The Measurement of Shallow Ocean Currents Beneath Deformed Mobile Sea Ice Using Upward Looking Sonar Instruments

T. Mudge, D. Fissel, K. Borg, N. Milutinovic, E. Ross
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引用次数: 1

Abstract

The under ice ocean currents are critical in the understanding of the boundary layer between the sea ice and the ocean, involving determination of the drag forces that sea-ice exerts on the upper water column and the related turbulence and mixing levels. A semi-automated algorithm has been developed, which accounts for the changes in sea ice drafts, to determine the nearest surface ocean current measurement level. Using long-term measurements from upward looking sonar datasets in the Chukchi and Beaufort Seas, the algorithm and its extensions to all current bins is investigated.
利用上视声纳测量变形移动海冰下的浅海洋流
冰下洋流对于理解海冰和海洋之间的边界层是至关重要的,它涉及到确定海冰对上层水柱施加的阻力以及相关的湍流和混合水平。研究人员开发了一种半自动化算法,该算法考虑了海冰吃水的变化,以确定最近的海面洋流测量水平。利用楚科奇海和波弗特海向上观测声纳数据集的长期测量数据,研究了该算法及其对所有当前箱的扩展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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