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Data Processing of Laser Airborne Depth Mapping

机译:激光机载深度测绘的数据处理

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摘要

A laser airborne depth mapping (LADM) for the topography of coastal water was developed in China. System was implemented in South China Sea between 2001 and 2002. Data processing subsystem is introduced in this paper. Three automated waveform processing algorithms have been developed around several sets of heuristic rules to extract reliably accurate depths with a low false alarm rate. The position, pulse width and ratio of signal to noise are obtained by the low-pass differentiator algorithm (LD). The floor reflecting is determined by the signal above some thresholds in LD method. According to the characteristics of water attenuation, the received signal is revised by the inverse of the water attenuation coefficient (here after, RA method). The bottom is easier to distinguished from the enhanced contrast between the floor reflecting and water scattering. The LD and RA algorithms show a consist results in the post-flight data processing. A more simple and fast algorithms of delayed signal subtracter (DS) is used on flight as a real time data processing, in which the signal is delayed some time abd subtracted by the original signal. The three methods are analyzed in details. The result of data processing isalso presented.
机译:在中国开发了用于沿海水域地形的激光机载深度测绘(LADM)。该系统于2001年至2002年在南海实施。本文介绍了数据处理子系统。围绕几组启发式规则开发了三种自动波形处理算法,以可靠地提取准确的深度且误报率低。通过低通微分算法(LD)获得位置,脉冲宽度和信噪比。地板反射是由LD方法中高于某些阈值的信号确定的。根据水衰减的特性,通过水衰减系数的倒数来修正接收信号(此后称为RA方法)。底部更容易与地板反射和水散射之间增强的对比度区分开。 LD和RA算法在飞行后数据处理中显示出一致的结果。一种更简单,更快速的延迟信号减法器(DS)算法在飞行中用作实时数据处理,其中信号延迟了一段时间,并被原始信号减去。详细分析了这三种方法。还介绍了数据处理的结果。

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