首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Characterizing uncertainties for quantifying bathymetry change between time-separated multibeam echo-sounder surveys
【24h】

Characterizing uncertainties for quantifying bathymetry change between time-separated multibeam echo-sounder surveys

机译:表征时间间隔多波束回声测深测量之间测深变化变化的不确定性特征

获取原文
获取原文并翻译 | 示例
           

摘要

Changes of bathymetry derived from multibeam sonars are useful for quantifying the effects of many sedimentary, tectonic and volcanic processes, but depth changes also require an assessment of their uncertainty. Here, we outline and illustrate a simple technique that aims both to quantify uncertainties and to help reveal the spatial character of errors. An area of immobile seafloor is mapped in each survey, providing a common 'benchmark'. Each survey dataset over the benchmark is filtered with a simple moving-averaging window and depth differences between the two surveys are collated to derive a difference histogram. The procedure is repeated using different length-scales of filtering. By plotting the variability of the differences versus the length-scale of the filter, the different effects of spatially uncorrelated and correlated noise can be deduced. The former causes variability to decrease systematically as predicted by the Central Limit Theorem, whereas the remaining variability not predicted by the Central Limit Theorem then represents the effect of spatially correlated noise. Calculations made separately for different beams can reveal whether problems are due to heave, roll, etc., which affect inner and outer beams differently. We show how the results can be applied to create a map of uncertainties, which can be used to remove insignificant data from the bathymetric change map. We illustrate the technique by characterizing changes in nearshore bed morphology over one annual cycle using data from a subtidal bay, bedrock headland and a banner sand bank in the Bristol Channel UK. (C) 2008 Elsevier Ltd. All rights reserved.
机译:来自多束声纳的测深法变化可用于量化许多沉积,构造和火山过程的影响,但深度变化还需要对其不确定性进行评估。在这里,我们概述并说明了一种简单的技术,该技术旨在量化不确定性并帮助揭示错误的空间特征。在每个调查中都绘制了一个固定的海底区域,提供了一个共同的“基准”。使用简单的移动平均窗口对基准之上的每个调查数据集进行过滤,并整理两次调查之间的深度差异,以得出差异直方图。使用不同的过滤长度尺度重复该过程。通过绘制差异的变化与滤波器的长度比例关系,可以推断出空间不相关和相关噪声的不同影响。前者导致变异性如中央极限定理所预测的那样系统地降低,而其余变异性则没有中央极限定理所预测,则代表了空间相关噪声的影响。对不同梁单独进行的计算可以揭示问题是否是由起伏,侧倾等引起的,这些问题对内梁和外梁的影响不同。我们展示了如何将结果应用于创建不确定性图,该图可用于从测深更改图中删除不重要的数据。我们通过使用潮汐湾,基岩岬角和英国布里斯托尔海峡的旗帜砂岸的数据来表征一年周期内近岸床形态变化的特征来说明这项技术。 (C)2008 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号