论文标题
开发用于冰中波的原位测量的开源仪器
Development of open source instruments for in-situ measurements of waves in ice
论文作者
论文摘要
表面波和海冰之间的相互作用涉及许多复杂的物理现象,例如粘性阻尼,波衍射和非线性效应。这些现象的结合以及冰构型的差异很大,从粘稠的冰冰滑冰到大型冰山,通过封闭的漂浮冰和Landfast冰,使在冰模型中发展强劲而准确的波动变得具有挑战性。在这种情况下,建模者面临的挑战的原因可能在于可用于测试理论的冰数据中波浪的相对稀缺与海上现象发生的广泛多样性之间的不匹配。缺乏实验数据可能至少部分通过冰仪器中的波浪成本来解释。因此,开源,低成本,高性能仪器的发展可能是帮助发展这一研究领域的关键因素。在这里,我们介绍了新一代的冰仪器中新一代开源浪潮的发展,该冰仪器具有高精度惯性单元以及GPS,机上处理能力,太阳能电池板和虹膜通信。这些乐器现在被几个小组使用,它们的简单和模块化设计使它们可以快速以降低成本来定制特定需求。因此,它们可能是允许以具有成本效益的方式收集更多数据的重要因素,从而为ICE社区的波浪提供了急需的数据。此处通过介绍最近的海冰漂移和波动活动数据来验证这种方法,并将这些结果与商购浮标获得的结果进行比较。此外,我们的设计可用作具有成本效益的其他原位仪器的一般平台,该工具对低功率数据记录,车载计算功率和卫星通信的要求相似。
The interaction between surface waves and sea ice involves many complex physical phenomena such as viscous damping, wave diffraction, and nonlinear effects. The combination of these phenomena, together with considerable variability in ice configuration, ranging from viscous grease ice slicks to large icebergs through closed drift ice and landfast ice, makes it challenging to develop robust and accurate waves in ice models. In this context, a reason for the challenges modellers are facing may lie in the mismatch between the relative scarcity of waves in ice data available for testing theories, and the wide diversity of phenomena happening at sea. This lack of experimental data may be explained, at least in part, by the high cost of waves in ice instruments. Therefore, development of open source, low-cost, high-performance instrumentation may be a critical factor in helping advance this field of research. Here, we present recent developments of a new generation of open source waves in ice instruments featuring a high accuracy Inertial Motion Unit as well as GPS, on-board processing power, solar panel, and Iridium communications. Those instruments are now being used by several groups, and their simple and modular design allows them to be customized for specific needs quickly and at reduced cost. Therefore, they may be an important factor in allowing more data to be gathered in a cost-effective way, providing much-needed data to the waves in ice community. This approach is here validated by presenting recent sea ice drift and wave activity data, and comparing these results with those obtained with commercially available buoys. In addition, our design may be used as a general platform for cost-effective development of other in-situ instruments with similar requirements of low-power data logging, on-board computational power, and satellite communications.