Check out this great video from UW's Applied Physics Lab
to learn how our network of ORCA (Oceanic Remote Chemical Analyzer)
buoys has helped scientists track the "blob" and it's effects in local
waters, including fish kills in Hood Canal.
From Jan Newton, Allad Devol and Wendi Ruef, University of Washington:
A fish kill occurred in late August in Hood Canal, documented by observations from the Skokomish Tribe and by ORCA buoy oxygen measurements by the University of Washington. The fish kill was most severe on 29 August, but with stress and some mortality observed both before and after.
Seth Book and others from the Skokomish Tribe DNR observed thousands of dead fish and crab on Friday, which was covered by the media. On Saturday-Sunday, we anticipated even more fish kill, due to sustained southerly winds, but the lowest oxygen waters stayed deep, below ~10 m. Videos show the fish and crabs confined to a narrow surface layer, which maintained sufficient oxygen.
A couple things to clarify from the media reports:
- Worst year? The low oxygen levels in southern Hood Canal were the most extreme we have measured, even worse than in 2006 and 2010. However, the fish kill events in 2003, 2006 and 2010 appear to have been worse than this year, at least so far.
- Blob effect? The effect of the blob (warmer than typical NE Pacific ocean waters) was last fall, when the ocean waters entering Puget Sound were warmer (less dense) and did not flush the southern reach of Hood Canal. The year 2015 started with hypoxic waters in southern Hood Canal. The blob, still offshore now, is not affecting current conditions. Strong coastal upwelling during June is what is flushing Hood Canal now. This seasonal intrusion started about a month earlier than normal, which is lucky because oxygen conditions would have worsened until the flushing started.
Oxygen conditions in Hood Canal appear to be improving as flushing continues. Conditions today at Hoodsport show the entire water column is above hypoxic levels; at Twanoh there is severe hypoxia (less than 1 mg/L) at 10 m depth, but the deepest waters now have oxygen concentrations above this.
Visit ORCA and NANOOS for more information on hypoxia in Washington waters.
Okay, so no one says that but they might as well... I mean, whoever heard of a
body of salt water this far from the poles freezing? That’s what was
going through my head as I drove our 20’ aluminum boat into the icy sheet last
winter.
It started out as a normal, albeit cold, field day for the
Oceanic Remote Chemical Analyzer (ORCA) team. We launched the M/V
Mackinaw at Twanoh State Park and drove out to our research buoy in Lynch Cove
to replace the CTD package and repair the winch control box. We thought
we were prepared for a cold day on the water, armed with extra layers, beanies,
scarves and multiple pairs of wool socks, but then the snow started. I
always seem to forget how difficult it is to do precise, mechanical work on
cold metal instruments with cold metal tools, while constantly being splashed
by cold, cold water. The work was taking much longer than anticipated
with all of this cold on cold. When we eventually finished the required
maintenance I pointed the boat toward the ORCA Hoodsport buoy where we were
scheduled to work on the router. As we turned around Sisters Point I
noticed a definite line on the water surface ahead of me. “Weird, that looks
just like…” CRUNCH!!!
Standing on the bow of the M/V Mackinaw as we try to push
our way through the ice
Before I could even finish my thought we were startled with a sudden crash as the Mackinaw tried pushing through a sheet
of ice.I slowed down and carefully
backed us out through the path we had just cut, and then motored along the
margin to see if there was any way through.No luck.A flock of seagulls
stood on the ice and watched us while we made a call and sent photos to our incredulous
supervisor at the University of Washington.There was no way we’d be able to continue.We couldn’t see the end of the ice sheet and
even if we made it through we’d lose too much daylight to get any work done.After a few more minutes playing with the chunks
of ice that had broken free of the sheet, we headed back to Twanoh to get our
boat out of the cold water.
Snapping some photos while we wait for confirmation to call
it a day
Encountering ice in Hood Canal surprised our group but
apparently it’s not that strange.Fresh water
that flows from the Skokomish River into Hood Canal tends to float on top of
the denser salt water, creating a thin fresh layer.When temperatures drop this layer can freeze,
just like any body of fresh water.If
temperatures stay low for long enough, the ice sheet can reach from shore to
shore like we witnessed... I’ve even heard stories of people driving wagons
across the canal in previous centuries!
