)、NASADEM全球DEM、森林和建筑物高度偏差从哥白尼GLO 30 DEM V1-0 (FABDEM)和TanDEM-X 30 m编辑DEM (EDEM)中去除。计算了dem与冰、云和陆地高程卫星-2 (ICESat-2)之间的残差的统计度量;(ii)来自dem的排水网络与来自布宜诺斯艾利斯省水务局的排水网络之间的最小距离;(三)与联合研究中心的全球地表水制图产品比较浅水水体dem计算的坡度。对四个高程带和七个坡度带进行了分析。与ICESat-2相比,TanDEM-X误差最小(中值0.19 m, NMAD 0.38 m),其次是FABDEM(中值0.31 m, NMAD 0.23 m), EDEM在排水网络中表现最佳(中值99.45 m, NMAD 117.16 m),其次是FABDEM。总体上,垂直误差随海拔升高而增大,水系网估算精度提高。垂直精度随坡度的增大而降低,在所有坡度范围内,FABDEM的表现最好。FABDEM在确定季节性分散的浅水水体方面表现最好,表明其在以低地堆积和侵蚀的风成地貌为特征的大尺度平原上的水文应用总体上是有用的。评估免费提供的产品为研究人员和专业人员提供了宝贵的资源,并可以指导管理水文资源的决策,包括洪水风险和基础设施发展。
Assessing open-access digital elevation models for hydrological applications in a large scale plain: Drainage networks, shallow water bodies and vertical accuracy
This study evaluated six open-access digital elevation models (DEMs) for the Del Azul Creek Basin in the Argentine Chaco-Pampean Plain: Shuttle Radar Topography Mission, Advanced Land Observing Satellite Phased Array L-Band Synthetic Aperture Radar, TerraSAR-X Add-On for Digital Elevation Measurements (TanDEM-X), NASADEM Global DEM, Forest and Building height biases were removed from Copernicus GLO 30 DEM V1-0 (FABDEM), and TanDEM-X 30 m Edited DEM (EDEM). Statistical metrics were calculated for (i) residuals between DEMs and the Ice, Cloud and Land Elevation Satellite-2 (ICESat-2); (ii) the minimum distance between DEM-derived drainage networks and those from the Buenos Aires Provincial Water Authority; and (iii) DEM-derived slopes in shallow water bodies compared with the Joint Research Centre's Global Surface Water Mapping product. Analyses were performed for four elevation and seven slope bands. TanDEM-X had the smallest errors compared to ICESat-2 (median 0.19 m, NMAD 0.38 m), followed by FABDEM (median 0.31 m, NMAD 0.23 m). EDEM performed best in drainage networks (median 99.45 m, NMAD 117.16 m), followed by FABDEM. In general, the vertical error increased with elevation and the accuracy of the drainage network estimates improved. The vertical accuracy decreased with steeper slopes, with FABDEM performing the best across all slope ranges. FABDEM exhibited the best performance in determining seasonally dispersed shallow water bodies, demonstrating its overall usefulness for hydrological applications in large-scale plains characterized by aeolian geoforms of lowland accumulation and erosion. Assessing freely available products provides valuable resources for researchers and professionals and can guide decision making for managing hydrological resources, including flood risk and infrastructure development.
期刊介绍:
Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with:
the interactions between surface processes and landforms and landscapes;
that lead to physical, chemical and biological changes; and which in turn create;
current landscapes and the geological record of past landscapes.
Its focus is core to both physical geographical and geological communities, and also the wider geosciences