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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Unmanned Aerial System (UAS) observations of water surface elevation in a small stream: Comparison of radar altimetry, LIDAR and photogrammetry techniques
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Unmanned Aerial System (UAS) observations of water surface elevation in a small stream: Comparison of radar altimetry, LIDAR and photogrammetry techniques

机译:无人机空中系统(UAS)在小型流中观察水面升高:雷达高铁,激光雷达和摄影测量技术的比较

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摘要

Water Surface Elevation (WSE) is an important hydrometric observation, useful to calibrate hydrological models, predict floods, and assess climate change. However, the number of in-situ gauging stations is in decline worldwide. Satellite altimetry, including the recently launched satellite missions (e.g. the radar altimetry missions Cryosat 2, Jason 3, Sentinel 3A/B and the LIDAR mission ICESat-2), can determine WSE only in rivers which are more than ca. 100 m wide. WSE measurements in small streams currently remain limited to the few existing in-situ stations or to time-consuming in-situ surveys. Unmanned Aerial Systems (UAS) can acquire real-time WSE observations during periods of hydrological interest (but with flight limitations in extreme weather conditions), within short survey times and with automatic or semi-automatic flight operations. UAS-borne photogrammetry is a well-known technique that can estimate land elevation with an accuracy as high as a few cm, similarly UAS-borne LIDAR can estimate land elevation but without requiring Ground Control Points (GCPs). However, both techniques face limitations in estimating WSE: water transparency and lack of stable visual key points on the Water Surface (WS) complicate the UAS-borne photogrammetric estimates of WSE, while the LIDAR reflection from the water surface is generally not strong enough to be captured by most of the UAS-borne LIDAR systems currently available on the market. Thus, LIDAR and photogrammetry generally require extraction of the elevation of the "water-edge" points, i.e. points at the interface between land and water, for identifying the WSE. We demonstrate highly accurate WSE observations with a new radar altimetry solution, which comprises a 77 GHz radar chip with full waveform analysis and an accurate dual frequency differential Global Navigation Satellite System (GNSS) system. The radar altimetry solution shows the lowest standard deviation (sigma) and RMSE on WSE estimates, ca. 1.5 cm and ca. 3 cm respectively, whilst photogrammetry and LIDAR show a sigma and an RMSE at decimetre level. Radar altimetry also requires a significantly shorter survey and processing time compared to LIDAR and especially to photogrammetry.
机译:水表面升高(WSE)是一个重要的液压测量观察,可用于校准水文模型,预测洪水,评估气候变化。然而,原位衡量站的数量在全世界下降。卫星Altimetry包括最近发射的卫星任务(例如,雷达Altimetry Missions Cryosat 2,Jason 3,Sentinel 3a / B和Lidar Missionsat-2),只能在河流中确定WSE,这些河流超过CA。 100米宽。小型流中的WSE测量目前仍然限于现有的原位站点或耗时的原位调查。无人机空中系统(UAS)可以在短暂的调查时间内和极端天气条件下的飞行限制期间获得实时WSE观察,以及自动或半自动飞行操作。 UAS-Borne摄影测量是一种众所周知的技术,可以估算陆地高程,精度高达几厘米,同样uas-borne ridar可以估计陆地高程,但不需要地面控制点(GCPS)。然而,两种技术面临估计WSE的限制:水透明度和水面上缺乏稳定的视觉键点(WS)复杂化了WSE的UAS播种摄影测量估计,而来自水面的激光雷达反射通常不够强大由目前市场上目前可用的大多数UAS传统的激光器系统捕获。因此,LIDAR和摄影测量通常需要提取“水边”点的升高,即陆地和水之间的界面点,用于识别WSE。我们用新的雷达高级解决方案展示了高度准确的WSE观察,它包括具有全波形分析的77 GHz雷达芯片和精确的双频差分全球导航卫星系统(GNSS)系统。雷达Altimetry解决方案显示了最低标准偏差(Sigma)和WSE估计的RMSE,CA。 1.5厘米和加利福尼亚州。 3厘米分别,摄影测量和激光雷达展示了一个Sigma和Decimetre水平的RMSE。与LIDAR相比,雷达Altimetry还需要显着较短的调查和处理时间,特别是摄影测量。

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