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首页> 外文期刊>Marine Geodesy >Centimeter-Level Positioning of Seafloor Acoustic Transponders from a Deeply-Towed Interrogator
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Centimeter-Level Positioning of Seafloor Acoustic Transponders from a Deeply-Towed Interrogator

机译:深层询问器对海底声应答器的厘米级定位

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摘要

An array of three seafloor transponders was acoustically surveyed to centimeter pieci-sion with a deeply-towed interrogator. Measurements of two-way acoustic travel lime and hydrostatic pressure made as the interrogator was towed above the array were combined in a least-squares adjustment to estimate the interrogator and transponder positions in two surveys spanning two years. No transponder displacements were ex-pected at this site in the interior of the Juan de Fuca Plate (48°11′ N, 127°12? W) due to the lack of active faults. This was confirmed to a precision of ±2 cm by least-squares adjustment. Marginally detectable blunders in the observations were shown 10 affect the transponder position estimates by no more than 3 mm, demonstrating the geometric strength of the data set. The accumulation of many hundreds of observations resulted in a significant computational burden on the least-squares inversion procedure. The sparseness of the normal matrix was exploited to reduce by a factor of 1000 the num-ber of calculations. The acoustic survey results suggested that the near-bottom sound speed fields during the two surveys were in better agreement than inferred from yearly single-profile conductivity, temperature, and pressure (CTD) measurements.
机译:用一个拖曳的询问器对三个海底应答器阵列进行声学测量,以达到厘米精度。将询问器拖到阵列上方时进行的双向声学传播石灰和静水压力的测量以最小二乘平差进行组合,以估算两年中两次调查中的询问器和应答器位置。由于没有活动断层,在胡安德富卡板块内部(48°11'N,127°12°?W)没有发现应答器位移。通过最小二乘平差将其确认为±2 cm的精度。观测结果中的边缘可检测到的错误显示10对应答器位置估计的影响不超过3毫米,证明了数据集的几何强度。数百个观测值的累积导致最小二乘反演程序的计算负担很大。利用正常矩阵的稀疏性将计算数量减少了1000倍。声学调查结果表明,两次调查中的近底声速场比从年度单剖面电导率,温度和压力(CTD)测量得出的结论更好。

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