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SSM Sediment Transport: Swinomish Channel

Sediment Transport into the Swinomish Navigation Channel, Puget Sound

Study area showing Swinomish Navigation Channel near the mouth of Skagit River estuary, located in Whidbey Basin, Puget Sound, Washington. (A) North Dike, (B) McGlinn Island to Goat Island Jetty, (C) South Jetty, (D) McGlinn Island to Mainland causeway, (E) McGlinn Island.

PNNL supported U.S. ACE and the Skagit River System Cooperative with hydrodynamic and sediment transport modeling to evaluate the merits and demerits of proposed alternatives in connection with maintenance of the Swinomish Navigation Channel. The 11-mile Swinomish Federal Navigation Channel provides a safe and short passage to fishing and recreational craft in and out of Northern Puget Sound by connecting Skagit and Padilla Bays. A network of dikes and jetties were constructed through the Swinomish corridor between 1893 and 1936 to improve navigation functionality. Over the years, these river training dikes and jetties designed to minimize sedimentation in the channel have deteriorated resulting in reduced protection of the channel. The need to repair or modify dikes/jetties for channel maintenance however may be in conflict with salmon habitat restoration goals aimed at improving access, connectivity and brackish water habitat. A number of restoration projects have been proposed in the Skagit delta involving breaching, lowering, or removal of dikes.
(Left) The Skagit River estuary model grid with expanded domain covering Padilla Bay to the north and Saratoga Passage to the South with Swinomish Channel connecting the two basins. (Right) A close up of the model grid near the mouth of North Fork of Skagit River showing detailed definition of the dikes and jetties defining the Swinomish Navigation Channel.

To assess relative merits of two of the available alternatives, a hydrodynamic model of the Skagit River estuary was developed using the Finite Volume Community Ocean Model (FVCOM). The model development, grid refinement, and calibration were conducted using oceanographic data collected from the years 2006 and 2009 with a focus on the sediment and brackish water transport from the river and Skagit Bay tide flats to the Swinomish Channel. The model was applied to assess the feasibility of achieving the desired dual outcome of (a) reducing sedimentation and shoaling in the Swinomish Channel and (b) providing direct migration pathway and improved conveyance of freshwater into the Swinomish Channel. The potential reduction in shoaling through site-specific structure repairs was evaluated. Similarly, potential to significantly improve of brackish water habitat through restoration actions using the McGlinn Causeway project example along with its impacts on sediment deposition in the Swinomish Navigation Channel were examined.
Modified model configuration used for (Left) SCN-1 South Jetty Repair and (Right) SCN-2, McGlinn Causeway Restoration. Note – color contours indicate depths (negative elevations) relative NAVD88 datum.

Time averaged total suspended sediment (TSS) distribution (20 days) for (left) baseline conditions and (right) McGlinn Causeway restoration, SCN-2.

Project Highlights

Contacts and Project Team

Tarang Khangaonkar, Salish Sea Modeling Center
Adi Nugraha, PNNL
Steve Hinton, Skagit River System Cooperative
David Michalsen and Scott Brown, U.S. Army Corps of Engineers


Khangaonkar T, A Nugraha, S Hinton, D Michalsen, S Brown. 2017. Sediment Transport into the Swinomish Navigation Channel, Puget Sound – Habitat Restoration versus Navigation Maintenance Needs. Journal of Marine Science and Engineering 5(2): 1-22 doi: 10.3390/jmse5020019.

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