Study takes next step in remote sensing methods for rivers

By on June 13, 2013
Top image: This optical attachment connected the spectroradiometer to a submersible fibre optic cable allowed for measurements above and below water (Credit: Carl Legleiter)

Top image: This optical attachment connected the spectroradiometer to a submersible fibre optic cable allowed for measurements above and below water (Credit: Carl Legleiter)

A series of experiments at a novel outdoor laboratory could have scientists one step closer to measuring important attributes of rivers and streams from airborne instruments.

Carl Legleiter, assistant professor with the University of Wyoming’s Department of Geography, specializes in remote sensing of rivers. His past work has focused on calculating river depth from spectral data collected by instruments carried by aircraft or satellites.

He said the methods he’s helped to develop for estimating depth are close to becoming fully operational, which had him wondering what might be next.

“We’ve done a study on the Snake River here in Wyoming showing that estimating water depth from satellite image data is definitely feasible,” Legleiter said. “So we wanted to move on to seeing what else we could try to measure from remote sensing data.”

Moving on to estimating other stream attributes from the sky meant starting on the ground, in this case at the National Center for Earth-Surface Dynamics Outdoor StreamLab. The StreamLab features an engineered stream channel fed by water pumped from the Mississippi River that meanders across the property of the University of Minnesota’s St. Anthony Falls Laboratory.

The Outdoor StreamLab was an ideal setting for the experiments, the results of which were recently published in the journal River Research and Applications. The facility allowed the researchers to manipulate some conditions that wouldn’t have been possible on a natural river. And the experiments were based on measurements of how the river reflected light energy coming from the sun, so working with an experimental flume indoors wouldn’t cut it.

“For us, it was really critical because doing our study inside wouldn’t make any sense,” Legleiter said. “We need to have the sun as a source of energy for the reflectance measurements.”

The researchers mounted their instruments to a mechanized cart that spanned the channel, allowing for precise positioning of the devices over the water surface. The instruments included a spectroradiometer for recording radiance, an ultrasonic profiler for high resolution measurements of water surface elevation, and an acoustic Doppler velocimeter for flow velocity.

An overview of the experimental setup at the Outdoor StreamLab, including the mechanized cart supporting the acoustic Doppler velocimeter and spectrometer (Credit: Carl Legleiter)

An overview of the experimental setup at the Outdoor StreamLab, including the mechanized cart supporting the acoustic Doppler velocimeter and spectrometer (Credit: Carl Legleiter)

One experiment was an early step in determining whether the abundance of algae growing on the stream bed could be estimated by remote sensing. The researchers controlled algal abundance by placing ceramic tiles on the stream bed one at a time over the course of nine days. The longer a tile had been in the stream, the more algae it accumulated on its surface.

Using the spectroradiometer, the researchers found that certain characteristics of the light reflecting off of the tiles corresponded with the differing amounts of algae that had colonized each tile. That’s an encouraging result that suggests this method could be scaled up to calculate algal abundance or map periphyton development through remotely sensed image data.

Another practical application that could take advantage of algae’s strong spectral signal from the stream bed is the detection of stream sections where the bed has been recently disturbed, whether by sediment transport or a salmon digging around in the gravel to build a nest.

“It boils down to the difference between the top and the bottom of the rocks,” Legleiter said. “The top is going to have been exposed and have algae coating it, whereas if the the bed is disturbed, some of the rocks are going to be flipped over upside down.”

That means the clean, fresh face of the upended rocks will give off a much different spectral signal than the rocks around it.

“If you can identify places that have a larger proportion of the bed agitated like this, with some of the rocks turned over, we could use that to map salmon spawning locations,” he said.

Legleiter will be working on a project attempting to do just that on a river in Oregon on this fall. That project attests to the value of their efforts at the Outdoor StreamLab, which were funded by the National Center for Earth-Surface Dynamics Visitor Program and the Office of Naval Research Littoral Geoscience and Optics Program.

“This study at the outdoor stream lab was really a proof-of-concept to show that there is some physical basis for this,” Legleiter said. “It definitely works in this controlled lab setting, so we now have some justification for trying to apply this approach to actual image data.”

Top image: This optical attachment connected the spectroradiometer to a submersible fibre optic cable allowed for measurements above and below water (Credit: Carl Legleiter)

About Jeff Gillies

Jeff Brooks-Gillies has written about science, energy and the environment for going on 10 years. He's a native Michigander who, after a stint in Colorado, lives in Indianapolis with his wife and two kids.

Leave a Reply

Your email address will not be published. Required fields are marked *

Time limit is exhausted. Please reload CAPTCHA.