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 will be derived from sediment cores.
This research is part of the project, “Sediment Transport in Coastal Environments.”
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 data or web applications associated with this project.
Bathymetric surveys collected near Dumbarton Bridge in south San Francisco Bay, California, 2008 to 2019
High-resolution (1 m) digital elevation model (DEM) of San Francisco Bay, California, created using bathymetry data collected between 1999 and 2020 (ver. 2.0, July 2021)
Pilot study on bathymetric change analyses in the Sacramento-San Joaquin Delta, California
Bathymetry, topography, and acoustic backscatter data, and a digital elevation model (DEM) of the Cache Slough Complex and Sacramento River Deep Water Ship Channel, Sacramento-San Joaquin Delta, California
Gravity cores from San Pablo Bay and Carquinez Strait, San Francisco Bay, California
Below are publications associated with this project.
Drivers of extreme water levels in a large, urban, high-energy coastal estuary – A case study of the San Francisco Bay
Shoreline retreat of the Corte Madera marshes, 1853 to 2016, Marin County, California
Morphodynamic resilience of intertidal mudflats on a seasonal time scale
Intertidal mudflats are morphodynamic features present in many estuaries worldwide. Often located between vegetated shores and deep channels they comprise valuable ecosystems and serve to protect the hinterland by attenuating waves. Although mudflats are persistently present on yearly to decadal time scales, little is known on their morphodynamic adaptation to short‐term variations in forcing such
A revised continuous surface elevation model for modeling
Slough evolution and legacy mercury remobilization induced by wetland restoration in South San Francisco Bay
Modeling morphodynamic development in the Alviso Slough system, South San Francisco Bay, California
How can climate change and engineered water conveyance affect sediment dynamics in the San Francisco Bay-Delta system?
Description of gravity cores from San Pablo Bay and Carquinez Strait, San Francisco Bay, California
A new seamless, high-resolution digital elevation model of the San Francisco Bay-Delta Estuary, California
Is “morphodynamic equilibrium” an oxymoron?
Mudflat morphodynamics and the impact of sea level rise in South San Francisco Bay
Bathymetric survey and digital elevation model of Little Holland Tract, Sacramento-San Joaquin Delta, California
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 will be derived from sediment cores.
This research is part of the project, “Sediment Transport in Coastal Environments.”
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 data or web applications associated with this project.
Bathymetric surveys collected near Dumbarton Bridge in south San Francisco Bay, California, 2008 to 2019
High-resolution (1 m) digital elevation model (DEM) of San Francisco Bay, California, created using bathymetry data collected between 1999 and 2020 (ver. 2.0, July 2021)
Pilot study on bathymetric change analyses in the Sacramento-San Joaquin Delta, California
Bathymetry, topography, and acoustic backscatter data, and a digital elevation model (DEM) of the Cache Slough Complex and Sacramento River Deep Water Ship Channel, Sacramento-San Joaquin Delta, California
Gravity cores from San Pablo Bay and Carquinez Strait, San Francisco Bay, California
Below are publications associated with this project.
Drivers of extreme water levels in a large, urban, high-energy coastal estuary – A case study of the San Francisco Bay
Shoreline retreat of the Corte Madera marshes, 1853 to 2016, Marin County, California
Morphodynamic resilience of intertidal mudflats on a seasonal time scale
Intertidal mudflats are morphodynamic features present in many estuaries worldwide. Often located between vegetated shores and deep channels they comprise valuable ecosystems and serve to protect the hinterland by attenuating waves. Although mudflats are persistently present on yearly to decadal time scales, little is known on their morphodynamic adaptation to short‐term variations in forcing such