ADCP数据收集自Liquid Robotics Wave Glider®

J. Mullison, D. Symonds, Neil Trenaman
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引用次数: 8

摘要

Liquid Robotics, Inc. (LRI)开发了一种自动驾驶汽车,Wave Glider®,它利用波浪能推进,铱星®卫星用于指挥、控制和数据泄露,GPS卫星传输用于定位。该船由一个配备了太阳能电池板、能量储存和岸上通信基础设施的低调水面浮子和一个位于大约7米深的地下机翼组成,它们通过一根复杂的绳索相互连接。机翼的设计是为了响应其深度的波浪能量,从而为操作员选择的任何位置提供推进力。这样,车辆所利用的波浪能可以用于移动到任何感兴趣的点,也可以用于在到达该位置后保持站点(通过在一个紧密的圆圈中行驶)。与岸上操作人员的实时通信可以监控平台的位置和收集的数据,指挥移动到新的位置,甚至完成任务的重新用途。Wave Glider®在各种环境和各种任务剖面中完成任务的能力现已得到充分证明。此外,Wave Glider®当然能够携带各种传感器有效载荷。LRI和Teledyne RD Instruments (TRDI)现在已经合作,提供车辆的当前轮廓测量。2009年的初步现场测试结果令人鼓舞,表明了该方法的可行性,值得进一步的研究,尽管有一些迹象表明,海面浮子的不对称运动(在某些海况下,浮子往往会在波面上滑动)加上低分辨率的GPS采样可能会使速度测量产生偏差。这导致了2010年配备ADCP,更高分辨率GPS和惯性运动单元的波浪滑翔机®的额外测试。一旦广泛的集成项目充分完成,就会启动新的现场活动,将新的、更集成的Wave Glider®ADCP测量结果与作为独立参考部署的底部安装的Workhorse ADCP进行比较。本次野外活动的任务概要包括对Wave Glider®进行编程,使其在参考ADCP部署的浅水和淹没峡谷的深水之间循环。通过这种方式,可以在浅水中进行测量,在浅水中可以有效地依靠底部跟踪能力来消除平台运动,而在深水中,底部不在范围内,平台的相对运动可以通过其他方式消除。考虑到深度的变化,没有理由假设参考ADCP测量值在较深的水中是有效的。然而,将参考仪器在浅水中的相对速度与底部轨迹和其他方法的相对速度进行比较,可以证明其他方法的实用性,并且在浅、参考和深、非参考状态之间的测量连续性表明两种情况下的测量都是正确的。我们报告现场测试的初步结果,以及集成的当前状态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ADCP data collected from a Liquid Robotics Wave Glider®
Liquid Robotics, Inc. (LRI) has developed an autonomous vehicle, the Wave Glider®, which utilizes wave energy for propulsion, Iridium® Satellite for command, control and data exfiltration and GPS satellite transmissions for positioning. The vehicle consists of a low-profile surface float outfitted with solar panels, energy storage and shore communication infrastructure and a subsurface wing located at approximately seven meters depth connected to each other by a sophisticated tether. The wing is designed to respond to the wave energy at its depth in such a way that it provides propulsion for the vehicle toward any location chosen by the operator. The wave energy thus harnessed by the vehicle can be used for locomotion to any point of interest as well as for station keeping (by driving in a tight circle) once that position is reached. Real time communication with the shore-based operator allows monitoring of platform's location and data gathered, commanding movement to a new position, or even complete repurposing of the mission. The capability of the Wave Glider® to accomplish its mission in a variety of environments with a variety of mission profiles is now well proven. In addition, the Wave Glider® is of course capable of carrying a variety of sensor payloads. LRI and Teledyne RD Instruments (TRDI) have now partnered to provide current profile measurements from the vehicle. An initial encouraging field test in 2009 showed the feasibility sufficiently to merit further work, though there was some indication that asymmetric motion of the surface float (it tends to skate on wave faces in some sea states) combined with low resolution GPS sampling could be biasing the velocity measurements. This led to additional testing of a Wave Glider® equipped with an ADCP, higher resolution GPS and an Inertial Motion Unit in 2010. Once the extensive integration project was completed sufficiently, a new field campaign was launched for comparison of the new, more integrated Wave Glider® ADCP measurements with those of a bottom mounted Workhorse ADCP that was deployed as an independent reference. The mission profile for this field campaign included programming the Wave Glider® to circle between the shallow water in which the reference ADCP was deployed to the deeper water of a submerged canyon. In this way measurements could be taken in shallow water, where bottom tracking capability could be effectively relied upon to remove platform motion, and in deeper water where the bottom was out of range and the relative motion of the platform removed by other means. Given the change in depth, there is no reason to assume the reference ADCP measurements are valid in the deeper water. However, comparison of the reference instrument in the shallow water with the relative velocity removed by bottom track and by the other methods can prove the utility of the other methods, and continuity of measurement between the shallow, referenced and deep, unreferenced regimes would indicate that the measurement in both instances is correct. We report on the initial results of the field testing, and on the current status of the integration.
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