Dead zone returns to Oregon Coast |

Dead zone returns to Oregon Coast

Jeff Barnard
Associated Press
Vail, CO Colorado
Elizabeth Gates, AP/Oregon State UniversityDungeness crabs are washed ashore along the Oregon coastline. Dead zones, which sometimes appear off the Oregon Coast kill fish, crabs and sea worms.

GRANTS PASS, Ore. ” For the sixth year in a row, a dead zone of oxygen-depleted water that kills crabs and drives out fish is forming off the Oregon Coast, raising the possibility it could become the new normal as the climate warms, scientists said Monday.

The formation appeared to be dissipating in early July, but a survey of the 25 miles of Continental Shelf between Newport and Cape Perpetua last Friday by the Oregon State University research vessel Elakha found conditions returning to those of last year.

“It does, indeed, appear to be the new normal,” said Jane Lubchenco, professor of marine biology at OSU. “The appearance of the low-oxygen water again is consistent with predictions of climate change. The fact that we are seeing six in a row now tells us that something pretty fundamental has changed about conditions off of our coast.”

Unlike the dead zone in the Gulf of Mexico, which is caused by fertilizer washing down the Mississippi River, the Oregon Coast dead zone is triggered by northerly winds, which create an ocean-mixing condition called upwelling.

This brings low-oxygen waters from deep in the ocean close to shore, and spreads nitrogen and other nutrients through the water column, kicking off a population boom of plankton, the tiny plants and animals at the foundation of the ocean food web.

Normally, this is good for salmon, giving them lots of food to eat. But when huge amounts of plankton die, they fall to the bottom of the ocean, where they decompose, depleting the water of oxygen.

The wind patterns responsible for the dead zones are consistent with what is expected with global warming: warmer temperatures on land strengthen a low pressure area that draws more air in from the cooler ocean, creating the winds that set up the upwelling, and driving the dead zone closer to shore.

After dissipating with a change in wind patterns in the fall, the dead zone was reforming in early summer this year, when an abrupt cooling on land switched the wind around to the south, turning off the upwelling and allowing the dead zone to dissipate, said Francis Chan, a research professor of marine ecology at OSU.

Then the northerly winds returned, and so did the dead zone.

Instruments towed back and forth last week from one mile offshore to 12 miles offshore between Cape Perpetua and Newport found oxygen levels as low as one-sixth of normal, Chan said. That is not as bad as last year, but weather forecasts call for strong northerly winds the rest of this week.

“The system is primed for a replay of last year,” Lubchenco said. “But that doesn’t mean it will necessarily happen. It may not be as bad as last year and it all depends on the winds.”

Last year, the worst yet, scientists plotted a dead zone that stretched from southern Oregon to the tip of Olympic Peninsula in Washington, a distance of nearly 300 miles.

Video from a remotely operated submersible showed a crab graveyard on the Perpetua Reef south of Newport, and fishermen reported unusually large numbers of rockfish ” apparently able to swim away from the dead zone ” in unexpected areas on its edges, Lubchenco said.

New video from May showed some rockfish and sea stars had returned, but less mobile creatures such as sea anemones and sea cucumbers had not.

“The current low oxygen conditions may knock the system back to the starting line, delivering another setback to an already stressed system,” Lubchenco added. “This marine ecosystem may take as long to recover as the terrestrial ecosystem did from the eruption of Mount St. Helens.”

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