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Waveform Simulator and Analytical Procedure for JAXA's Future Spaceborne LiDAR to Measure Canopy Height

机译:JAXA未来星载激光雷达测量冠层高度的波形模拟器和分析程序

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High-accuracy three-dimensional (3D) information of global area is useful in various fields, such as global observations of canopy height, elevation and ice sheet. Especially, there are pressing needs to advance understanding of how changes in the 3D structure of terrestrial vegetation are affecting the global carbon dynamics and their implications for climate change. Thus new space based observations are needed to measure global maps of the 3D structure of vegetation. Japan Aerospace Exploration Agency has started a conceptual study of the spaceborne vegetation LiDAR called MOLI (Multi-Footprint Observation LiDAR and Imager) which will enable us to obtain high-accuracy 3D information of vegetation areas from the globe. To investigate waveforms and analysis procedure, the waveform-simulator for MOLI was developed. Comparing with previous studies about the canopy height estimation from GLAS waveforms, waveform analysis procedure in which waveforms were fitted with a sum of Gaussian functions was studied. The maximum canopy height error was divided into two components; the basic error (E_B) which was not depending on terrain index (TI), which was the vertical difference between the highest and lowest elevation within a footprint, and the error depending on TI (E_(TI)). The total error (E_(Total)) could be RMS of the two. We propose E_(Total) in which E_B is 1 m and E_(TI) is 1/3~*TI as a target observation accuracy of MOLI. According to this error estimation, the observation accuracy of MOLI is 1m at a plane area (TI ≈ 0) and 3 m at slope area up to about 20 degree.
机译:全球面积的高精度三维(3D)信息在各个领域都非常有用,例如对冠层高度,海拔和冰盖的全球观测。尤其是,迫切需要进一步了解陆地植被的3D结构变化如何影响全球碳动态及其对气候变化的影响。因此,需要基于空间的新观测来测量植被的3D结构的全局图。日本航空航天探索局已经开始对称为MOLI(多脚印观察LiDAR和成像仪)的星载植被激光雷达进行概念研究,这将使我们能够从全球获取植被区域的高精度3D信息。为了研究波形和分析程序,开发了用于MOLI的波形模拟器。与先前关于通过GLAS波形估算树冠高度的研究相比较,研究了将波形与高斯函数之和拟合的波形分析程序。最大树冠高度误差分为两个部分:基本误差(E_B)不受地形指数(TI)的影响,该误差是足迹内最高和最低海拔之间的垂直差,而误差则取决于TI(E_(TI))。总误差(E_(Total))可能是两者的RMS。我们提出以E_(Total)为目标,将E_B为1 m,E_(TI)为1/3〜* TI作为目标观测精度。根据该误差估计,MOLI的观测精度在一个平面区域(TI≈0)为1m,在倾斜区域(约为20度)为3m。

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