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Dams in Oregon: impacts, opportunities and future directions Rose Wallick Chauncey Anderson, Stewart Rounds, Mackenzie Keith, Krista Jones USGS Oregon Water Science Center U.S. Department of the Interior U.S. Department of the Interior U.S.


  1. Dams in Oregon: impacts, opportunities and future directions Rose Wallick Chauncey Anderson, Stewart Rounds, Mackenzie Keith, Krista Jones USGS Oregon Water Science Center U.S. Department of the Interior U.S. Department of the Interior U.S. Geological Survey U.S. Geological Survey

  2. Dams in Oregon Dam Height More than 1,100 dams in state dam inventory 48 dams more than 100ft tall 10 dams more than 300 ft tall Cougar Dam is tallest – 519 ft

  3. Overview Purpose and environmental impacts of dams Strategies to address impacts  Removal, infrastructure modifications, operations Science insights from USGS studies Future directions

  4. U.S. has more than 87,000 documented dams Source: National Inventory of Dams, ttp://nid.usace.army.mil/ Dams built per decade Detroit Dam, completed 1953, 463 ft After Doyle et al. (2003) Cougar Dam, completed 1963, 519 ft Photographs courtesy USACE

  5. Purpose of dams Dams provide:  Hydropower  Flood control  Water storage  Navigation Middle Fork Willamette, USGS photo  Recreation  Other benefits Detroit Lake, Photo courtesy: https://www.detroitlakeoregon.org/

  6. Environmental impacts of dams  Alter river flows, water temperature, water quality, trap sediment, carbon, nutrients in reservoirs  Block fish passage  Change ecosystems above and below dams  Support conditions that can lead to harmful algae blooms Cougar Reservoir, South Fork McKenzie, USGS photo Middle Fork Willamette River below Dexter Dam, USGS photo

  7. Motivating factors for removing, upgrading or re-operating dams Examples include: • Dams age, expensive to maintain safely • Facilities may not work as initially intended • Reservoirs fill with sediment • Regulatory requirements • Fish passage • Water quality Iron Gate Dam and Reservoir, Klamath River, Photograph by C. Anderson, USGS

  8. Management strategies Obsolete or unsafe dams are candidates for removal Upgrade facilities Fish passage Temperature control Total dissolved gas Modify operations of existing facilities Environmental flows for habitats Flow management to address temperature Drawdowns to flush sediment or pass fish Portable Floating Fish Collector, Cougar Reservoir, photo by R. Wallick, USGS

  9. Dam removal reasons Ecosystem restoration  Fish passage and habitat  Upstream / downstream connectivity  Water temperature changes (seasonal timing, & absolute temperatures) Safety  Many old facilities expensive to modernize  Earthquakes Economic  FERC relicensing  Costs of retrofitting or management changes to meet ESA or other requirements Elwha Dam, 108 ft, removed in 2011 Photo by C. Magirl, USGS New York Times article on risks of Lake Isabella dam failure

  10. Dam removal in the U.S. Major et al., Gravel-Bed Rivers v. 8, in press, based on American Rivers database

  11. Dam removal –technical concerns  Hydrologic Changes – Flooding, channel changes  Sediment Erosion / Transport / Deposition  Reservoir erosion  Downstream deposition  Impacts to habitats  Debris  Contaminants  Water quality  Invasive aquatic species & plants  Loss of fish collection facilities  Decreased groundwater levels  Impacts on infrastructure (WTPs, pumps, pipelines…) Potential benefits include: improvements to habitat, fish passage, water quality, removal of non-native reservoir fish…

  12. Effects of dam removal proportional to dam size and operation • Dam’s effects on flow and sediment transport (dam presence and operations both matter) • Dam height, and pace of removal • Reservoir sediment volume, composition 64 m high dam 4 m high dam Homestead Dam, Ashuelot River, Glines Canyon Dam, Elwha River, WA NH (Gartner et al., 2015) USGS photographs

  13. Overarching conceptual model Foley and others, 2017

  14. Ecosystem impacts, benefits from dam removal Much still to learn about ecosystem responses, but making progress. 1. Ecosystem responses mediated through bio-physical processes 2. Many complex relationships, feedbacks Pess et al., in revision

  15. Coupled upstream-downstream system Ecological responses Pess et al, in revision. Pess et al., in revision

  16. Case study: Marmot Dam, Sandy River February 26, 2008 Photos by J. Major, USGS Lessons learned (Foley and others, 2017) • Physical responses typically fast • Ecological responses differ longitudinally • Connectivity quickly restored • Geomorphic context matters • Quantitative models useful for predicting effects • Fish respond rapidly

  17. Using science and engineering to inform dam operations Examples from Willamette and Columbia U.S. Department of the Interior U.S. Geological Survey (photos from Corps of Engineers and PGE)

  18. USACE dams in Willamette Valley Willamette Basin  13 USACE dams  ESA-listed fish  Chinook salmon  Steelhead salmon  Bull trout Operations consider  Flood control, hydropower, downstream water users, recreation  Temperature management  Seasonal flow requirements for listed fish 10mi

  19. Total Dissolved Gas Critical regulatory metric for dam operations  Goal: Minimize gas bubble trauma for outmigrating juvenile salmonids  Real time decisions regarding spill and power generation  Infrastructure improvements Lower Granite Dam, Snake River. Photo credit: E. Glisch, USACE

  20. Total Dissolved Gas Monitoring http://www.nwd.usace.army.mil/Missions/Water/Columbia/Water-Quality/

  21. Downstream Temperatures Temperature affects fish habitat and the timing of migration, spawning, egg incubation and Detroit Dam emergence, etc. 463 feet tall Multiple outlets: • Spillway • Power penstocks •Upper regulating outlets •Lower regulating outlets Warm or cool temperatures accessed with different outlets U.S. Department of the Interior U.S. Geological Survey photo from U.S. Army Corps of Engineers

  22. Willamette River Models CE-QUAL-W2 444 river miles • Calibrated for 2001 and 2002 for temperature TMDL. • Used to assess effects of upstream dams. • Used to evaluate 2011 (cool/wet) and 2015 (hot/dry) conditions and aid in evaluations of flow management • Used to help quantify a Thermal Mosaic U.S. Department of the Interior map from USGS U.S. Geological Survey of the river.

  23. Flow Comparison, With and Without Dams 2 3 Simulated Flow, Willamette River at Salem 100,000 With Dams Lower flows in winter and spring No Dams 40,000 Streamflow (ft 3 /s) Higher flows in late summer and 20,000 early fall 10,000 4,000 2,000 1,000 Apr May Jun Jul Aug Sep Oct 2002 See http://pubs.usgs.gov/sir/2010/5153/

  24. Temperature Comparison, With and Without Dams North Santiam River at Big Cliff Dam 20 Warmer Measured, with dams 18 Estimated, without dams in Cooler in autumn 16 Water Temperature ( ° C) summer 14 12 10 8 6 4 2 0 J F M A M J J A S O N D J F M A M J J A S O N D 2001 2002 See http://pubs.usgs.gov/sir/2010/5153/

  25. 2 Thermal Effect of Dams on River Network 5 Coast Fork Willamette and Willamette Rivers In spring and autumn, river experiences warming 2002 During summer, river experiences cooling from dams River Mile Long Tom Santiam Row MF McKenzie Clackamas Temperature Change = “With Dams” minus “No Dams” Important Tributary Inputs -6.0 -5.0 -4.0 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5 -0.3 -0.2 -0.1 0.0 0.1 0.2 0.3 0.5 1.0 1.5 2.0 2.5 3.0 4.0 5.0 6.0 7dADM Temperature Change ( ° C) See http://pubs.usgs.gov/sir/2010/5153/

  26. 26 Downstream Thermal Effect of Dams on Fish Fish Use Periods Return 2002 Holding Spawning Incubation -6.0 -5.0 -4.0 -3.0 -2.5 -2.0 -1.5 -1.0 -0.5 -0.3 -0.2 -0.1 0.0 0.1 0.2 0.3 0.5 1.0 1.5 2.0 2.5 3.0 4.0 5.0 6.0 7dADM Temperature Change ( ° C)

  27. 27 Modeled 7-day Average of Daily Max Temperatures 2011 McKenzie Calapooia Santiam Tualatin Preliminary results; subject to revision

  28. 28 Modeled 7-day Average of Daily Max Temperatures 2015 In 2015, most of the Willamette River exceeded 18 deg. C from June to Sept Calapooia McKenzie Santiam Tualatin Preliminary results; subject to revision

  29. Example of temperature blending: Detroit Dam, Oregon 29 Lake warms gradually through summer Warm water floats on top of cold water Blending outflows from different outlets can help mitigate temperature issues Spillways (warm water) Power Upper ROs (cool water) Upstream side of Detroit Dam Image from Corps of Engineers

  30. 30 Detroit Lake water levels for different scenarios In all years, lake level above spillway, but duration varies • In dry year, water level drops below spillway August 1 • In cool/wet years and normal year, below spillway early September rule curve Month See http://dx.doi.org/10.3133/ofr20151012

  31. 31 Detroit Modeled Temperatures, Without Blending When releasing cool water from power penstock, temperatures are below target most of summer. Water remaining in the fall is warm, resulting in releases that exceed targets for spawning and incubation. In all year types, temperature exceeds target during temperature salmon spawning/incubation period target ~ 6 °C Brown lines are desirable temperature ranges rule curve See http://dx.doi.org/10.3133/ofr20151012

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