通过文献延时摄影预测水位和排水量

Kenneth W. Chapman, T. Gilmore, M. Mehrubeoglu, Christian D. Chapman, A. Mittelstet, John E. Stranzl
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引用次数: 0

摘要

固定地面相机拍摄的图像包含丰富的定性和定量信息,可改善溪流排放监测。例如,延时图像可以填补传感器故障和/或监测项目资金短缺时的数据缺口。在这项研究中,我们使用了一个大型图像档案(从 2012 年到 2019 年,超过 40,000 张图像),该档案来自一台固定的地面相机,是文献流域成像项目的一部分 (https://plattebasintimelapse.com/)。从每隔一小时拍摄的日光图像中提取了标量图像特征。图像特征与美国地质调查局的水位和排水量数据融合,作为现场的响应变量。多层感知器、随机森林回归和支持向量回归模型生成了模拟一年数据缺口(2015、2016 和 2017 水年)的水位和排水量预测值。预测结果采用卡尔曼滤波器去除噪声。计算了误差指标,包括纳什-苏特克利夫效率(NSE)和一种基于阈值的替代性能指标,该指标考虑了季节性径流。全年间隙预测的排泄量 NSE 为 0.63 至 0.90,水位 NSE 为 0.47 至 0.90,其中 2016 年的误差更大,因为间隙期的河流排泄量大大超过了训练期的排泄量。重要的是,与不使用图像的缺口填补方法不同,2016 年的高排水量情况可以通过图像数据直观地(定性地)验证。为 2016 年创建了半年测试集,以便在训练集中包含更高的排水量,从而提高模型性能。虽然应进一步测试所选模型的其他机器学习算法和调整参数,但本研究证明了地面延时图像在填补水文时间序列数据的巨大空白方面的潜在价值。专用于水文传感的相机,包括夜间图像,可以进一步改善结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stage and discharge prediction from documentary time-lapse imagery
Imagery from fixed, ground-based cameras is rich in qualitative and quantitative information that can improve stream discharge monitoring. For instance, time-lapse imagery may be valuable for filling data gaps when sensors fail and/or during lapses in funding for monitoring programs. In this study, we used a large image archive (>40,000 images from 2012 to 2019) from a fixed, ground-based camera that is part of a documentary watershed imaging project (https://plattebasintimelapse.com/). Scalar image features were extracted from daylight images taken at one-hour intervals. The image features were fused with United States Geological Survey stage and discharge data as response variables from the site. Predictions of stage and discharge for simulated year-long data gaps (2015, 2016, and 2017 water years) were generated from Multi-layer Perceptron, Random Forest Regression, and Support Vector Regression models. A Kalman filter was applied to the predictions to remove noise. Error metrics were calculated, including Nash-Sutcliffe Efficiency (NSE) and an alternative threshold-based performance metric that accounted for seasonal runoff. NSE for the year-long gap predictions ranged from 0.63 to 0.90 for discharge and 0.47 to 0.90 for stage, with greater errors in 2016 when stream discharge during the gap period greatly exceeded discharge during the training periods. Importantly, and in contrast to gap-filling methods that do not use imagery, the high discharge conditions in 2016 could be visually (qualitatively) verified from the image data. Half-year test sets were created for 2016 to include higher discharges in the training sets, thus improving model performance. While additional machine learning algorithms and tuning parameters for selected models should be tested further, this study demonstrates the potential value of ground-based time-lapse images for filling large gaps in hydrologic time series data. Cameras dedicated for hydrologic sensing, including nighttime imagery, could further improve results.
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