Tag Archives: Hypoxia

Hood Canal report compiles oxygen studies

Despite millions of dollars spent on research in Hood Canal, the precise causes of low-oxygen problems in Southern Hood Canal are still not fully understood, according to a report released this week by the U.S. Environmental Protection Agency and the Washington Department of Ecology.

News articles about the report have created some confusion, and I’ll get to that in a moment.

As I reported in Tuesday’s Kitsap Sun, research has not proven that nitrogen from human sources is responsible for a decline in oxygen levels greater than 0.2 milligrams per liter anywhere in Hood Canal. That number is important, because it is the regulatory threshold for action under the Clean Water Act.

Mindy Roberts, one of the authors of the report, told me that scientists who have worked on the low-oxygen problem have gained an appreciation for Hood Canal’s exceedingly complex physical and biological systems. So far, they have not come to consensus about how much human inputs of nitrogen contribute to the low-oxygen problems in Lower Hood Canal.

The report, which examined the complexity and scientific uncertainty about these systems, seems to have generated some confusion, even among news reporters. I think it is important to understand two fundamental issues:

1. The deep main channel of Hood Canal is almost like a separate body of water from Lower Hood Canal (also called Lynch Cove in some reports). This area is generally defined as the waters between Sisters Point and Belfair. Because Lower Hood Canal does not flush well, low-oxygen conditions there are an ongoing and very serious problem.

2. Fish kills around Hoodsport cannot be equated or even closely correlated with the low-oxygen conditions in Lower Hood Canal. The cause of these fish kills was not well understood a decade ago, but now researchers generally agree that heavy seawater coming in from the ocean pushes up a layer of low-oxygen water. When winds from the south blow away the surface waters, the low-oxygen water rises to the surface, leaving fish no place to go.

I’m not aware that researchers were blaming nitrogen from septic systems for the massive episodic fish kills, as Craig Welch reports in the Seattle Times. At least in recent years, most researchers have understood that this was largely a natural phenomenon and that human sources of nitrogen played a small role, if any, during a fish kill.

The question still being debated is how much (or how little) humans contribute to the low-oxygen level in the water that is pushed to the surface during a fish kill and whether there is a significant flow of low-oxygen water out of Lower Hood Canal, where oxygen conditions are often deadly at the bottom.

The new report, which was reviewed by experts from across the country, concludes that fish kills can be explained fully without considering any human sources of nitrogen. Evidence that low-oxygen water flows out of Lower Hood Canal in the fall is weak, the report says, though it remains a subject of some debate.

“We have not demonstrated that mechanism to their satisfaction,” Jan Newton of the Hood Canal Dissolved Oxygen Program told me in an interview. “We never said it caused the fish kill, only that it can reduce the oxygen level below what it was. In some years, it wouldn’t matter, but in some years it would make it worse.”

A cover letter (PDF 83 kb) to the EPA/Ecology reports includes this:

“While the draft report concludes that although human-caused pollution does not cause or contribute to the fish kills near Hoodsport, our agencies strongly support additional protections to ensure that nitrogen and bacteria loadings from human development are minimized.

“Water quality concerns extend beyond low dissolved oxygen and include bacteria and other pathogens that limit shellfish health. Overall, human impacts to Hood Canal water quality vary from place to place and at different times of year. Hood Canal is a very sensitive water body and people living in the watershed should continue their efforts to minimize human sources of pollution.”

One of the most confounding factors is the large amount of nitrogen born by ocean water that flows along the bottom of Hood Canal. An unresolved but critical questions is: How much of that nitrogen reaches the surface layer, where it can trigger plankton growth in the presence of sunlight?

Plankton growth is a major factor in the decline of oxygen levels, because plankton eventually die and decay, consuming oxygen in the process.

Human sources of nitrogen often enter Hood Canal at the surface, but researchers disagree on how much of the low-oxygen problem can be attributed to heavy seawater that reaches the sunny euphotic zone near the surface.

Here are the principal findings in the EPA/Ecology report, “Review and Synthesis of Available Information to Estimate Human Impacts to Dissolved Oxygen in Hood Canal” (PDF 3.8 mb).

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You, too, can observe oxygen changes in Hood Canal

I’m becoming something of a nerd when it comes to oxygen levels in southern Hood Canal. I’m sure it stems from the realization that we now have the technology to predict when fish will react to low-oxygen conditions by swimming to the surface, acting sluggish and sometimes dying.

Wolf eels at Sund Rocks in Hood Canal are disturbed by low-oxygen conditions.
Photo courtesy of Pat Lynch

In a story published in Monday’s Kitsap Sun, I took a step back from the immediate low-oxygen conditions and discussed our knowledge of Hood Canal, along with plans being formulated to address the low-oxygen problem.

Low-oxygen conditions reared their ugly head during the last week in September (Water Ways, Sept. 27). No major fish kills were reported before things began to improve somewhat by Friday (Water Ways, Sept. 30).

I’m keeping my eye on the charts and graphs and noticed a couple things that we can talk about. Compare the two oxygen profiles below with an eye to the surface conditions at Hoodsport (blue line) and deeper waters there below 40 meters.

Oxygen profile from Sept. 30
Oxygen profile today (Oct. 5)

The first thing I noticed was that the top of the hypoxic layer moved up from about 17 to 10 meters. That means if fish are avoiding that low-oxygen water, they will also move up. As far as I know, divers have not reported any observations to confirm or deny that change. One explanation is that the heavy ocean layer at the bottom is pushing up the entire water column. It also could mean that the surface layer has grown thinner, such as when south winds blow or north winds stop.

Meanwhile, the bottom of that middle hypoxic layer has moved up from about 70 to 50 meters and the edge has smoothed. That is an indication that the heavy ocean water, which contains more oxygen, is mixing with the bottom of the hypoxic layer.

One may also notice that the deep water at Twanoh (turquoise line) has become more oxygenated all the way through and is sharply higher in oxygen at the bottom. Perhaps this is an indication that the heavy ocean water has reached Twanoh and is mixing at the bottom, while winds and tides mix the water at the top.

University of Washington oceanographer Jan Newton has noticed a decline in the oxygen concentration in the middle layer at Hoodsport. She raises the prospect that this could result, in part, from low-oxygen water being pushed back from Lower Hood Canal by the annual intrusion of heavy ocean water. It needs to be checked further, she said.

I hope we get some diver observations this weekend or sooner. In discussing the current conditions with Dan Hannifious of Hood Canal Salmon Enhancement Group, we both wondered when deep-water fish will move back to their normal depth. What would it take for them to break through the middle low-oxygen layer to reach deeper water that is higher in oxygen.

If you would like to become an armchair observer of these conditions in Hood Canal, check out the graphs on the website of the Hood Canal Dissolved Oxygen Program. You’ll have to save old graphs to compare them closely, although another graph on the Nanoos website shows you changes in oxygen levels and other parameters over time for selected depths. (Click on “Regions” then “Puget Sound” and locate the Hoodsport buoy to find the graphs.)

Will the conditions in Hood Canal get better or worse this year? I’ll let you know, but if you see something unusual, feel free to post a comment here.

Oxygen levels improve in Hood Canal past few days

Fish and other sea creatures are finding some room to breathe in southern Hood Canal as higher oxygen levels have returned to the upper portion of the waterway after things looked pretty bleak on Monday. See Water Ways post.

I reported yesterday that fish could safely go down to 60 feet in a story posted on the Kitsap Sun website, but conditions are changing all the time. Now it looks like the cutoff depth is closer to 50 feet, while waters closer to the surface appear to be more oxygenated than yesterday.

I discussed the situation with Dan Hannifious of the Hood Canal Salmon Enhancement Group and included some of Dan’s comments in the story. Rather than repeat those comments here, I’ll let you click on the story.

What I did want to share are a couple graphs that show current conditions as of 9:30 this morning. Most of the real-time analysis comes from monitoring buoys in Hood Canal.

This is a profile of the oxygen levels from the surface down to the bottom of Hood Canal, or close to it. The blue line is for the Hoodsport buoy, turquoise for Twanoh and green for Dabob Bay. The black line is for Carr Inlet in South Puget Sound and purple is Point Wells near Edmonds. Biological "stress" occurs at less than 5 milligrams per liter, while "hypoxia" is shown at 2 mg/l. At Hoodsport, if fish go below about 18 meters, they will be in hypoxic conditions. Earlier this week, these condition were seen at the surface.
Data from the Hood Canal Dissolved Oxygen Program.
This graph shows changes over time. While conditions have gotten better near the surface (blue line), it doesn't show much change at 66 feet (green line). As we can see in the previous graph, the changes are occurring in shallower water and will take time to reach this depth. The red line shows the intrusion of heavy seawater containing more oxygen. When comparing, remember one graph uses meters, the other feet.
Data compiled by the Integrated Ocean Observing System

Oxygen in Hood Canal bounces back overnight

UPDATE: Sept. 24, 2010

Conditions have remained pretty much the same the last couple of days, although the intrusion of dense higher-oxygen water from the ocean is beginning to create a thicker layer at the bottom of Hood Canal. The middle layer of low-oxygen water remains fairly thick, but the upper layer with higher oxygen concentrations is still providing fish some relief. South winds remain a threat, as I’ve explained for the last few weeks.

One can observe the three layers in the upper graph. The lower graph shows changes over the past week or so. Notice how oxygen concentrations are rising in the deep layer.
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Fish kill reported in southern Hood Canal

UPDATE: 9-21-2010, 11:35 a.m.

Low-oxygen conditions grew worse overnight. Lots of Hood Canal residents are reporting dead fish and spot prawns on beaches in southern Hood Canal. I’ve posted an update on the Kitsap Sun’s website.

Here are some graphics of the oxycline and time changes, courtesy of Jan Newton.
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Report notes oxygen troubles in Northwest waters

Low-oxygen problems in Hood Canal and along the Washington-Oregon Coast are highlighted as “case studies” in a new federal report regarding the growing number of “dead zones” across the United States. See “Scientific Assessment of Hypoxia in U.S. Coastal Waters” (PDF 2.7 mb).

Incidents of hypoxia have increased 30-fold since 1960, according to the report. The new federal review describes the causes of hypoxia, discusses past and ongoing research efforts and lays out policy recommendations to deal with the problem. Eight troubled waterways are reviewed as “case studies.”

In a news release (PDF 116 kb) accompanying the report, Jane Lubchenco, administrator of the National Oceanic and Atmospheric Administration, offered these comments regarding hypoxia and the seasonal low-oxygen area off the coast of Washington and Oregon:

“The report shows good progress on research into the causes of hypoxia and the specific management requirements to restore systems such as the Gulf of Mexico and Chesapeake Bay, but we still have a long way to go to reduce this environmental threat. The discovery of a new seasonal hypoxic zone off the coast of Oregon and Washington that may be linked to a changing climate emphasizes the complexity of this issue.”

That West Coast dead zone is now ranked the second largest in the United States and the third largest in the world. Federal officials say there may be serious consequences to the ecological health of the region.

Lisa Jackson, administrator of the Environmental Protection Agency, said the EPA is proud to have played a role in the research leading up to the report:

“These growing dead zones endanger fragile ecosystems and potentially jeopardize billions of dollars in economic activity. This science can be the foundation for measures that will preserve our waters and reverse the trend, including innovative, watershed-based solutions to this challenge.”

Mike Lee, a reporter with the San Diego Union-Bulletin, interviewed Tony Koslow, who studies low-oxygen areas at the Scripps Institution of Oceanography.

“This is a large phenomenon not due to nutrient outflows” from land, Lee quoted Koslow as saying. “The big question is, ‘Is this due to climate change?’ ”

As the oxygen-rich surface layers warm up, they mix less with colder layers down deep where oxygen levels are low, Koslow said. Global climate models predict that the oxygen levels in deep oceans will decline 20 to 40 percent the next century.

“There are substantial ecosystem concerns,” Koslow said. “A number of species that live in the deep ocean are very sensitive to changes in oxygen levels. These species — although they are not of commercial interest — are prey to squid, fish, marine mammals and seabirds, so changes in oxygen will have repercussions throughout the food web.”

The report suggests these policy actions:

  • Develop and implement cost-effective and scientifically
    sound nutrient reduction strategies to achieve healthy water
    quality in rivers, lakes and coastal waters.
  • Improve ecosystem models to assess how hypoxia
    affects commercially important fish populations in order to
    refine management strategies to protect coastal economies.
  • Improve scientific understanding for emerging sites such
    as the Oregon and Washington shelf, where hypoxia may be
    driven primarily by events linked to climate change. This
    knowledge will help managers mitigate impacts on natural
    resources and coastal economies.
  • Expand stream and river monitoring to document extent
    and sources of nutrients and progress in achieving management
    goals. This can lead to more strategic and effective targeting of
    nutrient reduction actions.
  • More systematically monitor oxygen levels in coastal
    waters using new technologies and observing systems. This is
    critical for forecast model development, fisheries management,
    and determining nutrient reduction success.