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可视化和量化海洋运动。

Visualizing and Quantifying Oceanic Motion.

机构信息

Graduate School of Oceanography, University of Rhode Island, Narragansett, Rhode Island 02882; email:

出版信息

Ann Rev Mar Sci. 2016;8:35-57. doi: 10.1146/annurev-marine-122414-033849. Epub 2015 Aug 7.

Abstract

Here I review the use of two highly complementary acoustical technologies for measuring currents in the ocean: acoustically tracked neutrally buoyant floats and vessel-mounted acoustic Doppler current profilers (ADCPs). The beauty of floats lies in their ability to efficiently and accurately visualize fluid motion in fronts and vortices and the dispersion caused by mesoscale eddy processes. Floats complement classical hydrography by articulating mechanisms and pathways by which waters spread out from their source region. Vessel-mounted ADCPs can profile the water column at O(1 km) horizontal resolution to depths greater than 1,000 m. These vessel-based scans capture in detail the cross-stream structure of fronts and eddies as well as the impact of bathymetry on currents. Sustained sampling along selected routes builds up valuable databases both for statistical studies of the submesoscale velocity field and for accurate estimates of fluid transport, as well as how these vary over time.

摘要

在这里,我回顾了两种高度互补的声学技术在测量海洋中电流的应用:声学跟踪的中性浮力浮标和船载声学多普勒海流剖面仪 (ADCP)。浮标的优点在于它能够高效、准确地可视化锋面和涡旋中的流体运动以及中尺度涡过程引起的扩散。浮标通过阐明水从源区扩散的机制和途径来补充经典的海洋学。船载 ADCP 可以以 O(1 公里)的水平分辨率对水柱进行剖面测量,深度大于 1000 米。这些基于船只的扫描详细捕捉了锋面和涡旋的横向结构以及海底地形对水流的影响。沿着选定路线进行持续采样,可以为亚中尺度速度场的统计研究以及对流体输运的准确估计以及这些随时间的变化建立有价值的数据库。

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