This entry is part of a series that describes my participation in the Cook Inlet Beluga Monitoring Citizen Science Project
Sunday September 1, 2019.
Anchorage Small Boat Launch.
The trio of tugs sortie from the float adjacent to the small
boat ramp toward the Anchorage wharves as I arrive to begin my two-hour shift
scanning the waters of the Cook Inlet for beluga whales. I surmise the vessels will assist the impending
departure of the blue Tote Maritime Lines cargo ship. Today’s session is one of many over the next
three month in the citizen science project to catalog the presence and behavior
of beluga under the auspices of the Beluga Whale Alliance and the Alaska Beluga
Whale Monitoring Program. The observation period begins in a few minutes at
5:00 p.m. This is my fourth session in eight days at this location and I have
yet to spy anyone of the critters. Harbor
seals have been viewed regularly, but thus far no beluga. Maybe today will be the day!
Scanning the coastline reveals the physical environment in
which today’s monitoring occurs. Launching
anything from the boat ramp would be impossible given the gap between the base
of the ramp and water’s edge. The tugs move slowly into the industrial port
immediately to the north. A bit closer,
the deep furrow through the grey mud that marks the mouth of Ship Creek lies
well above the waterline. The adjacent tidal flats appear littered with fallen
tree trunks and root balls—the water-worked remains of once living trees
deposited by the eroding shoreline or washed down waterways that enter into the
Inlet. In the next two hours, the
incoming tide will fill the boat ramp, inundate the creek channel and cover
most of the surrounding tidelands, which when exposed is a mud slurry best described
as “part water, part glacial till, punctuated by exposed channels and dead
trees.”
In Cook Inlet, the tide does not so much “rise” as it does
“flow” or “flood” On this day, as shown by the graph from the Tides4Fishing
website, the second of the two low tides that day was three-quarters of an hour
earlier at -4.0 feet. The next high tide
will be at 9:44 p.m. at 33.0 feet, a change of 37 feet in 5 ½ hours--a lot of
water movement. These levels are not
quite the maximum low tide for Anchorage of -5.6 feet and a maximum high of
34.4 feet, but pretty close. The tidal
coefficient in red at the top of the chart indicates the likelihood of major
currents and fish movements upstream on the incoming tide—two features which
factor into beluga behavior.
The United States
Coast Pilot 9 for the vicinity of Anchorage helps put into context what I
am seeing:
“Close off the town,
the current floods northeast at a velocity of 1.5 knots and ebbs southwest at a
velocity of 2.5 knots. One mile off the town, the current averages 2.9 knots.
Strong currents that attain velocities of 4 knots or more, at times, in
midchannel, and swirls in the area make navigation difficult. It is reported
that the flood following the higher of the low waters is unpredictable,
especially during the last 3 hours, in the vicinity of the Port of Anchorage
wharves.”
The energy of moving this water volume is evident as the
dead trees lift with the rising tide and entrain in the tidal rips moving
quickly past out observation point. Each
draws our attention, as any out of the ordinary movement on the water is likely
to do when scanning for beluga. Binoculars
on the target confirm it is a submerged log; one of many we see that day. It seems a collision between a boat and the
log would leave the boat much worse off from the encounter. In some cases, when the log may float near
vertical, it would appear that the cryptid Loch Ness monster resides in the
Inlet as well as the beluga.
These conditions are conducive to observing beluga. According to NOAA’s 2016 Cook Inlet Beluga
Recovery plan “habitat use in the summer months consists of semi-predictable
movements of groups of belugas between river mouths and shallow tidal flats in
the upper Inlet. These movements are largely cued to physical conditions,
especially tide…. Traditional ecological knowledge indicates that daily
movements are determined by the ebb and flow of the tide and the related
movements and size of fish runs,...”
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