Computer-Aided Mapping of Hydromorphic Features in the Columbia River

The Science

Interactions between flowing water and the geometry of river channels create forces that cause river water to enter the sediments surrounding the channel and eventually return to the channel. Such exchanges of surface and subsurface waters (called hydrologic exchange flows or HEFs) play a critical role in the fate of nutrients and contaminants in the river and thus significantly impact water quality. To simplify and enable computer simulation of these effects in large river reaches, this research developed a novel machine learning approach to map regions of the riverbed that have similar hydraulic and geometric characteristics (called hydromorphic features) and can be expected to exhibit similar HEFs.

The Impact

Geologists have long mapped hydromorphic features using subjective observations and expert knowledge. This work demonstrates a novel application of machine learning to combine hydrologic model outputs with remotely sensed data to perform this work in an objective, consistent, and automated manner. This result is an important step toward improving the ability to predict HEFs and their effects on nutrient cycling and water quality in large, complex river systems.

Summary

A team of scientists developed a machine learning method for quantitatively defining and mapping hydromorphic classes and then demonstrated this method on the 70-km Hanford Reach of the Columbia River (southeastern Washington state, USA). The novel approach uses outputs from river flow simulation models (depths and velocities) and remotely sensed bathymetric/topographic data to objectively define and map hydromorphic features. The identified feature classes are shown to correspond to spatially contiguous regions, and these coherent features are physically interpretable and consistent over the entire reach. Classification accuracy was verified using field observations of feature geometry and riverbed textural properties. Preliminary analysis of relationships between the mapped hydromorphic features and simulated values of exchange flows and transit time distributions based on high-resolution mechanistic modeling confirm that these important characteristics of river-subsurface exchange are distinct for each feature type. These confirmations provide a rational basis for using the results of high-resolution mechanistic models (feasible only within limited spatial domains) to predict system behaviors over much larger spatial domains.

Principal Investigator

Tim Scheibe
Pacific Northwest National Laboratory
[email protected]

Program Manager

Paul Bayer
U.S. Department of Energy, Biological and Environmental Research (SC-33)
Environmental System Science
[email protected]

Funding

This research was supported by the River Corridor Scientific Focus Area project at Pacific Northwest National Laboratory (PNNL) through the Office of Biological and Environmental Research (BER) Environmental System Science (ESS) program, within the U.S. Department of Energy’s (DOE) Office of Science.

References