The USGS Coastal Storm Modeling System (CoSMoS) team has extensively studied overland flooding and coastal change due to rising seas and storms. Interactions with coastal stakeholders have elucidated another important question; will rising seas also intrude into coastal aquifers and raise groundwater tables? The CoSMoS-Groundwater (CoSMoS-GW) modeling effort seeks to provide initial insight into this question for the entire California coastline, as well as San Francisco Bay.
Why CoSMoS-GW
As sea levels rise, the shallow groundwater table in coastal communities will also rise (Befus et al. 2020). This slow but chronic threat can flood communities from below, damaging buried infrastructure, flooding below grade structures, reducing storm sewer capacity, liberating pollutants, compromising foundations, and emerging above ground as an urban flood hazard that can amplify overland storm flooding. As communities develop climate adaptation plans to address sea level rise and extreme storm events, it is important to consider this additional hazard.
An initial study by Hoover et al. 2017 found that groundwater shoaling (or the rising of groundwater toward the ground surface) due to sea-level rise could result in significant hazards in three coastal California sites with shallow well data, but risk assessment for other areas was limited by a lack of data.
Through continued discussions with coastal California stakeholders, it became clear that more detailed information and modeling for this hazard was imminently needed. In response, the USGS Coastal Climate Impacts project team partnered with Dr. Kevin Befus (U. Arkansas) to model the impacts of rising seas on shallow coastal groundwater. Building on the initial work of the Coastal Storm Modeling System (CoSMoS), the team developed the model-driven, observation-validated CoSMoS-Groundwater (CoSMoS-GW) tool to predict representative coastal groundwater conditions today and into the future.
Modeling Details
CoSMoS-GW mapping is based on steady-state groundwater flow modeled in three dimensions using the USGS MODFLOW program. Water tables for present-day to +5 meters are simulated separately over 12 sea level rise increments, allowing water tables to equilibrate to each sea-level scenario based on two tidal datums, local mean sea level (LMSL) and mean higher high waters (MHHW). These datums bracket the range of likely elevations where groundwater would discharge at the coast. Interannual, seasonal, and daily fluctuations are not considered, nor are any human activities (e.g., pumping, drains, augmentation).
A series of overlapping groundwater flow models, ten within the Bay Area alone, provide high-resolution (10 m by 10 m) predictions that are merged for continuous groundwater results. Model inputs include very high resolution (2m by 2m) digital land surface models (DEMs) derived primarily from LiDAR topography-bathymetry data, gridded effective average groundwater recharge rates from 2000-2013, ocean salinity, and tidal datum elevations for setting present-day and higher sea levels. Unknown 3D hydrogeology is represented in the models by varying the hydraulic conductivity three orders of magnitude (0.1-10 m/day) while setting the lower impermeable boundary as a flat layer at -50 m NAVD88.
Modeled present-day water table elevations (i.e., hydraulic heads) are validated against State Water Resources Control Board GeoTracker, USGS, and California Department of Water Resources well observations, totaling approximately 3000 locations.
The modeled steady state (i.e., equilibrium) groundwater surface represents the long-term average elevation of the groundwater table that would occur for groundwater discharging along the coast at the tidal datum used (LMSL or MHHW). The resulting water table can be viewed as a baseline that then would be overprinted by seasonal, tidal, and other transient signals such as storms. Areas of emergent groundwater (when the groundwater table rises to or above the surface of the ground and create surface flooding) are likely to experience chronic ‘sunny day’ surface flooding (i.e., surface flooding in the absence of heavy precipitation) and compound flooding from surface runoff during storms.
Stakeholder Engagement
The development of this model was informed by a workshop with a broad group of technical experts who have studied this hazard in other coastal settings (see technical advisory team members below). Initial findings from the research were discussed with key coastal and San Francisco Bay partners during a workshop in November 2019. We continue to work closely with partners across California to share this science and make it usable and accessible to coastal managers for their coastal planning needs.
The results from CoSMoS-GW are publicly available on the USGS ScienceBase data catalog and on HydroShare. The results will also be presented on the Our Coast Our Future web tool, managed by Point Blue Conservation Science, and associated socioeconomic analysis will be presented on the USGS Hazards Exposure Reporting and Analytics web tool.
CoSMoS-GW Technical Advisory Experts
- Tiffany Anderson, University of Hawaii, Manoa
- Chip Fletcher, University of Hawaii, Manoa
- Shellie Habel, University of Hawaii, Manoa
- Andy Fisher, University of California, Santa Cruz
- Graham Fogg, University of California, Davis
- Kristina Hill, University of California, Berkeley
- Michelle Hummel, University of Texas at Arlington
- John Masterson, USGS
- Ferdinand Oberle, USGS
- Chris Smith, USGS
- Kris May, Slivestrum
- Peter Swarzenski, USGS
Below are links to related CoSMoS models and information.
Coastal Storm Modeling System (CoSMoS)
CoSMoS 2.1: San Francisco Bay
CoSMoS 2.0: North-central California (outer coast)
Operational CoSMoS model: San Francisco Bay
Below are data or web applications associated with this project.
Projected responses of the coastal water table for California using present-day and future sea-level rise scenarios
Below are publications associated with this project.
Increasing threat of coastal groundwater hazards from sea-level rise in California
Sea-level rise and coastal groundwater inundation and shoaling at select sites in California, USA
Below are partners associated with this project.
- Overview
The USGS Coastal Storm Modeling System (CoSMoS) team has extensively studied overland flooding and coastal change due to rising seas and storms. Interactions with coastal stakeholders have elucidated another important question; will rising seas also intrude into coastal aquifers and raise groundwater tables? The CoSMoS-Groundwater (CoSMoS-GW) modeling effort seeks to provide initial insight into this question for the entire California coastline, as well as San Francisco Bay.
Why CoSMoS-GW
As sea levels rise, the shallow groundwater table in coastal communities will also rise (Befus et al. 2020). This slow but chronic threat can flood communities from below, damaging buried infrastructure, flooding below grade structures, reducing storm sewer capacity, liberating pollutants, compromising foundations, and emerging above ground as an urban flood hazard that can amplify overland storm flooding. As communities develop climate adaptation plans to address sea level rise and extreme storm events, it is important to consider this additional hazard.
An initial study by Hoover et al. 2017 found that groundwater shoaling (or the rising of groundwater toward the ground surface) due to sea-level rise could result in significant hazards in three coastal California sites with shallow well data, but risk assessment for other areas was limited by a lack of data.
Through continued discussions with coastal California stakeholders, it became clear that more detailed information and modeling for this hazard was imminently needed. In response, the USGS Coastal Climate Impacts project team partnered with Dr. Kevin Befus (U. Arkansas) to model the impacts of rising seas on shallow coastal groundwater. Building on the initial work of the Coastal Storm Modeling System (CoSMoS), the team developed the model-driven, observation-validated CoSMoS-Groundwater (CoSMoS-GW) tool to predict representative coastal groundwater conditions today and into the future.
Modeling Details
CoSMoS-GW mapping is based on steady-state groundwater flow modeled in three dimensions using the USGS MODFLOW program. Water tables for present-day to +5 meters are simulated separately over 12 sea level rise increments, allowing water tables to equilibrate to each sea-level scenario based on two tidal datums, local mean sea level (LMSL) and mean higher high waters (MHHW). These datums bracket the range of likely elevations where groundwater would discharge at the coast. Interannual, seasonal, and daily fluctuations are not considered, nor are any human activities (e.g., pumping, drains, augmentation).
A series of overlapping groundwater flow models, ten within the Bay Area alone, provide high-resolution (10 m by 10 m) predictions that are merged for continuous groundwater results. Model inputs include very high resolution (2m by 2m) digital land surface models (DEMs) derived primarily from LiDAR topography-bathymetry data, gridded effective average groundwater recharge rates from 2000-2013, ocean salinity, and tidal datum elevations for setting present-day and higher sea levels. Unknown 3D hydrogeology is represented in the models by varying the hydraulic conductivity three orders of magnitude (0.1-10 m/day) while setting the lower impermeable boundary as a flat layer at -50 m NAVD88.
Examples of CoSMoS-GW mapping products that show (left) modeled current groundwater tables with red depicting sites of emergent groundwater and (right) groundwater tables with 6 feet of sea-level rise. Blue indicates coastal-driven flooding and inundation. Both figures are for a horizontal hydraulic conductivity of 1.0 m/d and LMSL tidal datum. Modeled present-day water table elevations (i.e., hydraulic heads) are validated against State Water Resources Control Board GeoTracker, USGS, and California Department of Water Resources well observations, totaling approximately 3000 locations.
The modeled steady state (i.e., equilibrium) groundwater surface represents the long-term average elevation of the groundwater table that would occur for groundwater discharging along the coast at the tidal datum used (LMSL or MHHW). The resulting water table can be viewed as a baseline that then would be overprinted by seasonal, tidal, and other transient signals such as storms. Areas of emergent groundwater (when the groundwater table rises to or above the surface of the ground and create surface flooding) are likely to experience chronic ‘sunny day’ surface flooding (i.e., surface flooding in the absence of heavy precipitation) and compound flooding from surface runoff during storms.
Stakeholder Engagement
Workshop attendees discuss the emerging phenomenon of a rising groundwater table due to sea-level rise. They addressed the challenges currently faced, and anticipated future challenges with rising water tables. The development of this model was informed by a workshop with a broad group of technical experts who have studied this hazard in other coastal settings (see technical advisory team members below). Initial findings from the research were discussed with key coastal and San Francisco Bay partners during a workshop in November 2019. We continue to work closely with partners across California to share this science and make it usable and accessible to coastal managers for their coastal planning needs.
The results from CoSMoS-GW are publicly available on the USGS ScienceBase data catalog and on HydroShare. The results will also be presented on the Our Coast Our Future web tool, managed by Point Blue Conservation Science, and associated socioeconomic analysis will be presented on the USGS Hazards Exposure Reporting and Analytics web tool.
CoSMoS-GW Technical Advisory Experts
- Tiffany Anderson, University of Hawaii, Manoa
- Chip Fletcher, University of Hawaii, Manoa
- Shellie Habel, University of Hawaii, Manoa
- Andy Fisher, University of California, Santa Cruz
- Graham Fogg, University of California, Davis
- Kristina Hill, University of California, Berkeley
- Michelle Hummel, University of Texas at Arlington
- John Masterson, USGS
- Ferdinand Oberle, USGS
- Chris Smith, USGS
- Kris May, Slivestrum
- Peter Swarzenski, USGS
- Science
Below are links to related CoSMoS models and information.
Coastal Storm Modeling System (CoSMoS)
The Coastal Storm Modeling System (CoSMoS) makes detailed predictions of storm-induced coastal flooding, erosion, and cliff failures over large geographic scales. CoSMoS was developed for hindcast studies, operational applications and future climate scenarios to provide emergency responders and coastal planners with critical storm-hazards information that can be used to increase public safety...CoSMoS 2.1: San Francisco Bay
With primary support from the National Estuarine Research Reserve (NERR), CoSMoS is set-up within the San Francisco Bay as part of Our Coast Our Future (OCOF).CoSMoS 2.0: North-central California (outer coast)
Our Coast Our Future (OCOF) is a collaborative, user-driven project providing science-based decision-support tools to help coastal planners and emergency responders understand, visualize, and anticipate local impacts from sea-level rise (SLR) and storms in the San Francisco Bay region.Operational CoSMoS model: San Francisco Bay
The San Francisco Bay Coastal Flood Forecast pilot project is an operational CoSMoS model, part of a project funded by the California Department of Water Resources (CA-DWR) and NOAA’s Earth System Research Laboratory (ESRL). - Data
Below are data or web applications associated with this project.
Projected responses of the coastal water table for California using present-day and future sea-level rise scenarios
Coastal groundwater levels (heads) can increase with sea level rise (SLR) where shallow groundwater floats on underlying seawater. In some areas coastal groundwater could rise almost as much as SLR, but where rising groundwater intersects surface drainage features, the increase will be less. Numerical modeling can provide insight into coastal areas that may be more or less vulnerable to hazards as - Publications
Below are publications associated with this project.
Increasing threat of coastal groundwater hazards from sea-level rise in California
Projected sea-level rise will raise coastal water tables, resulting in groundwater hazards that threaten shallow infrastructure and coastal ecosystem resilience. Here we model a range of sea-level rise scenarios to assess the responses of water tables across the diverse topography and climates of the California coast. With 1 m of sea-level rise, areas flooded from below are predicted to expand ~50AuthorsK.M. Befus, Patrick L. Barnard, Daniel J. Hoover, Juliette Finzi Hart, Clifford I. VossSea-level rise and coastal groundwater inundation and shoaling at select sites in California, USA
Study regionThe study region spans coastal California, USA, and focuses on three primary sites: Arcata, Stinson Beach, and Malibu Lagoon.Study focus1 m and 2 m sea-level rise (SLR) projections were used to assess vulnerability to SLR-driven groundwater emergence and shoaling at select low-lying, coastal sites in California. Separate and combined inundation scenarios for SLR and groundwater emergenAuthorsDaniel J. Hoover, Kingsley Odigie, Peter W. Swarzenski, Patrick L. Barnard - Partners
Below are partners associated with this project.