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Main Introduction Methods Results & Discussions Data Repository


Introduction
The Puget Sound is a fjord type estuary divided into four main basins. Located in the main basin of Puget Sound is Quartermaster Harbor, a bay inside the Vashon-Maury Island that consists of 3,000 acres of water surface area with a depth of 5-6 meters in the inner harbor and 11-46 in the outer harbor. The largest contribution of fresh water comes from Judd Creek located in the inner harbor. At the entrance of the bay lies a sill which is followed by a steep drop off which can be seen in the surfer plots on the results and discussions page (King County 2014). Due to the enclosed geography of the inner bay to Quartermaster Harbor, flushing rates vary from 20 to 100 days whereas the outer harbor can be anywhere from 10 to 40 days (Alberston 2013).

The low flushing rate, combined with anthropogenic nutrient sources and the resulting high concentration of phytoplankton, contributes to the high level of stratification in the harbor (King County 2014).  Following spring blooms, decomposition of phytoplankton on the harbor bottom rapidly depletes dissolved oxygen, creating a eutrophic system. The sediment of Quartermaster Harbor has also been shown to have easily the highest concentration of Alexandrium cantenella cysts in Puget Sound (Horner et. al 2011). When motile, this dinoflagellate produces a toxin that is a major contributor to paralytic shellfish poisoning.

Captain: Bob Goodman Crew: Julie Masura, EJ Rauschl, Alison Dunn, Taylor Wesenberg, Rafi Azami, Shirley Low, Lauren Reetz, Richard Davis, Corey King, Brandon Spencer
qmh_stations



Stations

Name Landmarks Latitude (N) Longitude (W) Depth (m) Time (PDT) Sampling
50 Outer Harbor 47.318833 122.4729166 176 14:00 C,N,P,Z
51 Outside Mouth 47.33623 122.4787666 52 13:20 C,N,P,S
52 Mouth 47.35028 122.48333 20 12.46 C,N,P,S
53 Between Central Outer Harbor and Mouth 47.363133 122.48045 18 12:06 C,N,P,S
54 Centeral Outer Channel 47.378595 122.4673166 13.5 11:24 C,N,P,S
Dockton Dockton Dock 47.373126 122.4532783 6 11:01 C,N,P,S
55 Inner Channel 47.38396833 122.446866 15.42 10:18 C,N,P,S
56 Inner Harbor 47.3984583 122.448805 5.6 9:42 C,N,P,S

N-Nutrients, P-Phytoplankton, Z-Zooplankton, C-Chlorophyll, S-Sediments
*Microplastics tow in the Thea Foss Water Way.


Tides and Weather

The weather at the beginning of the trip to about 10am was overcast, wind, and slight sunbreaks. Some small amounts of rain around 10:30am. From 11-12am the wind persisted but the sun came out for some time. The rest of the trip was moderate to heavy rains with periodic wind increase.
tides2
http://tidesandcurrents.noaa.gov/
weeklyprecip


Acknowledgements:

Thank you Bob, the captain of the R/V Barnes, for the memorable day and the full fridge!


Works Cited:

Albertson S. 2013. Quartermaster Harbor Nitrogen Management Study. Hydrodynamic Model Report [Internet]. Seattle (WA): Washington Department of Ecology; [cited 2014 Jun 5]. Available from: https://fortress.wa.gov/ecy/publications/publications/1303026.pdf.

Horner RA, Greengrove CL, Davies-Volllum KS, Gawel JE, Postel JR, Cox AM. 2011 Spatial distribution of benthic cysts of Alexandrium catenella in surface sediments of Puget Sound, Washington, USA. Harmful Algae 11: 96-105.

King County. Quartermaster Harbor Nitrogen Management Study: Final Study Report [Internet]. 2014. Seattle (WA): King County, [cited 2014 May 3]. Available from: http://your.kingcounty.gov/dnrp/library/2014/kcr2528.pdf


Middle banner image by Pete Murray

http://www.komonews.com/weather/blogs/scott/50502497.html



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Webpage created by Corey King and Brandon Spencer on June 2014