海流和涡度测量的远程互易声传输综述

B. Dushaw, D. Chester, P. Worcester
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引用次数: 3

摘要

声波的互反传输精确地测量了洋流的正压和斜压分量,加上合适的射线路径几何形状。层析导出的潮流与独立测量和数值模型都一致。层析成像导出的电流本质上是范围平均值。然而,与点测量的比较,例如从当前的仪表,显示在所有情况下令人满意的一致。层析成像导出的面平均相对涡度是独特的,难以验证,但在佛罗里达海峡和墨西哥湾流区域层析成像涡度估计与电流计导出的涡度估计一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A review of ocean current and vorticity measurements using long-range reciprocal acoustic transmissions
Reciprocal acoustic transmissions accurately measure the barotropic and, with suitable ray-path geometry, baroclinic components of ocean currents. Tomographically-derived tidal currents agree with both independent measurements and numerical models. Tomographically-derived currents are inherently range averages. Comparison with point measurements, such as from current meters, nonetheless show satisfactory agreement in all cases. Tomographically-derived, areal-averaged relative vorticity is unique and difficult to verify, but in both the Florida Straits and Gulf Stream regions tomographic vorticity estimates are consistent with current-meter-derived vorticity estimates.<>
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