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Characteristics of ocean bottom roughness for several seamounts derived from multibeam bathymetric data

机译:从多波束测深数据得出的若干海山海底粗糙度特征

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Multibeam bathymetric systems offer to revolutionize our understanding of the ocean bottom and its major structural features by providing highly detailed measurements of the bottom. Further, multibeam measurements yield bottom depth as a function of both spatial coordinates (i.e. along-track and across-track). The depth resolution is sufficiently fine that conventional contour charts would never incorporate all the information available in the multibeam data. As an alternative to such deterministic presentations, it can be suggested that statistical characterizations be developed for topographic variability at horizontal scales which are small in comparison to the overall dimensions of the feature of interest. We here discuss the study of rough topography on several seamounts by means of multibeam bathymetry. The bottom topography is analyzed in terms of numerous samples of1600 m times 1600m extent. A primary quantity of interest is the rms value of the residual topography. The pattern of variability for the rms values is described for several seamounts and shown to have certain overall similarities.
机译:多波束测深系统通过提供对海底的高度详细的测量,彻底改变了我们对海底及其主要结构特征的理解。此外,多光束测量产生的底部深度是两个空间坐标(即沿轨道和跨轨道)的函数。深度分辨率足够精细,以至于常规轮廓图永远不会包含多光束数据中的所有可用信息。作为这种确定性表示的替代方法,可以建议针对水平尺度的地形变异性开发统计特征,该特征与感兴趣特征的整体尺寸相比较小。我们在这里讨论通过多波束测深法在几个海山上的粗糙地形的研究。根据 1600 m×1600 m范围的大量样本分析底部地形。感兴趣的主要数量是剩余形貌的均方根值。均方根值的变异性模式在几个海山上都有描述,并显示出一定的总体相似性。

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