The last few
weeks provided us with some great conditions for field work, followed by this
final week of dense fog allowing us to spend time in doors organizing and studying
the data. A few of our days out in the
field we were lucky to get close to some of the resident gray whales that feed
along the rocky shoreline outside of Sunset Bay. I was surprised to see the whales so close to
the rocks, with a few we saw appearing to be right up against some very shallow
outcroppings, as if they were scratching their sides on the rocks! I was told later that they were feeding on
mysid shrimp found in the kelp beds, a behavior that the resident whales have
adapted to the local habitat.
We were able to get three days of field work
in the week of the 25th along with a set of plankton samples on a day the front
was clearly present at Sunset Bay. It
will be exciting to see how are samples differ from each other. Samples were taken shoreward of the foam line
at three different depths including the surface, offshore of the foamline at
the same depths, and within the foamline
at the surface. Up until now I
wasn’t sure of what the cause of the
foam along the front was but was surprised when told that it is due to the
release of lipids from certain plankton when they breakdown. The break down of these organisms can
actually be caused by the forces created at the front between the two water
masses and also along the rocks where wave disturbance causes a lot of
breakdown, producing large amounts of foam.
On the week of the 6th winds had shifted to the south for a few days, giving us the chance to do some field work during downwelling favorable winds. We were surprised to see that a foamline was still present and it was the first time that our drogues at 5.5 meters depth both traveled offshore, with the inshore drogues crossing the foam line.
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