NOAA's Response and Restoration Blog

An inside look at the science of cleaning up and fixing the mess of marine pollution

NOAA Tracks Path of Possible Japan Tsunami Dock off Washington Coast

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This is a post by Amy MacFadyen, oceanographer and modeler in the Office of Response and Restoration’s Emergency Response Division.

A dock washed up on the rocky northern coast of Washington.

The dock washed up on the rocky northern coast of Washington state, as viewed from a U.S. Coast Guard helicopter on December 18, 2012. (U.S. Coast Guard)

As a NOAA oceanographer working in pollution response, part of my job is to predict where pollutants (mostly oil) spilled into the ocean will end up. Sometimes I am asked to forecast possible paths, or trajectories, for other objects spotted at sea—such as a large dock recently reported to be floating off the coast of Washington state, approximately 16 nautical miles northwest of Grays Harbor.

We suspect [Editor’s note 1/18/13: Japan has confirmed this as a piece of tsunami debris.] that this dock began its oceanic journey in March of 2011 at the Port of Misawa, Japan, following the devastating Tōhoku earthquake and subsequent tsunami. Three* docks were ripped away from this port.  After approximately 15 months at sea, one of the docks turned up on Agate Beach near Newport, Ore., in June 2012. A second dock suspected** to be from Misawa was spotted offshore of the Hawaiian Islands in September. The vast difference in the paths of these three docks is a good illustration of how turbulent ocean currents and winds can scatter widely objects floating at sea.

When this latest dock was spotted on Friday, December 14, we at NOAA were asked to forecast where winds and currents might move the dock over the next few days. The dock is a large, unlit, concrete structure and hence posed a significant hazard to navigation. Furthermore, with stormy weather and strong onshore winds in the forecast, it seemed likely the dock would end up on the beach. Many beaches along the northern Washington coast are quite remote, varying from sandy or rocky beaches to cliffs dropping right down to the water. Depending on where the dock came ashore, access could prove difficult and might allow possible invasive species hitching a ride on the dock time to spread into local ecosystems. To be better prepared to take action, we needed to know where and when the dock might come ashore so it could be located quickly.

In order to predict the trajectory of an object floating at sea, we require forecasts of winds and ocean currents. Those of us who live in the Pacific Northwest are especially familiar with the difficulty involved in predicting the weather. Although weather forecasts are generally reliable for the first few days of a forecast period, a forecast always contains some uncertainty which tends to increase over time. For example, this weekend’s weather forecast is generally more accurate than next weekend’s forecast.

Forecasting ocean currents faces similar difficulties, which may be compounded by a lack of observations. There are few (if any) direct measurements of real-time ocean currents on the Washington coast. In addition, there is further uncertainty about how a floating object such as a large dock will move in response to the currents and winds. For example, an object that is floating high in the water will “feel” the winds more than an object floating lower in the water. While we could estimate this effect for the dock, it adds another source of uncertainty to the mix.

Map of the northern Washington coast shows projected and actual locations of the dock.

This map of the northern Washington coast shows an example output from the GNOME model for the predicted “best guess” area (red ellipse) and uncertainty boundary (blue ellipse). The location where the dock was found is shown by the black arrow. (NOAA)

So what can we do with all this uncertainty when “I don’t know” is not an acceptable answer? The approach we took was twofold. In addition to providing a “best estimate” trajectory for the dock, in which we considered the wind and currents forecasts as truth, we also ran multiple scenarios in our trajectory model to determine where else the dock possibly could end up. These additional scenarios might use different values approximating how much the dock gets pushed along like a sailboat or they might adjust the wind and current forecasts slightly to see how this affects the projected path of the dock.

After running the trajectory model multiple times, we produced a map that indicated the most likely area that the dock would come ashore, but the map also included a larger area of uncertainty around it (an “uncertainty boundary”) where the dock might be found if, for example, the currents were stronger than predicted.

Because the dock was not spotted again after the initial report on December 14, our trajectory could only narrow down the search area to an approximately 50 mile stretch of the Washington coast (remember, forecast error grows with time).

However, using the forecast guidance, state, federal, and tribal representatives mobilized search teams, and the dock was located on the afternoon of December 18 by a Coast Guard helicopter aerial survey. The dock had been washed ashore, most likely sometime during the evening before, on a rugged stretch of coastline north of the Hoh River. Access to the region is difficult, but personnel from the National Park Service and Washington State Fish and Wildlife are attempting to reach the dock to sample it for invasive species and to attach a tracking buoy in case it refloats before it can be salvaged.

Here you can see an example animation of our trajectory model GNOME showing a potential path of the dock. Particles are released in the model at the position where the dock was initially sighted. The particles move under the influence of winds and ocean currents. They also spread apart over time; this is simulating the small-scale turbulence in the winds and currents. This particular scenario was run after the dock was stranded and uses observed winds from a nearby weather station (wind direction and strength is shown by the arrow on the upper right) and a northward coastal current of approximately 1 knot.

Download the video animation showing the potential path of the dock off the coast of Washington [Quicktime].

*[UPDATE 4/5/2013: This story originally stated that four docks were missing from Misawa, Japan and that “one of the four turned up several weeks later on an island south of Misawa.” We now know only three docks were swept from Misawa in the 2011 tsunami, and none were found on a Japanese island.]

**The dock near Hawaii has not been confirmed by the Japanese Consulate as being from Misawa.

Amy MacFadyen

Amy MacFadyen

Amy MacFadyen is a physical oceanographer at the Emergency Response Division of the Office of Response and Restoration (NOAA). The Emergency Response Division provides scientific support for oil and chemical spill response — a key part of which is trajectory forecasting to predict the movement of spills. During the Deepwater Horizon/BP oil spill in the Gulf of Mexico, Amy helped provide daily
trajectories to the incident command. Before moving to NOAA, Amy was at the University of Washington, first as a graduate student then as a postdoctoral researcher. Her research examined transport of harmful algal blooms from offshore initiation sites to the Washington coast.

Author: Office of Response and Restoration

The National Ocean Service's Office of Response and Restoration (OR&R) provides scientific solutions for marine pollution. A part of the National Oceanic and Atmospheric Administration (NOAA), OR&R is a center of expertise in preparing for, evaluating, and responding to threats to coastal environments. These threats could be oil and chemical spills, releases from hazardous waste sites, or marine debris.

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