A Simple Solution for Refining Lake Water Temperature Profiles Data Arrayed from High-Frequency Monitoring Sensors

A. B. Santoso, E. Triwisesa, M. Fakhrudin
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Abstract

The revolutionized aquatic monitoring sensors are essential in capturing environmental patterns that traditional discrete samplings might not be able to. They allow scientists to further synthesize and better conclude processes in aquatic ecosystems. These sensors produce high-frequency data that provide information on a fine temporal scale, even near real-time. The massive quantities of the streamed data, however, create challenges for scientists to grasp the concrete information. Filtering data quality, on the other hand, is another problem scientists might have encountered as sensor accuracy and precision may drift along the line. Hence, quality assurance and quality control might be quite labouring owing to the size of datasets to handle. This paper proposed a semi-mechanistic algorithm to improved false water temperature data. Using “theoretical” thermal stratification as a reference, this algorithm fixed sensors error readings. A 5-month dataset of water temperature profiles of Lake Maninjau, West Sumatra, captured every 10 minutes from a set of sensors in thermistor chain was applied. We found that most data fit to the theoretical temperature profile, R2 = 0.962, RMSE = 0.081oC. A number of errors, however, were observed in the upper layer of the lake (<20 m), the most dynamic layer in terms of its thermal variation. Sensor drifts in this active upper mixed layer can be related to the generated errors. Through this simple solution, not only improving the quality of the observed water temperature data, but was also able to identify the most probable source of errors
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从高频监测传感器阵列中提炼湖泊水温剖面数据的简单解决方案
革命性的水生监测传感器对于捕获传统的离散采样可能无法实现的环境模式至关重要。它们使科学家能够进一步综合和更好地总结水生生态系统的过程。这些传感器产生高频数据,提供精细时间尺度的信息,甚至接近实时。然而,大量的流数据给科学家们掌握具体信息带来了挑战。另一方面,过滤数据质量是科学家可能遇到的另一个问题,因为传感器的准确性和精度可能会随线路漂移。因此,由于要处理的数据集的大小,质量保证和质量控制可能相当费力。提出了一种半机械式的水温数据修正算法。该算法以“理论”热分层为参考,固定了传感器的误差读数。利用热敏电阻链上的一组传感器每10分钟采集一次西苏门答腊岛Maninjau湖5个月的水温剖面数据集。我们发现大部分数据符合理论温度曲线,R2 = 0.962, RMSE = 0.081oC。然而,在湖的上层(<20 m)观测到一些误差,这是热变化最动态的层。传感器在这个主动上层混合层中的漂移可能与产生的误差有关。通过这个简单的解决方案,不仅提高了观测水温数据的质量,而且能够识别出最可能的误差来源
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