We investigate mechanisms of sediment transport, resuspension dynamics in shoals, wave evolution in the shallows, wave attenuation in marshes, and transport of sediment between mudflats and marshes. We produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
This research is part of the project, “Sediment Transport in Coastal Environments.”
Objectives
Investigate mechanisms of sediment transport from shoals to channels
Investigate resuspension dynamics in subtidal and intertidal shoals, and determine critical shear stresses for these environments
Investigate wave evolution in the shallows, because of its critical importance to sediment resuspension
Investigate wave attenuation in marshes
Investigate transport of sediment between mudflats and marshes
Produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
Accomplishments
Four large deployments (30-40 instruments at 5-8 stations) measuring waves, currents, turbulence, and suspended sediment concentration have been completed: two in South San Francisco Bay, focused on exchange between shoal and channel, in collaboration with UC Berkeley; and two in San Pablo Bay, focused on transport between intertidal and subtidal regions, as part of a post-doctoral research project. See a video on this project. A smaller deployment in Corte Madera Bay was also completed, focused on wave attenuation in the shallows, as part of a larger San Francisco Bay Conservation and Development Commission project.
Learn about all of the “Sediment Transport in Coastal Environments” research studies by choosing a title below.
Sediment Transport in Coastal Environments
Coastal watershed and estuary restoration in the Monterey Bay area
Transport of invasive microorganisms
Sediment transport in submarine canyons
Columbia River estuary
Sediment transport between estuarine habitats in San Francisco Bay
Drag and sediment transport: conditions at the bottom boundary
San Francisco Bay geomorphology
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.
- Overview
We investigate mechanisms of sediment transport, resuspension dynamics in shoals, wave evolution in the shallows, wave attenuation in marshes, and transport of sediment between mudflats and marshes. We produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.
This research is part of the project, “Sediment Transport in Coastal Environments.”
Objectives
Investigate mechanisms of sediment transport from shoals to channels
Investigate resuspension dynamics in subtidal and intertidal shoals, and determine critical shear stresses for these environments
Investigate wave evolution in the shallows, because of its critical importance to sediment resuspension
Investigate wave attenuation in marshes
Investigate transport of sediment between mudflats and marshes
Produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.Accomplishments
Four large deployments (30-40 instruments at 5-8 stations) measuring waves, currents, turbulence, and suspended sediment concentration have been completed: two in South San Francisco Bay, focused on exchange between shoal and channel, in collaboration with UC Berkeley; and two in San Pablo Bay, focused on transport between intertidal and subtidal regions, as part of a post-doctoral research project. See a video on this project. A smaller deployment in Corte Madera Bay was also completed, focused on wave attenuation in the shallows, as part of a larger San Francisco Bay Conservation and Development Commission project.
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. The amount of sediment supplied to estuaries is important to the fate of shallow water habitats, including mudflats and tidal marshes. In San Francisco Bay, U.S. Geological Survey scientists and collaborators are investigating the influence of tides, waves, and water levels on sediment delivery and deposition in wave-exposed tidal salt marshes. - Science
Learn about all of the “Sediment Transport in Coastal Environments” research studies by choosing a title below.
Sediment Transport in Coastal Environments
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...Coastal watershed and estuary restoration in the Monterey Bay area
Objectives: Support further work by the USGS and collaborating federal, state, and local agencies and academic partners in analyzing the effectiveness of restoration work in coastal watersheds and estuaries in the Monterey Bay area. The USGS will play a supporting role in field efforts led by NOAA and California State University - Monterey Bay to measure physical and ecological changes in the...Transport of invasive microorganisms
The objectives of his project are to investigate the vectors and timing of microbiological invasions and the subsequent dispersal of these non-native organisms due to sediment transport. We will attempt to confirm the identification of specific invasives encountered with molecular sequencing, monitor the spread of the invading populations through their recent distribution and the historic...Sediment transport in submarine canyons
Objectives: Produce a step-change in understanding of submarine turbidity currents by measuring their two key features (synchronous velocity and concentration profiles) in detail (every 2-to-30 seconds) for the first time, and documenting spatial changes in their flow velocity from source-to-sink for the first time.Columbia River estuary
This research is part of the project “Sediment Transport in Coastal Environments.” We aim to support regional sediment management in the Columbia River littoral cell by monitoring and modeling shoreline change, modeling fate of disposed dredged material, and studying bedform morphology.Sediment transport between estuarine habitats in San Francisco Bay
We investigate mechanisms of sediment transport, resuspension dynamics in shoals, wave evolution in the shallows, wave attenuation in marshes, and transport of sediment between mudflats and marshes. We produce data sets for calibration of and comparison with sediment transport models, including wave parameters, suspended sediment concentration, and sediment flux.Drag and sediment transport: conditions at the bottom boundary
Research on bed sediment grain size, bedform morphology, vegetation characteristics, and sediment resuspension and transport.San Francisco Bay geomorphology
The primary objective of this task is to develop tools for predicting the long-term geomorphic evolution of estuaries. Sediment core and historical change analysis will be used in combination with interpretation of high-resolution seismic profiles to develop tools for predicting geomorphic evolution of estuaries. Historical change analysis will use hydrographic and lidar data. Longer-term data... - Data
- 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