Landscape Response to Disturbance Active
Fire plus Flood equals Beach
A new study combines decades of coastal satellite imagery with hydrologic and oceanographic data to look at how changes on land affect coastlines in Big Sur, California
Klamath River Mouth
4 dams on the river are pending removal: USGS is studying coastal watershed response
This project characterizes and measures sediment-related effects of landscape disturbances (such as major storms, drought, or wildfire) and river management. We focus primarily on the U.S. west coast, and our work relates to natural hazards and resource management.
Climate models project that in the future the western U.S. will experience more extreme rain events, greater wildfire activity, and more pronounced swings between extreme drought and extreme wet conditions. These changes could result in landscapes shedding more sediment from hillslopes and transporting it along rivers to the coast. At the same time, removal of aging dams is becoming common in the U.S.; dam removal (and some other human activities) releases sediment downstream, changing the river and coastal environments. Our research is guided by the questions: How does the scale of landscape response (such as the amount of sediment generated) correspond to the scale of disturbance (the amount of storm rainfall)? What controls lag times in landscape response signals—how long after a disturbance do its effects appear downstream, and how long do they last? How do superimposed disturbances, such as fire and subsequent storms, or a dam removal followed by extreme rain, combine to drive landscape evolution? How will variations in landscape sediment output affect the amount of sediment reaching the coast, and how might that affect the shape and evolution of beaches?
Currently active tasks:
1. Dam removal. Our team studies river and coastal response to sediment released by large dam removals, in collaboration with other federal, state, tribal, and academic researchers. Research efforts include long-term studies of the Elwha River, Washington (largest dam removal worldwide), the Carmel River (largest dam removal in California), and Klamath estuary (four pending dam removals in California and Oregon).
2. Landscape response to extreme rainfall. Extreme rain can cause major landslides and flooding, greatly increasing the amount of sediment moving along rivers to the coast. We study effects of extreme rain in, for example, the San Lorenzo and Tuolumne Rivers (California), collaborating with the Coastal Change Hazards program, USGS Geology, Minerals, Energy, and Geophysics Science Center, and others.
3. Post-fire sediment mobilization. Hillslopes commonly shed large quantities of sediment in the aftermath of a wildfire, with potential hazards for downstream communities, infrastructure and water supply. The size and duration of these effects vary widely among landscapes, and have not been measured in detail for many regions. We are collaborating with the National Park Service and other partners to investigate post-fire landscape evolution after the 2018 Carr Fire, northern California, a federally declared disaster. Our efforts focus on Whiskeytown National Recreation Area, evaluating sediment movement that affects Whiskeytown Lake and surrounding watersheds.
Below are other science projects associated with this project.
Below are data or web applications associated with this project.
Grain-size data for sediment samples collected in Whiskeytown Lake, northern California, in 2018 and 2019
Chirp sub-bottom data collected in 2019 in Whiskeytown Lake, California during USGS field activity 2018-686-FA
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2017
River-channel topography and sediment grain size on the Elwha River, Washington, 2006 to 2017
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2012
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, March 2013
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, September 2013
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, September 2014
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2015
Bathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, February 2016
Below are publications associated with this project.
World’s largest dam removal reverses coastal erosion
Conceptualizing ecological responses to dam removal: If you remove it, what's to come?
Geomorphic evolution of a gravel‐bed river under sediment‐starved vs. sediment‐rich conditions: River response to the world's largest dam removal
Understanding river response to sediment pulses is a fundamental problem in geomorphic process studies, with myriad implications for river management. However, because large sediment pulses are rare and usually unanticipated, they are seldom studied at field scale. We examine fluvial response to a massive (~20 Mt) sediment pulse released by the largest dam removal globally, on the Elwha River, Was
A regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes
River response to large‐dam removal in a Mediterranean hydroclimatic setting: Carmel River, California, USA
Morphodynamic evolution following sediment release from the world’s largest dam removal
Sediment pulses can cause widespread, complex changes to rivers and coastal regions. Quantifying landscape response to sediment-supply changes is a long-standing problem in geomorphology, but the unanticipated nature of most sediment pulses rarely allows for detailed measurement of associated landscape processes and evolution. The intentional removal of two large dams on the Elwha River (Washingto
Geomorphic responses to dam removal in the United States – a two-decade perspective
Dam removal: Listening in
Channel-planform evolution in four rivers of Olympic National Park, Washington, U.S.A.: The roles of physical drivers and trophic cascades
Large-scale dam removal on the Elwha River, Washington, USA: river channel and floodplain geomorphic change
Large-scale dam removal on the Elwha River, Washington, USA: source-to-sink sediment budget and synthesis
Understanding landscape responses to sediment supply changes constitutes a fundamental part of many problems in geomorphology, but opportunities to study such processes at field scales are rare. The phased removal of two large dams on the Elwha River, Washington, exposed 21 ± 3 million m3, or ~ 30 million tonnes (t), of sediment that had been deposited in the two former reservoirs, allowing a comp
Below are news stories associated with this project.
- Overview
This project characterizes and measures sediment-related effects of landscape disturbances (such as major storms, drought, or wildfire) and river management. We focus primarily on the U.S. west coast, and our work relates to natural hazards and resource management.
Climate models project that in the future the western U.S. will experience more extreme rain events, greater wildfire activity, and more pronounced swings between extreme drought and extreme wet conditions. These changes could result in landscapes shedding more sediment from hillslopes and transporting it along rivers to the coast. At the same time, removal of aging dams is becoming common in the U.S.; dam removal (and some other human activities) releases sediment downstream, changing the river and coastal environments. Our research is guided by the questions: How does the scale of landscape response (such as the amount of sediment generated) correspond to the scale of disturbance (the amount of storm rainfall)? What controls lag times in landscape response signals—how long after a disturbance do its effects appear downstream, and how long do they last? How do superimposed disturbances, such as fire and subsequent storms, or a dam removal followed by extreme rain, combine to drive landscape evolution? How will variations in landscape sediment output affect the amount of sediment reaching the coast, and how might that affect the shape and evolution of beaches?
Currently active tasks:
1. Dam removal. Our team studies river and coastal response to sediment released by large dam removals, in collaboration with other federal, state, tribal, and academic researchers. Research efforts include long-term studies of the Elwha River, Washington (largest dam removal worldwide), the Carmel River (largest dam removal in California), and Klamath estuary (four pending dam removals in California and Oregon).
2. Landscape response to extreme rainfall. Extreme rain can cause major landslides and flooding, greatly increasing the amount of sediment moving along rivers to the coast. We study effects of extreme rain in, for example, the San Lorenzo and Tuolumne Rivers (California), collaborating with the Coastal Change Hazards program, USGS Geology, Minerals, Energy, and Geophysics Science Center, and others.
3. Post-fire sediment mobilization. Hillslopes commonly shed large quantities of sediment in the aftermath of a wildfire, with potential hazards for downstream communities, infrastructure and water supply. The size and duration of these effects vary widely among landscapes, and have not been measured in detail for many regions. We are collaborating with the National Park Service and other partners to investigate post-fire landscape evolution after the 2018 Carr Fire, northern California, a federally declared disaster. Our efforts focus on Whiskeytown National Recreation Area, evaluating sediment movement that affects Whiskeytown Lake and surrounding watersheds.
- Science
Below are other science projects associated with this project.
- Data
Below are data or web applications associated with this project.
Filter Total Items: 23Grain-size data for sediment samples collected in Whiskeytown Lake, northern California, in 2018 and 2019
The Carr Fire ignited in northern California in July 2018, and ultimately burned almost 300,000 acres (approximately half on federal lands), resulting in a federal major-disaster declaration (DR-4382). Approximately 93% of the area within Whiskeytown National Recreation Area was burned extensively during the Carr Fire, including all of the landscape surrounding and draining into Whiskeytown Lake.Chirp sub-bottom data collected in 2019 in Whiskeytown Lake, California during USGS field activity 2018-686-FA
High-resolution chirp sub-bottom data were collected by the U.S. Geological Survey, Pacific Coastal and Marine Science Center in May of 2019 in Whiskeytown Lake, California using an Edgetech SB-512i sub-bottom profiler. These data were collected to measure possible debris flows into the lake during the 2018-2019 rainy season following the July-August 2018 Carr fire that burned vegetation around thBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2017
Two dams on the Elwha River, Washington State, USA trapped over 20 million m3 of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta system to changesRiver-channel topography and sediment grain size on the Elwha River, Washington, 2006 to 2017
The Elwha River, Washington, USA, was the site of the largest dam-removal project to date, in which two dams were removed between 2011 and 2014. Dam removal was made in stages over about a one-year period for the Elwha Dam (32 m high) and a three-year period for the Glines Canyon Dam (64 m high). This data release presents topographic and sediment grain size data collected by the U.S. Geological SBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, August 2012
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, March 2013
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, September 2013
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, September 2014
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, July 2015
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta systemBathymetry, topography, and sediment grain-size data from the Elwha River delta, Washington, February 2016
Two dams on the Elwha River, Washington State, USA trapped over 20 million cubic meters of sediment, reducing downstream sediment fluxes and contributing to erosion of the river's coastal delta. The removal of the Elwha and Glines Canyon dams between 2011 and 2014 induced massive increases in river sediment supply and provided an unprecedented opportunity to examine the response of a delta system - Maps
- Publications
Below are publications associated with this project.
Filter Total Items: 23World’s largest dam removal reverses coastal erosion
Coastal erosion outpaces land generation along many of the world’s deltas and a significant percentage of shorelines, and human-caused alterations to coastal sediment budgets can be important drivers of this erosion. For sediment-starved and erosion-prone coasts, large-scale enhancement of sediment supply may be an important, but poorly understood, management option. Here we provide new topographiAuthorsJonathan Warrick, Andrew W. Stevens, Ian M. Miller, Shawn R Harrison, Andrew C. Ritchie, Guy R. GelfenbaumConceptualizing ecological responses to dam removal: If you remove it, what's to come?
One of the desired outcomes of dam decommissioning and removal is the recovery of aquatic and riparian ecosystems. To investigate this common objective, we synthesized information from empirical studies and ecological theory into conceptual models that depict key physical and biological links driving ecological responses to removing dams. We define models for three distinct spatial domains: upstreAuthorsJ. Ryan Bellmore, George R. Pess, Jeffrey J. Duda, Jim E. O'Connor, Amy E. East, Melissa M. Foley, Andrew C. Wilcox, Jon J. Major, Patrick B. Shafroth, Sarah A. Morley, Christopher S. Magirl, Chauncey W. Anderson, James E. Evans, Christian E. Torgersen, Laura S. CraigByEcosystems Mission Area, Coastal and Marine Hazards and Resources Program, Species Management Research Program, Arizona Water Science Center, Forest and Rangeland Ecosystem Science Center, Fort Collins Science Center, Geology, Minerals, Energy, and Geophysics Science Center, John Wesley Powell Center for Analysis and Synthesis, Oregon Water Science Center, Pacific Coastal and Marine Science Center, Western Fisheries Research CenterGeomorphic evolution of a gravel‐bed river under sediment‐starved vs. sediment‐rich conditions: River response to the world's largest dam removal
Understanding river response to sediment pulses is a fundamental problem in geomorphic process studies, with myriad implications for river management. However, because large sediment pulses are rare and usually unanticipated, they are seldom studied at field scale. We examine fluvial response to a massive (~20 Mt) sediment pulse released by the largest dam removal globally, on the Elwha River, Was
AuthorsAmy E. East, Joshua B. Logan, Mark C. Mastin, Andrew C. Ritchie, Jennifer A. Bountry, Christopher S. Magirl, Joel B. SankeyA regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes
Small, steep watersheds are prolific sediment sources from which sediment flux is highly sensitive to climatic changes. Storm intensity and frequency are widely expected to increase during the 21st century, and so assessing the response of small, steep watersheds to extreme rainfall is essential to understanding landscape response to climate change. During record winter rainfall in 2016–2017, theAuthorsAmy E. East, Andrew W. Stevens, Andrew C. Ritchie, Patrick L. Barnard, Pamela L. Campbell‐Swarzenski, Brian D. Collins, Christopher H. ConawayRiver response to large‐dam removal in a Mediterranean hydroclimatic setting: Carmel River, California, USA
Dam removal provides a valuable opportunity to measure the fluvial response to changes in both sediment supply and the processes that shape channel morphology. We present the first study of river response to the removal of a large (32‐m‐high) dam in a Mediterranean hydroclimatic setting, on the Carmel River, coastal California, USA. This before‐after/control‐impact study measured changes in channeAuthorsLee R. Harrison, Amy E. East, Douglas P. Smith, Joshua B. Logan, Rosealea Bond, Colin L. Nicol, Thomas H. Williams, David A. Boughton, Kaitlyn Chow, Lauren LunaMorphodynamic evolution following sediment release from the world’s largest dam removal
Sediment pulses can cause widespread, complex changes to rivers and coastal regions. Quantifying landscape response to sediment-supply changes is a long-standing problem in geomorphology, but the unanticipated nature of most sediment pulses rarely allows for detailed measurement of associated landscape processes and evolution. The intentional removal of two large dams on the Elwha River (Washingto
AuthorsAndrew C. Ritchie, Jonathan Warrick, Amy E. East, Christopher S. Magirl, Andrew W. Stevens, Jennifer A. Bountry, Timothy J. Randle, Christopher A. Curran, Robert C. Hilldale, Jeffrey J. Duda, Ian M. Miller, George R. Pess, Emily Eidam, Melissa M. Foley, Randall McCoy, Andrea S. OgstonByEcosystems Mission Area, Natural Hazards Mission Area, Water Resources Mission Area, Coastal and Marine Hazards and Resources Program, Arizona Water Science Center, Pacific Coastal and Marine Science Center, Washington Water Science Center, Western Fisheries Research Center, Sediment Lab Suite and Carbon Analysis LaboratoryGeomorphic responses to dam removal in the United States – a two-decade perspective
Recent decades have seen a marked increase in the number of dams removed in the United States. Investigations following a number of removals are beginning to inform how, and how fast, rivers and their ecosystems respond to released sediment. Though only a few tens of studies detail physical responses to removals, common findings have begun to emerge. They include: (1) Rivers are resilient and respAuthorsJon J. Major, Amy E. East, Jim E. O'Connor, Gordon E. Grant, Andrew C. Wilcox, Christopher S. Magirl, Matthias J. Collins, Desiree D. TullosDam removal: Listening in
Dam removal is widely used as an approach for river restoration in the United States. The increase in dam removals—particularly large dams—and associated dam-removal studies over the last few decades motivated a working group at the USGS John Wesley Powell Center for Analysis and Synthesis to review and synthesize available studies of dam removals and their findings. Based on dam removals thus farAuthorsMelissa M. Foley, James Bellmore, James E. O'Connor, Jeffrey J. Duda, Amy E. East, Gordon G. Grant, Chauncey W. Anderson, Jennifer A. Bountry, Mathias J. Collins, Patrick J. Connolly, Laura S. Craig, James E. Evans, Samantha Greene, Francis J. Magilligan, Christopher S. Magirl, Jon J. Major, George R. Pess, Timothy J. Randle, Patrick B. Shafroth, Christian E. Torgersen, Desiree D. Tullos, Andrew C. WilcoxByEcosystems Mission Area, Natural Hazards Mission Area, Water Resources Mission Area, Volcano Hazards Program, Forest and Rangeland Ecosystem Science Center, John Wesley Powell Center for Analysis and Synthesis, Oregon Water Science Center, Pacific Coastal and Marine Science Center, Volcano Science Center, Western Fisheries Research Center, Columbia River Research Laboratory (CRRL)Channel-planform evolution in four rivers of Olympic National Park, Washington, U.S.A.: The roles of physical drivers and trophic cascades
Identifying the relative contributions of physical and ecological processes to channel evolution remains a substantial challenge in fluvial geomorphology. We use a 74-year aerial photographic record of the Hoh, Queets, Quinault, and Elwha Rivers, Olympic National Park, Washington, U.S.A., to investigate whether physical or trophic-cascade-driven ecological factors—excessive elk impacts after wolveAuthorsAmy E. East, Kurt J. Jenkins, Patricia J. Happe, Jennifer A. Bountry, Timothy J. Beechie, Mark C. Mastin, Joel B. Sankey, Timothy J. RandleLarge-scale dam removal on the Elwha River, Washington, USA: river channel and floodplain geomorphic change
A substantial increase in fluvial sediment supply relative to transport capacity causes complex, large-magnitude changes in river and floodplain morphology downstream. Although sedimentary and geomorphic responses to sediment pulses are a fundamental part of landscape evolution, few opportunities exist to quantify those processes over field scales. We investigated the downstream effects of sedimenAuthorsAmy E. East, George R. Pess, Jennifer A. Bountry, Christopher S. Magirl, Andrew C. Ritchie, Joshua B. Logan, Timothy J. Randle, Mark C. Mastin, Justin Toby Minear, Jeffrey J. Duda, Martin C. Liermann, Michael L. McHenry, Timothy J. Beechie, Patrick B. ShafrothLarge-scale dam removal on the Elwha River, Washington, USA: source-to-sink sediment budget and synthesis
Understanding landscape responses to sediment supply changes constitutes a fundamental part of many problems in geomorphology, but opportunities to study such processes at field scales are rare. The phased removal of two large dams on the Elwha River, Washington, exposed 21 ± 3 million m3, or ~ 30 million tonnes (t), of sediment that had been deposited in the two former reservoirs, allowing a comp
AuthorsJonathan A. Warrick, Jennifer A. Bountry, Amy E. East, Christopher S. Magirl, Timothy J. Randle, Guy R. Gelfenbaum, Andrew C. Ritchie, George R. Pess, Vivian Leung, Jeff J. Duda - News
Below are news stories associated with this project.
Filter Total Items: 14