首页> 外文会议>OCEANS 2012 MTS/IEEE Yeosu >Obtaining absolute water velocity profiles from glider-mounted Acoustic Doppler Current Profilers
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Obtaining absolute water velocity profiles from glider-mounted Acoustic Doppler Current Profilers

机译:从安装在滑翔机上的声学多普勒电流剖面仪获得绝对水速剖面

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ADCP sensors have recently been incorporated into AUV Gliders offering the potential for increased physical and biological oceanographic observations. These vehicles can collect high-density measurements for weeks at a time at a small cost compared to vessel-reliant operations. Glider-based ADCPs can provide absolute water velocity profiles based on the “shear method” developed from LADCP research and offer the ability to perform oceanographic research where stationary platform and vessel-based ADCP observations are unavailable or not suitable. The ability to obtain accurate velocity profiles from gliders will further enable high resolution and cost-effective oceanographic observations. Shear is calculated from water track velocities measurements for every ensemble and averaged within depth intervals to create one shear profile for each glider dive. The vertically averaged shear profile is integrated to establish a velocity profile relative to the bottom of the glider dive. As shear is independent of platform motion, integrated relative velocities will not contain glider motion bias. Absolute velocities are computed by referencing dive-averaged velocity measurements, based on the glider drift. Bottom track velocities, where available, they be referenced to water track measurements and provide absolute velocities. Bottom referenced velocities provide a verification for dive-averaged velocities and are valuable for removing diverging velocity offsets. Effective data processing methods, data filtering, accurate heading information, and instrument settings for high-quality data collection are the tools for obtaining absolute water velocity profiles from gliders. The Oregon State University Glider Research Group is refining these methods by comparing results against concurrent velocity measurements from adjacent ADCP platforms. The findings described in this document result from experiments performed in 2011 by OSU off the Oregon Shelf and during the Off- ce of Naval Research sponsored Lateral Mixing Project in the Sargasso Sea.
机译:ADCP传感器最近已被合并到AUV滑翔机中,具有增加物理和生物海洋学观测的潜力。与依靠船只的操作相比,这些车辆可以一次收集数周的高密度测量值,而费用却很少。基于滑翔机的ADCP可以基于LADCP研究开发的“剪切法”提供绝对水速剖面,并提供在无法使用固定平台和基于船只的ADCP观测值或不合适的情况下进行海洋学研究的能力。从滑翔机获得准确的速度剖面的能力将进一步实现高分辨率和具有成本效益的海洋学观测。剪切力是根据每个集合体的水道速度测量值计算得出的,并在深度间隔内求平均值,以为每次滑翔机俯冲创造一个剪切力轮廓。垂直平均剪切剖面被整合以建立相对于滑翔机潜水底部的速度剖面。由于剪切力与平台运动无关,因此集成的相对速度将不包含滑翔机运动偏差。通过参考潜水平均速度测量值(基于滑翔机漂移)来计算绝对速度。底部航迹速度(如果有的话)将作为水迹测量的参考,并提供绝对速度。底部参考速度为潜水平均速度提供了验证,对于消除发散速度偏移非常有用。有效的数据处理方法,数据过滤,准确的航向信息以及用于高质量数据收集的仪器设置是从滑翔机获取绝对水速剖面的工具。俄勒冈州立大学滑翔机研究小组正在通过将结果与相邻ADCP平台同时进行的速度测量结果进行比较来完善这些方法。本文档中描述的发现来自俄勒冈州立大学2011年在俄勒冈架子外进行的实验以及海军研究资助的Sargasso海横向混合项目期间的实验。

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