Sediment Transport in Coastal Environments Active
Our research goals are to provide the scientific information, knowledge, and tools required to ensure that decisions about land and resource use, management practices, and future development in the coastal zone and adjacent watersheds can be evaluated with a complete understanding of the probable effects on coastal ecosystems and communities, and a full assessment of their vulnerability to natural and human-driven changes.
Coastal resource managers face a wide range of problems related to sediment transport. Sediment management or questions related to sediment transport are involved in dredging operations, preventing or planning for coastal erosion, evaluation of the impacts of anthropogenic alterations on coastal ecosystems, restoration of coastal habitats, and planning for climate change. To address these questions, coastal managers typically require both site-specific information about sediment transport processes, and predictive models of the outcome of potential management actions.
Understanding of sediment transport processes and the ability to model sediment transport have advanced significantly in recent decades, but important limitations remain. It is still a common practice to report results of sediment transport modeling with limited or no calibration, due to lack of suitable data for calibration. The relative importance of factors governing sediment transport varies between coastal environments due to differences in both sediment properties and physical forcing. The development of robust models of sediment transport applicable to all aquatic environments, and the movement of sediment between them, requires data from a range of settings for testing.
Project Objectives
- to utilize USGS Coastal and Marine Hazards and Resources Program expertise to investigate problems in coastal sediment transport that are relevant to sediment management issues, including protection of coastal ecosystems, reducing the risk of natural hazards, and adapting to or predicting effects of climate change
- to utilize the results obtained in these studies to improve understanding of sediment transport processes, and incorporate this improved understanding in predictive models
- to conduct research and advise resource managers on the impacts of human activities and the effectiveness of restoration measures on river, estuarine, and marine habitats in collaboration with federal, state, and local agencies, and academic partners.
Current Research Topics
Click to learn more about our research:
- Drag and sediment transport: conditions at the bottom boundary
- Coastal watershed and estuary restoration in the Monterey Bay area
- Sediment transport in submarine canyons
- Columbia River estuary
- San Francisco Bay geomorphology
- Sediment transport between estuarine habitats in San Francisco Bay
- Transport of invasive microorganisms
Below are the study topics associated with this project.
Below are data sets associated with this project.
Below are multimedia items associated with this project.
Sediment Transport in San Francisco Bay
The Sacramento and San Joaquin Rivers deliver half the amount of sediment they did 50 years ago to San Francisco Bay. Just as sea-level rise is accelerating, the demand for sediment is growing.
Below are publications associated with this project.
Linking direct measurements of turbidity currents to submarine canyon-floor deposits
Submarine canyons are conduits for episodic and powerful sediment density flows (commonly called turbidity currents) that move globally significant amounts of terrestrial sediment and organic carbon into the deep sea, forming some of the largest sedimentary deposits on Earth. The only record available for most turbidity currents is the deposit they leave behind. Therefore, to understand turbidity
Measuring settling velocity in a strongly tidal estuary
Predicting sediment transport in estuarine systems requires understanding sediment settling velocity, its range of fluctuations, and the shortcomings of the tools to measure it. Previous studies have used Laser In-Situ Scattering and Transmissometry (LISST) instruments to measure particle size and Acoustic Doppler Velocimeters (ADV) to return estimates of settling velocity. We deployed both instru
Discovery of an extensive deep-sea fossil serpulid reef associated with a cold seep, Santa Monica Basin, California
Conceptualizing ecological responses to dam removal: If you remove it, what's to come?
Do we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers
Controls on submarine channel-modifying processes identified through morphometric scaling relationships
Controls on submarine canyon head evolution: Monterey Canyon, offshore central California
The influence of neap-spring tidal variation and wave energy on sediment flux in salt marsh tidal creeks
Wave attenuation across a tidal marsh in San Francisco Bay
Developing Foram-AMBI for biomonitoring in the Mediterranean: Species assignments to ecological categories
Removal of San Clemente Dam did more than restore fish passage
Coherence between coastal and river flooding along the California coast
Below are news stories associated with this project.
- Overview
Our research goals are to provide the scientific information, knowledge, and tools required to ensure that decisions about land and resource use, management practices, and future development in the coastal zone and adjacent watersheds can be evaluated with a complete understanding of the probable effects on coastal ecosystems and communities, and a full assessment of their vulnerability to natural and human-driven changes.
Coastal resource managers face a wide range of problems related to sediment transport. Sediment management or questions related to sediment transport are involved in dredging operations, preventing or planning for coastal erosion, evaluation of the impacts of anthropogenic alterations on coastal ecosystems, restoration of coastal habitats, and planning for climate change. To address these questions, coastal managers typically require both site-specific information about sediment transport processes, and predictive models of the outcome of potential management actions.
Understanding of sediment transport processes and the ability to model sediment transport have advanced significantly in recent decades, but important limitations remain. It is still a common practice to report results of sediment transport modeling with limited or no calibration, due to lack of suitable data for calibration. The relative importance of factors governing sediment transport varies between coastal environments due to differences in both sediment properties and physical forcing. The development of robust models of sediment transport applicable to all aquatic environments, and the movement of sediment between them, requires data from a range of settings for testing.
Project Objectives
- to utilize USGS Coastal and Marine Hazards and Resources Program expertise to investigate problems in coastal sediment transport that are relevant to sediment management issues, including protection of coastal ecosystems, reducing the risk of natural hazards, and adapting to or predicting effects of climate change
- to utilize the results obtained in these studies to improve understanding of sediment transport processes, and incorporate this improved understanding in predictive models
- to conduct research and advise resource managers on the impacts of human activities and the effectiveness of restoration measures on river, estuarine, and marine habitats in collaboration with federal, state, and local agencies, and academic partners.
Current Research Topics
Click to learn more about our research:
- Drag and sediment transport: conditions at the bottom boundary
- Coastal watershed and estuary restoration in the Monterey Bay area
- Sediment transport in submarine canyons
- Columbia River estuary
- San Francisco Bay geomorphology
- Sediment transport between estuarine habitats in San Francisco Bay
- Transport of invasive microorganisms
- Science
Below are the study topics associated with this project.
- Data
Below are data sets associated with this project.
- Multimedia
Below are multimedia items associated with this project.
Sediment Transport in San Francisco Bay
The Sacramento and San Joaquin Rivers deliver half the amount of sediment they did 50 years ago to San Francisco Bay. Just as sea-level rise is accelerating, the demand for sediment is growing.
- Publications
Below are publications associated with this project.
Filter Total Items: 78Linking direct measurements of turbidity currents to submarine canyon-floor deposits
Submarine canyons are conduits for episodic and powerful sediment density flows (commonly called turbidity currents) that move globally significant amounts of terrestrial sediment and organic carbon into the deep sea, forming some of the largest sedimentary deposits on Earth. The only record available for most turbidity currents is the deposit they leave behind. Therefore, to understand turbidity
AuthorsKatherine L. Maier, Jenny Gales, Charles K. Paull, Kurt J. Rosenberger, Peter J. Talling, Stephen Simmons, Roberto Gwiazda, Mary McGann, Matthieu J.B. Cartigny, Eve M. Lundsten, Krystle Anderson, Michael Clare, Jingping Xu, Daniel Parsons, James P. Barry, Monica Wolfson-Schwher, Nora M. Nieminski, Esther J. SumnerMeasuring settling velocity in a strongly tidal estuary
Predicting sediment transport in estuarine systems requires understanding sediment settling velocity, its range of fluctuations, and the shortcomings of the tools to measure it. Previous studies have used Laser In-Situ Scattering and Transmissometry (LISST) instruments to measure particle size and Acoustic Doppler Velocimeters (ADV) to return estimates of settling velocity. We deployed both instru
AuthorsRachel Allen, Jessica R. Lacy, Evan A VarianoDiscovery of an extensive deep-sea fossil serpulid reef associated with a cold seep, Santa Monica Basin, California
Multi-beam mapping of the Santa Monica Basin in the eastern Pacific has revealed the existence of a number of elevated bathymetric features, or mounds, harboring cold seep communities. During 2013-2014, mounds at ~600 m water depth were observed for the first time and sampled by Monterey Bay Aquarium Research Institute’s ROV Doc Ricketts. Active cold seeps were found, but surprisingly one of theseAuthorsMagdalena N Georgieva, Charles K. Paull, Crispin TS Little, Mary McGann, Diana Sahy, Daniel Condon, Lonny Lundsten, Jack Pewsey, David W Caress, Robert C VrijenhoekConceptualizing 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 CenterDo we know how much fluvial sediment reaches the sea? Decreased river monitoring of U.S. coastal rivers
Given the present and future changing climate and human changes to land use and river control, river sediment fluxes to coastal systems are changing and will continue to change in the future. To delineate these changes and their effects, it is increasingly important to document the fluxes of river-borne sediment discharged to the sea. Unfortunately, broad-scale river sediment monitoring programsAuthorsJonathan Warrick, John D. MillimanControls on submarine channel-modifying processes identified through morphometric scaling relationships
Submarine channels share morphological similarities with rivers, but observations from modern and ancient systems indicate they are formed under processes and controls unique to submarine settings. Morphologic characteristics of channels—e.g., width, depth, slope, and the relationships among them—can constrain interpretations of channel-forming processes. This work uses morphometric scaling relatiAuthorsLauren E. Shumaker, Zane R. Jobe, Samuel Johnstone, Luke A. Pettinga, Dingxin Cai, Jeremiah D. MoodyControls on submarine canyon head evolution: Monterey Canyon, offshore central California
The Monterey submarine canyon, incised across the continental shelf in Monterey Bay, California, provides a record of the link between onshore tectonism, fluvial transport, and deep-marine deposition. High-resolution seismic-reflection imaging in Monterey Bay reveals an extensive paleocanyon unit buried below the seafloor of the continental shelf around Monterey and Soquel canyon heads. PaleocanyoAuthorsKatherine L. Maier, Samuel Y. Johnson, Patrick E. HartThe influence of neap-spring tidal variation and wave energy on sediment flux in salt marsh tidal creeks
Sediment flux in marsh tidal creeks is commonly used to gage sediment supply to marshes. We conducted a field investigation of temporal variability in sediment flux in tidal creeks in the accreting tidal marsh at China Camp State Park adjacent to northern San Francisco Bay. Suspended-sediment concentration (SSC), velocity, and depth were measured near the mouths of two tidal creeks during threeAuthorsJessica R. Lacy, Matthew C. Ferner, John C. CallawayWave attenuation across a tidal marsh in San Francisco Bay
Wave attenuation is a central process in the mechanics of a healthy salt marsh. Understanding how wave attenuation varies with vegetation and hydrodynamic conditions informs models of other marsh processes that are a function of wave energy (e.g. sediment transport) and allows for the incorporation of marshes into coastal protection plans. Here, we examine the evolution of wave height across a tidAuthorsMadeline R. Foster-Martinez, Jessica R. Lacy, Matthew C. Ferner, Evan A. VarianoDeveloping Foram-AMBI for biomonitoring in the Mediterranean: Species assignments to ecological categories
Most environmental bio-monitoring methods using the species composition of marine faunas define the Ecological Quality Status of soft bottom ecosystems based on the relative proportions of species assigned to a limited number of ecological categories. In this study we analyse the distribution patterns of benthic foraminifera in the Mediterranean as a function of organic carbon gradients on the basAuthorsFrans Jorissen, Maria P. Nardelli, Ahuva Almogi-Labin, Christine Barras, Luisa Bergamin, Erica Bicchi, Akram El Kateb, Luciana Ferraro, Mary McGann, Caterina Morigi, Elena Romano, Anna Sabattini, Magali Schweizer, Silvia SpezzaferriRemoval of San Clemente Dam did more than restore fish passage
No abstract available.AuthorsThomas H. Williams, Amy E. East, Douglas P. Smith, David A. Boughton, Nate Mantua, Lee R. HarrisonCoherence between coastal and river flooding along the California coast
Water levels around river mouths are intrinsically determined by sea level and river discharge. If storm-associated coastal water-level anomalies coincide with extreme river discharge, landscapes near river mouths will be flooded by the hydrodynamic interactions of these two water masses. Unfortunately, the temporal relationships between ocean and river water masses are not well understood. The coAuthorsKingsley O. Odigie, Jonathan Warrick - News
Below are news stories associated with this project.