Leaburg Dam across Oregon's McKenzie River

Dams

Flow regulation is the alteration of the natural flow regime via construction of dams or diversions. Dams interrupt the downstream movement of water – and anything moving with the water, such as sediment – by creating an obstruction and an upstream reservoir. Depending on the details of dam design and operation, the downstream flow regime may become rapidly varied on a predictable schedule (dams used to generate hydroelectric power) or the peak flows may be reduced and the base flows increased (water storage or flood control dams). Regardless of the specifics, a dam alters the magnitude, duration, and timing of downstream water movement in a manner that commonly stresses or kills native aquatic and riparian species that are evolutionarily adapted to a natural flow regime. The altered flow regime typically also alters downstream sediment movement in a manner that results in channel and floodplain erosion and simplification. The dam itself usually blocks up- and downstream movements by aquatic organisms such as fish passage, even if fish passage structures are included in dam design.

A dam designed to facilitate barge navigation on the Mississippi River

An extensive scientific and popular literature describes the many detrimental effects of dams on river corridors. Although hydroelectric power is sometimes regarded as a clean, renewable source of energy, the increased emissions of methane and carbon dioxide from artificial reservoirs, and the massive destruction of river ecosystems, suggest that dams are not a clean or environmentally friendly source of power. Nonetheless, only an estimated 2% of the total lengths of rivers in the contiguous United States are not affected by dams.

Tempe Lake, an artificial reservoir created by a dam on the ephemeral Salt River in the Phoenix, Arizona metropolitan area.

Aerial view of Oahe Dam on the Missouri River in South Dakota. This is one of the largest earthen dams in the US.

Bibliography

Deemer, B.R., J.A. Harrison, S. Li, J.J. Beaulieu, et al. 2016. Greenhouse gas emissions from reservoir water surfaces: a new global synthesis. BioScience, 66, 949-964.

Graf, W.L. 1999. Dam nation: a geographic census of American dams and their large-scale hydrologic impacts. Water Resources Research, 35, 1305-1311.

Graf, W.L. 2001. Damage control: restoring the physical integrity of America’s rivers. Annals Association of American Geographers, 91, 1-27.

Ligon, F.K., W.E. Dietrich, and W.J. Trush. 1995. Downstream ecological effects of dams. BioScience, 45, 183-192.

Maeck, A., T. Del Sontro, D.F. McGinnis, H. Fischer, S. Flury, M. Schmidt, P. Fietzek, and A. Lorke. 2013. Sediment trapping by dams creates methane emission hot spots. Environmental Science and Technology, 47, 8130-8137.

Nilsson, C., C.A. Reidy, M. Dynesius, and C. Revenga. 2005. Fragmentation and flow regulation of the world’s large river systems. Science, 308, 405-408.

Poff, N.L., J.D. Allan, M.B. Bain, J.R. Karr, K.L. Prestegaard, B.D. Richter, R.E. Sparks, and J.C. Stromberg. 1997. The natural flow regime. BioScience, 47, 769-784.

Poff, N.L., J.D. Olden, D.M. Merritt, and D.M. Pepin. 2007. Homogenization of regional river dynamics by dams and global biodiversity implications. Proceedings National Academy of Sciences (US), 104, 5732-5737.

Wohl, E., B.P. Bledsoe, R.B. Jacobson, N.L. Poff, S.L. Rathburn, D.M. Walters, and A.C. Wilcox. 2015. The natural sediment regime in rivers: broadening the foundation for ecosystem management. BioScience, 65, 358-371.

Aerial view of Hoover Dam on the Colorado River. This is an example of a concrete arch-gravity dam.

Looking upstream to a dam along a de-watered portion of the Ocoee River in Tennessee

Diversions

An aerial view of the Central Arizona Project (dark, linear feature) in the greater Phoenix metropolitan area. This massive canal that carries water diverted from the Colorado River to urban areas in central and southern Arizona.

Although less well-documented than dams, diversions that transfer water from a river into adjacent lands or move water from one river to another are widespread in the contiguous United States. By removing water from the source river, diversions contribute to drying, sediment accumulation, and longitudinal disconnectivity in the river corridor. The receiving river may have unnaturally large peak flows that cause erosion and may be entered by contaminants and exotic organisms that harm the ecosystem of the receiving river.

Wing dams that partially span the channel near a diversion on the McKenzie River, Oregon

Bibliography

Caskey, S.T., T.S. Blaschak, E. Wohl, E. Schnackenberg, D.M. Merritt, and K.A. Dwire. 2015. Downstream effects of flow diversion on channel characteristics and riparian vegetation in the Colorado Rocky Mountains, USA. Earth Surface Processes and Landforms, 40, 586-598.

David, G.C.L., B.P. Bledsoe, D.M. Merritt, and E. Wohl. 2009. The impacts of ski slope development on stream channel morphology in the White River National Forest, Colorado, USA. Geomorphology, 103, 375-388.

Rader, R.B. and T.A. Belish. 1999. Influence of mild to severe flow alterations on invertebrates in three mountain streams. Regulated Rivers: Research and Management, 15, 353-363.

Ryan, S. 1997. Morphologic response of subalpine streams to transbasin flow diversion. Journal American Water Resources Association, 33, 839-854.

Wohl, E. and D. Dust. 2012. Geomorphic response of a headwater channel to augmented flow. Geomorphology, 138, 329-338.

Leaburg Dam across Oregon's McKenzie River

A dam designed to facilitate barge navigation on the Mississippi River

Tempe Lake, an artificial reservoir created by a dam on the ephemeral Salt River in the Phoenix, Arizona metropolitan area.

Aerial view of Oahe Dam on the Missouri River in South Dakota. This is one of the largest earthen dams in the US.

Aerial view of Hoover Dam on the Colorado River. This is an example of a concrete arch-gravity dam.

Looking upstream to a dam along a de-watered portion of the Ocoee River in Tennessee

An aerial view of the Central Arizona Project (dark, linear feature) in the greater Phoenix metropolitan area. This massive canal that carries water diverted from the Colorado River to urban areas in central and southern Arizona.

Wing dams that partially span the channel near a diversion on the McKenzie River, Oregon