Geologist Creek, near Hokitika, New Zealand

Noah P. Snyder

Associate Professor, Department of Earth and Environmental Sciences
Director, Environmental Studies Program
Boston College
140 Commonwealth Avenue
Chestnut Hill, MA 02467, USA

CV (pdf)

 

 

 

 

 

 

 

Research

Rivers are conduits for transport of fresh water, sediment and nutrients throughout the landscape. At the same time, rivers are vital pathways for the migration of aquatic species, such as salmon. My research focuses on understanding how rivers respond to changes, ranging from long-term variations in tectonics or climate to short-term shifts in management style or land use. I link measurements of channel morphology from high-resolution airborne lidar digital elevation models with field-based measurements of stream processes.

Controls on the morphology of rivers in response to deglaciation and land-use change

Field surveys in the Narraguagus River watershed (August 2008) and Sheepscot River (December 2006), Maine.

The New England landscape is rich with opportunities for studying geomorphic responses to changes in external forces. The region hosts a large human population and has undergone large-scale climate (late Pleistocene continental glaciation, Holocene transgression), geodynamic (post-glacial isostatic rebound) and land-use (deforestation and reforestation) changes. The challenge is studying fluvial processes in a landscape where relief and sediment supply bear the strong imprint of continental glaciation. Since I arrived at BC in 2004, I have developed a research program focusing on understanding the interrelated issues associated with Atlantic salmon habitat requirements, river restoration, and trajectories of channel change in northern New England. For this research, my students and I link measurements from high-resolution lidar digital elevation models with field measurements. In 2006, this work was funded by the National Fish and Wildlife Foundation Maine Atlantic Salmon Conservation Fund. In 2007, I received a National Science Foundation award for a project entitled CAREER: Land use, geologic and climatic controls on stream processes in northern New England using airborne laser swath mapping, funded by the Geomorphology and Land Use Dynamics program.

I am a member of the Penobscot River Science Steering Committee and a core network participant in the NSF-funded RCN: Diadromous Species Restoration Research Network (DSRRN).

Field workshop with students from Washington Academy and Boston College in the Narraguagus River watershed, Maine (May 2008).

Publications: Controls on New England river morphology

Armstrong, W.H.*, Collins, M.J., and Snyder, N.P., 2012, Increased frequency of low magnitude floods in New England, Journal of the American Water Resources Association, v. 48, n. 2, p. 306-320, doi: 10.1111 ⁄ j.1752-1688.2011.00613.x.

Snyder, N.P., 2012, Restoring geomorphic resilience in streams, in Church, M., Biron, P.M., and Roy, A., editors, Gravel-bed Rivers: Processes, Tools, Environments, John Wiley and Sons, Ltd., p. 160-164, doi: 10.1002/9781119952497.ch14.

Kasprak, A., Magilligan, F.J., Nislow, K.H., and Snyder, N.P., 2011, A lidar-derived evaluation of watershed-scale large woody debris sources and recruitment mechanisms: coastal Maine, USA, River Research and Applications, published online, doi: 10.1002/rra.1532.

Wilkins, B.C.*, and Snyder, N.P., 2011, Geomorphic comparison of two Atlantic coastal rivers: toward an understanding of physical controls on Atlantic salmon habitat, River Research and Applications, v. 27, n. 2, p. 135-156, doi: 10.1002/rra.1343.

Snyder, N.P. , 2009, Studying stream morphoogy with airborne laser elevation data, Eos, Transactions, American Geophysical Union, v. 90, n. 6, p.45-46, doi:10.1029/2009EO060001.

Snyder, N.P., Castele, M.R.*, and Wright, J.R., 2009, Bedload entrainment in low-gradient paraglacial coastal rivers of Maine, U.S.A.: Implications for habitat restoration, Geomorphology, v. 103, n. 3,p. 430-446, doi: 10.1016/j.geomorph.2008.07.013.

(*BC student co-authors.)

Links: Controls on New England river morphology

JAWRA editor's blog post on Armstrong et al. (2012): March 12, 2012.

BC Chronicle article about lidar mapping and Eos article: February 26, 2009. Other articles: EurekAlert; ScienceDaily.

BC Chronicle article about NSF CAREER award: March 15, 2007.

Predicted bed grain size on a river in Maine

Bed grain size predicted using a DEM-based model every 100 m on a segment of the West Branch Pleasant River, Maine (base is a lidar shaded-relief map; model information in Wilkins and Snyder, 2011).

 

Effects of dams and dam removal

Dams represent important breaks in the continuum of fluvial processes as they alter the flow of sediment, wood and water. Dams also present society with important environmental decisions because of their benefits (e.g., power generation, water storage, flood control) and costs (e.g., potential failure, maintenance costs, barrier to migrating aquatic species, changes in river habitats). Throughout the U.S., communities are making the decision to remove dams because they believe the costs exceed the benefits. This shift in river management motivates new research, both to aid in future decisions and to gain fundamental insight into watershed processes. I have several projects in New England that use the sediment stored behind dams as a natural laboratory. My students and I are studying sediment dynamics associated with the removal of the Merrimack Village Dam on the Souhegan River in southern New Hampshire. This work is funded by the NOAA Open Rivers Initiative. Dam removals provide opportunities to study large-magnitude channel changes over short intervals. Another aspect of this dam-related research was funded by a grant from the American Chemical Society Petroleum Research Fund, in which we used reservoir sediments as scale models for offshore depositional systems. Previously, I studied reservoir sedimentation rates and processes behind Englebright Dam in northern California, as part of the Upper Yuba River Studies Program.

Removal of the Merrimack Village Dam (left) and expsoure of impounded sediment (right, photo by Matt Collins) on August 6, 2008, Souhegan River, New Hampshire.

Publications: Dams and dam removal

Santaniello, D.J.*, Snyder, N.P., and Gontz, A.M., in press, Using ground penetrating radar to determine the quantity of sediment stored behind the Merrimack Village Dam, Souhegan River, New Hampshire, in GSA Reviews in Engineering Geology special volume, The Challenges of Dam Removals and River Restorations, accepted April 2011.

Pearson, A.J.*, Snyder, N.P., and Collins, M.J., 2011, River response to dam removal: the Souhegan River and the Merrimack Village Dam, Merrimack, New Hampshire, Water Resources Research, v. 47, doi:10.1029/2010WR009733.

Snyder, N.P., Wright, S.A., Alpers, C.N., Flint, L.E., Holmes, C.W., and Rubin, D.M, 2006, Reconstructing depositional processes and history from reservoir stratigraphy: Englebright Lake, Yuba River, northern California, Journal of Geophysical Research, v. 111, F04003, doi: 10.1029/2005JF000451.

Alpers, C.N., Hunerlach, M.P., Marvin-DiPasquale, M.C., Antweiler, R.C., Lasorsa, B.K., De Wild, J.F., and Snyder, N.P., 2006, Geochemical data for mercury, methylmercury, and other constituents in sediments from Englebright Lake, California, 2002, U.S Geological Survey Data-Series Report 2005-151, http://pubs.water.usgs.gov/ds151/, 95 p.

Curtis, J.A., Flint, L.E., Alpers, C.N., Wright, S.A., and Snyder, N.P., 2006, Use of Sediment Rating Curves and Optical Backscatter Data to Characterize Sediment Transport in the Upper Yuba River Watershed, California, 2001–03, U.S. Geological Survey Scientific Investigations Report 2005-5246, http://pubs.usgs.gov/sir/2005/5246/, 74 p.

Snyder, N.P., Rubin, D.M., Alpers, C.N., Childs, J.R., Curtis, J.A., Flint, L.E., and Wright, S.A., 2004, Estimating rates and properties of sediment accumulation behind a dam: Englebright Lake, Yuba River, northern California, Water Resources Research, v. 40, W11301, doi: 10.1029/2004WR003279.

Snyder, N.P. , Allen, J.R., Dare, C., Hampton, M.A., Schneider, G., Wooley, R.J., Alpers, C.N., and Marvin-DiPasquale M.C., 2004, Sediment grain-size and loss-on-ignition analyses from 2002 Englebright Lake coring and sampling campaigns, U.S. Geological Survey Open-File Report 2004-1080, http://pubs.usgs.gov/of/2004/1080/, 46 p.

Snyder, N.P. , Alpers, C.N., Flint, L.E., Curtis, J.A., Hampton, M.A., Haskell, B.J., and Nielson, D.L., 2004, Report on the May-June 2002 Englebright Lake deep coring campaign, U.S. Geological Survey Open-File Report 2004-1061, http://pubs.usgs.gov/of/2004/1061/, 32 p., 10 plates.

Snyder, N.P. , and Hampton, M.A., 2003, Preliminary cross section of Englebright Lake sediments, U.S. Geological Survey Open-File Report 03-397, http://geopubs.wr.usgs.gov/open-file/of03-397/, 1 plate.

Childs, J.R., Snyder, N.P., Hampton, M.A., 2003, Bathymetric and geophysical surveys of Englebright Lake, Yuba-Nevada Counties, California, U.S. Geological Survey Open-File Report 03-383, http://geopubs.wr.usgs.gov/open-file/of03-383/, 20 p.

(*BC student co-authors.)

Links: Dams and dam removal

Nashua Telegraph articles about the Souhegan River dam removal: August 22, 2008; August 29, 2008; May 7, 2009.

 

Previous research

Transient response of a desert river to forced diversion: Furnace Creek Wash, Death Valley National Park, California

Lidar DEM slope (colors, red = steep) and shaded-relief (grayscale) image of the diversion (arrow), Zabriskie Point, Death Valley National Park, California.

Publications: Death Valley area

Snyder, N.P., and Kammer, L.L.*, 2008, Dynamic adjustments in channel width in response to a forced diversion: Gower Gulch, Death Valley National Park, California, Geology, v. 25, p. 187-190, doi: 10.1130/G24217A.1

Snyder, N.P., and Hodges, K.V., 2000, Depositional and tectonic evolution of a supradetachment basin: 40Ar/ 39Ar geochronology of the Nova Formation, Panamint Range, California, Basin Research, v. 12, n. 1, p. 19-30, doi: 10.1046/j.1365-2117.2000.00108.x.

(*BC student co-authors.)

Links: Death Valley area

BC Magazine article about Death Valley research: Spring 2008.

Other articles about Death Valley research: EurekAlert; PhysOrg; ScienceDaily.

 

Publications: Channel response to tectonics, bedrock erosion processes, digital elevation model analysis

Wobus, C.W., Whipple, K.X, Kirby, E., Snyder, N.P., Johnson, J., Spyropolou, K., Crosby, B., and Sheehan, D., 2006, Tectonics from topography: Procedures, promise, and pitfalls, in Willett, S.D., Hovius, N., Brandon, M.T., and Fisher, D.M., editors, Tectonics, Climate, and Landscape Evolution, Geological Society of America Special Paper 398, p. 55-74, doi: 10.1130/2006.2398(04).

Snyder, N.P., Whipple, K.X., Tucker, G.E., and Merritts, D.J., 2003, Importance of a stochastic distribution of floods and erosion thresholds in the bedrock river incision problem, Journal of Geophysical Research, v. 108 (B2), 2117, doi: 10.1029/2001JB001655. correction

Snyder, N.P., Whipple, K.X., Tucker, G.E., and Merritts, D.J., 2003, Channel response to tectonic forcing: analysis of stream morphology and hydrology in the Mendocino triple junction region, northern California, Geomorphology, v. 53, p. 97-127, doi: 10.1016/S0169-555X(02)00349-5.

Snyder, N.P., Whipple, K.X., Tucker, G.E., and Merritts, D.J, 2002, Interactions between onshore bedrock-channel incision and nearshore wave-base erosion forced by eustasy and tectonics, Basin Research, v. 14, p. 105-127, doi: 10.1046/j.1365-2117.2002.00169.x.

Snyder, N.P., Whipple, K.X., Tucker, G.E., and Merritts, D.J, 2000, Landscape response to tectonic forcing: digital elevation model analysis of stream profiles in the Mendocino triple junction region, northern California, Geological Society of America Bulletin, v. 112, n. 8, p. 1250-1263, doi: 10.1130/0016-7606(2000)112<1250:LRTTFD>2.0.CO;2.

Whipple, K.X., Snyder, N.P., and Dollenmayer, K., 2000, Rates and processes of bedrock incision by the Upper Ukak River since the 1912 Novarupta ash flow in the Valley of Ten Thousand Smokes, Alaska, Geology, v. 28, n. 9, p. 835-838, doi: 10.1130/0091-7613(2000)28<835:RAPOBI>2.0.CO;2.

 

Teaching: courses taught on a regular basis

GE 132, Exploring the Earth I

GE 170, Rivers and the Environment

GE 201, Environmental Systems: The Human Footprint

GE 400, Watershed Geomorphology

GE 490, Remote Sensing and Image Interpretation

GE 580, Environmental Seminar

 

GE400 class fieldtrip on Mount Monadnock, NH (November 2007, left); GE132 lecture on Mount Sugarloaf, MA (November 2009, right).


© Noah P. Snyder,  revised 27 June 2012.