"The tidal currents that slosh the water back and forth, that's what's really obvious," MacCready says. "But there's also a slow, persistent circulation that is constantly bringing deep water in, mixing it up, and sending the surface water out," says Parker MacCready. (Credit: Minette/Flickr)

Puget Sound waters bubble up from turbulent canyon

Puget Sound’s headwaters lie far below the surface, in a submarine canyon that draws nutrient-rich water up from the deep ocean.

The new findings  may explain how the Pacific Northwest’s inland waters are able to support so many shellfish, salmon runs, and even the occasional pod of whales.

The first detailed measurements at the headwater’s source—offshore from the strait that separates the US and Canada—show water surging up through the canyon and mixing at surprisingly high rates.

An instrument that measured fast-moving water near the seafloor inside the Juan de Fuca Canyon showed water flowing as fast as 1.3 feet per second at 500 feet below the surface, and showed mixing up to 1,000 times the normal rate for the deep ocean. (Credit: Parker MacCready)
An instrument that measured fast-moving water near the seafloor inside the Juan de Fuca Canyon showed water flowing as fast as 1.3 feet per second at 500 feet below the surface, and showed mixing up to 1,000 times the normal rate for the deep ocean. (Credit: Parker MacCready)

“This is the headwaters of Puget Sound,” says coauthor Parker MacCready, professor of oceanography at the University of Washington. “That’s why it’s so salty in Puget Sound, that’s why the water is pretty clean, and that’s why there’s high productivity in Puget Sound, because you’re constantly pulling in this deep water.”

It has been known for decades that 20 to 30 times more deep water flows into Puget Sound than from all the rivers combined. Surface tides, while dramatic, play a minor role.

“The tidal currents that slosh the water back and forth, that’s what’s really obvious,” MacCready says. “But there’s also a slow, persistent circulation that is constantly bringing deep water in, mixing it up, and sending the surface water out.”

New measurements show this canyon potentially supplies most of the water coming into Puget Sound, the Strait of Juan de Fuca, and Canada’s Georgia Strait.

Marine canyons

The intense flow and mixing measured inside the canyon could help explain the mysterious productivity of Northwest shores. Coastal winds usually bring nutrients up on the west coast, but the numbers don’t add up for this region.

“Washington is several times more productive—has more phytoplankton—than Oregon or California, and yet the winds here are several times weaker. That’s been kind of a puzzle, for years,” says coauthor Matthew Alford, an oceanographer at the Applied Physics Laboratory.

The secret to the Northwest’s outsize productivity could be marine canyons, an idea first suggested by oceanographer Barbara Hickey. The northern section of the west coast has many more canyons than Oregon or California, with 11 along the Washington coast.

Published in the journal Geophysical Research Letters, the new paper provides the latest evidence for these canyons’ importance.

Measurements in the 1970s first showed water flowing through Juan de Fuca Canyon with a direction that depends on the coastal winds. More recently, 2008 calculations suggested submarine canyons could play an important role in supplying nutrients to the Northwest coastal waters.

Smooth flow of water

Alford and MacCready measured inside the Juan de Fuca Canyon in April 2013 using an instrument that takes water measurements near the seafloor. During a day and a half of round-the-clock observations they got lucky with the wind direction and recorded strong flow up through the canyon.

Water flowed as fast as 1.3 feet per second at 500 feet below the surface, and showed mixing up to 1,000 times the normal rate for the deep ocean. The data also showed that the flow is hydraulically-controlled, meaning it flows smoothly over a shallow ridge just off the cape and then forms a turbulent breaking wave on the other side, mixing with the waters far above.

The deep water forced up through the canyon is rich in nutrients that support the growth of marine plants which then feed other marine life. Those waters also are more acidic and lower in oxygen, all of which contribute to water conditions in the Sound.

“The location of this sill would be an outstanding place to fish,” Alford says. “People fish in Juan de Fuca Canyon pretty actively, and that’s probably no coincidence.”

Ocean acidity

Pinpointing the source of Puget Sound waters will help make better computer models of circulation through the region, and eventually could help forecast ocean acidity, harmful algal blooms, and low-oxygen events.

“Canyons might be important not just for coastal productivity, but that mixed water also gets exported into the interior of the ocean,” Alford says. “I look at this as a first step in getting canyons right in coastal models and in global climate models, because I think it could potentially be a very important source of mixing.”

The research was funded by the Office of Naval Research and the National Oceanic and Atmospheric Administration. University of Washington funded the ship time aboard the Thomas G. Thompson.

Source: University of Washington

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