Print this page

Charles Nittrouer

Recent Publications and Manuscripts in the Press

In Press

K.V. Boldt, C.A. Nittrouer, B. Hallet, M.N. Koppes, B.K. Forrest, J.S. Wellner, and J.B. Anderson, Modern rates of glacial sediment accumulation along a 15o S-N transect: in fjords of the Antarctic Peninsula and southern Chile, Jour. Geophys. Res. Earth Surface


C.A. Nittrouer, B. Raubenheimer and R.A. Wheatcroft, Lessons learned from comparison of mesotidal sand- and mudflats, Cont. Shelf Res., 33, (2013).

K.V. Boldt, C.A. Nittrouer and A.S. Ogston, Seasonal transfer and net accumulation of fine sediment on a muddy tidal flat: Willapa Bay, Washington, Cont. Shelf Res., 33, (2013).

K.L. Webster, A.S. Ogston and C.A. Nittrouer, Delivery, reworking and export of fine-grained sediment across the sandy Skagit River tidal flats, Cont. Shelf Res., 33, (2013).

C.A. Nittrouer, B. Raubenheimer, and R.A. Wheatcroft (eds), Hydrodynamics and sedimentation on mesotidal sand- and mudflats, special issue, Cont. Shelf Res., 33 (2013)

J.P. Walsh, D.R. Corbett, A.S. Ogston, C.A. Nittrouer, S.A. Kuehl, M.A. Allison, and S.L. Goodbred, Shelf and slope sedimentation associated with large deltaic systems, in T.S. Bianchi, M.A. Allison, and W.-J. Cai (eds) , Biogeochemical Dynamics at Large River-Coastal Interfaces: Linkages with Global Climate Change, Cambridge University Press, Cambridge (2013).

R.P. Hale, C.A Nittrouer, J.T. Liu, R.G. Kiel and A.S. Ogston, Effects of a major typhoon on sediment accumulation in Fangliao submarine canyon, SW Taiwan, Mar. Geol. 326-328, 116-130, (2012)

S.J. Bentley and C.A. Nittrouer, Accumulation and intense bioturbation of bioclastic muds along a carbonate-platform margin: Dry Tortugas, Florida, Mar. Geol., 315-318, 44-57, doi:10.1016/j.margeo.2012.05.002 (2012)

R. Aalto and C.A. Nittrouer, 210Pb geochronology of flood events in large tropical river systems, Phil. Trans. Royal Soc., 370, 2040-2074, doi:10.1098/rsta.2011.0607 (2012)

C.M. Palinkas, A.S. Ogston, and C.A. Nittrouer, Observations of event-scale sedimentary dynamics with an instrumented bottom-boundary-layer tripod, Mar. Geol., 274, 151-164 (2010).

T. Tesi, M.A. Goni, L. Langone, P. Puig, M. Canals, C.A. Nittrouer, X.D. de Madron, A. Calafat, A. Palanques, S. Heussner, M.H. Davies, T.M. Drexler, and J. Fabres, Reexposure and advection of 14C-depleted organic carbon from old deposits at the upper continental slope, Global Biogeochem. Cycles, 24, GB4002, doi:10.1029/2009GB003745 (2010).

J.P. Walsh and C.A. Nittrouer, Understanding fine-grained river-sediment dispersal on continental margins, Mar. Geol., 263, 34-45 (2009).

Current Research Interests

Hydrodynamics and sedimentation in tidal rivers

Intertidal sedimentation (tidal flats and mangrove forests)

Impacts of dam removal on coastal sedimentation

Tropical river deltas (Amazon and Mekong)

Tidewater glaciers impacting fjord circulation and sedimentation

Current C.V. URL

In the News

Tracking sediments' fate in largest-ever dam removal

Salmon are beginning to swim up the Elwha River for the first time in more than a century. But University of Washington marine geologists are watching what's beginning to flow downstream – sediments from the largest dam-removal project ever undertaken.
The 108-foot Elwha Dam was built in 1910, and after decades of debate it was finally dismantled last year. Roughly a third of the 210-foot Glines Canyon Dam still stands, holding back a mountain of silt, sand and gravel.
Removal of the upper dam was halted in January while crews repair a water-treatment plant near Port Angeles that got clogged with leaves and other debris. For engineers, this phase may be the trickiest part of the dam-removal project. For oceanographers, "the best is yet to come," said Charles Nittrouer, a UW professor of oceanography and of Earth and space sciences.
It turns out there is even more sediment than originally thought – about 34 million cubic yards. That's more than 3 million truck loads, enough to bury all of Seattle in a layer almost 3 inches thick.
Aerial photos show sediment starting to fan out around the river's mouth.
"One of the risks of just looking at these beautiful plume pictures is that you really don’t know the extent of where that sediment actually ends up," said Andrea Ogston, a UW associate professor of oceanography. "Our focus is looking at what's happening very close to the seabed – how it's going to move, where it's going to get to, what's its ultimate fate."
For the past five years, Ogston and Nittrouer and their students have been studying the sediment around the river mouth, initially with the support of Washington Sea Grant, to understand the condition before the dams' removal. Their current project, funded by the National Science Foundation, is looking for events that could act like a hundred-year storm and bury the sediment deep in the ocean.
The UW researchers have instruments to track particles in the water and record them accumulating on the ocean floor. They are on high alert for a rapid response when the river floods and dislodges the sediment. When that happens, they want to be onsite to record as much data as possible – and perhaps be the first to witness a rare geologic event.
In nature, deep-sea sediment flows triggered by earthquakes or extreme storms can be important for creating oil reserves and other geologic deposits, as a component of the global carbon cycle, and responsible for burying communication cables.
Computer models and the geologic record suggest that when the sediment is in high-enough concentrations, it goes directly to the ocean floor. Instead of the fresh river water floating on top of the seawater, the river water becomes denser than the sea, and the sediment-laden river water plunges below the ocean water.
For the Elwha, that path would take much of the sediment away from the coastline and deep into the Strait of Juan de Fuca.
"A surface plume is very much at the whim of the winds and tides, whereas these underflows are just going down the steepest gradient," Ogston said. "These are two very different mechanisms that would create very different impacts to the seabed."
The dams initially powered a pulp mill and were built unusually close to the ocean – the upper dam is just 13 miles from the river mouth. Their removal provides a unique opportunity to study large river discharges.
"There is an understanding of the general type of flow, and people have predicted that it occurs in rivers, but no one has seen the smoking gun yet," Nittrouer said. "This is a chance to document a 100-year storm. It's really somewhat new territory."
So far there have been dramatic changes to the seabed in the shallows, but few changes below about 20 feet, Ogston said.
Where the sediment ends up is of practical interest. Sediment can make the water murky, creating conditions that make it difficult for salmon to lay eggs, or block light from reaching algae and other life on the ocean floor. On the other hand, the sediment also has positive impacts. Many people hope that removing the dam will help with erosion along the Olympic Coast. The new sediment could accumulate and restore natural beaches on the bluffs near Port Angeles.
A better understanding of sediment transport could also help determine the timing of future dam removals.
"One of the arguments is that rather than having a river that’s unacceptable to salmon for many years, you can accelerate the erosion to flush the system. That way you have two or three really bad years instead of two or three pretty bad decades," Nittrouer said. Future projects might be trickier, he added, if the sediments contain pesticides or other chemicals.
Nobody knows when the Elwha's sediment mother lode will begin to shift. A heavy rainfall combined with spring melt could dislodge the heap; if not, next fall and early winter rains will do the job. Either way, the UW marine geologists will be ready to hop in their van, hitch up a boat, and race out to see what happens.
"This is a very exciting time," Ogston said.