Surface Flow Velocities From Space: Particle Image Velocimetry of Satellite Video of a Large, Sediment-Laden River

Carl J Legleiter,Paul J Kinzel

doi:10.3389/frwa.2021.652213

Abstract

Conventional, field-based streamflow monitoring in remote, inaccessible locations such as Alaska poses logistical challenges. Safety concerns, financial considerations, and a desire to expand water-observing networks make remote sensing an appealing alternative means of collecting hydrologic data. In an ongoing effort to develop non-contact methods for measuring river discharge, we evaluated the potential to estimate surface flow velocities from satellite video of a large, sediment-laden river in Alaska via particle image velocimetry (PIV). In this setting, naturally occurring sediment boil vortices produced distinct water surface features that could be tracked from frame to frame as they were advected by the flow, obviating the need to introduce artificial tracer particles. In this study, we refined an end-to-end workflow that involved stabilization and geo-referencing, image preprocessing, PIV analysis with an ensemble correlation algorithm, and post-processing of PIV output to filter outliers and scale and geo-reference velocity vectors. Applying these procedures to image sequences extracted from satellite video allowed us to produce high resolution surface velocity fields; field measurements of depth-averaged flow velocity were used to assess accuracy. Our results confirmed the importance of preprocessing images to enhance contrast and indicated that lower frame rates (e.g., 0.25 Hz) lead to more reliable velocity estimates because longer capture intervals allow more time for water surface features to translate several pixels between frames, given the relatively coarse spatial resolution of the satellite data. Although agreement between PIV-derived velocity estimates and field measurements was weak (R2 = 0.39) on a point-by-point basis, correspondence improved when the PIV output was aggregated to the cross-sectional scale. For example, the correspondence between cross-sectional maximum velocities inferred via remote sensing and measured in the field was much stronger (R2 = 0.76), suggesting that satellite video could play a role in measuring river discharge. Examining correlation matrices produced as an intermediate output of the PIV algorithm yielded insight on the interactions between image frame rate and sensor spatial resolution, which must be considered in tandem. Although further research and technological development are needed, measuring surface flow velocities from satellite video could become a viable tool for streamflow monitoring in certain fluvial environments.

Highlights

Regular, reliable monitoring of streamflow is crucial for a number of management applications including water supply forecasting, flood hazard assessment, habitat conservation, and provision of recreational opportunities
In a recent study on the Tanana River, we used video acquired from a helicopter hovering above the channel to produce continuous, two-dimensional, high spatial resolution surface velocity fields that agreed closely (R2 up to 0.99) with depth-averaged velocities measured directly in the field
A frame from the middle of the stack was designated as the reference and all of the other images were registered to this base using a scale-invariant feature transform (SIFT) algorithm that identified distinct features such as bridges and buildings that remained stationary throughout the video

Summary

Introduction

Reliable monitoring of streamflow is crucial for a number of management applications including water supply forecasting, flood hazard assessment, habitat conservation, and provision of recreational opportunities. Obtaining basic information on river discharge can be difficult and costly, in remote, inaccessible locations. The state of Alaska features over 1,200,000 km of rivers and streams, the U.S Geological Survey (USGS) streamgage network consists of only 111 continuous monitoring locations, a density of coverage far less than in the contiguous U.S (Conaway et al, 2019). The USGS is actively seeking to improve safety, increase efficiency, and expand the streamgage network by developing non-contact methods for measuring streamflow. In this study we explore an alternative strategy focused on inferring one component of discharge, flow velocity, from high spatial resolution satellite video that captures dynamic water surface features and enables particle image velocimetry (PIV)

Methods

Results

Discussion

Conclusion