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Logan, J. B.; Winklerprins, L. T.; Lacy, J. R. 2023. Structure-from-motion derived orthomosaic imagery and digital surface models (DSMs) from the intertidal region at Whale's Tail Marsh, South San Francisco Bay, CA. United States Geological Survey: South San Francisco Bay, CA.

This data release presents digital surface models (DSMs) and orthomosaic images of the Whale's Tail Marsh region of South San Francisco Bay, CA. The data were created using structure-from-motion (SfM) processing of repeat aerial imagery collected from fixed-wing aircraft. The raw images were acquired from an approximate altitude of 427 meters (1,400 feet) above ground level (AGL), using a Hasselblad A6D-100c camera fitted with an HC 80 lens, resulting in a nominal ground-sample-distance (GSD) of 2.5 centimeters per pixel. The acquisition flight lines were designed to provide approximately 50 percent overlap between adjacent flight lines (sidelap), with approximately 70 percent overlap between sequential images along the flight line (forelap). Survey control was established using an onboard camera-synchronized dual-frequency GPS system as well as ground control points (GCPs) distributed throughout the survey area and measured using survey-grade post-processed kinematic (PPK) GPS. Both the data from the onboard GPS and from the GPS used to measure the GCPs were post-processed using a nearby Continuously Operating Reference Station (CORS) operated by the National Geodetic Survey (NGS). Structure-from-motion processing of these data was conducted using a "4D" processing workflow in which imagery from each of the different acquisition dates were co-aligned to increase relative spatial precision between the final data products.

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Jones, C.; Davis, J.; Yee, D. 2022. Strategy for In-Bay Fate Modeling to Support Contaminant and Sediment Management in San Francisco Bay. SFEI Contribution No. 1090. San Francisco Estuary Institute: Richmond, California.

This report presents a strategy and multi-year workplan for modeling polychlorinated biphenyls (PCBs), contaminants of emerging concern (CECs), and sediment in San Francisco Bay (the Bay). Robust in-Bay fate modeling is needed to address priority management questions that have been identified for these constituents.

The strategy for in-Bay modeling presented in this report is a major element of a broader, integrated strategy that is being developed across RMP Workgroups for modeling contaminants flowing from the Bay watersheds and other pathways into the Bay. The broader project is expected to yield an integrated strategy in 2022, followed by implementation of a pilot effort in 2023. Coordination of the in-Bay modeling effort with the broader integrated strategy and other modeling work (e.g., nutrient modeling under the Nutrient Management Strategy) will be critical to optimizing use of the funds allocated to modeling.

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Cohen, A. N. 1994. Storming the Bay. Terrain 24, 4,7.
Cohen, A. N. 1996. Stopping ballast water invaders. Native Species Network 1, 1.
Zi, T. 2023. Stevens Creek Reservoir – Forecast Informed Reservoir Operation (FIRO) Phase One Report. Peterson, D., Stark, K., Eds.. SFEI Contribution No. 1120. Prepared for SCV Water District.
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Trowbridge, P. 2018. Status & Trends Monitoring Design: 2018 Update. San Francisco Estuary Institute : Richmond, CA.
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Cohen, A. N. 1999. Status of invasions and policy response on the U. S. west coast. First National Conference on Marine Bioinvasions.
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O'Connor, J. M.; Daum, T. H. 1992. Status and Assessment of Selected Monitoring Programs in the San Francisco Esturary. SFEI Contribution No. 172. San Francisco Estuary Institute: Richmond, Ca. p 128.
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Lowe, S.; Josh Collins; Pearce, S. 2013. Statistical Design, Analysis, and Graphics for the Guadalupe River Watershed Assessment 2012. SFEI Contribution No. 687. San Francisco Estuary Institute: Richmond, CA.
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Connor, M. S.; Davis, J. A. 2008. The State of San Francisco Bay: Water Quality. National Water Quality Monitoring Conference.
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Grossinger, R. M.; Wheeler, M.; Spotswood, E.; Ndayishimiye, E.; Carbone, G.; Galt, R. 2020. Sports and urban biodiversity. . SFEI Contribution No. 1028.

SFEI collaborated with the International Union for the Conservation of Nature (IUCN) and the International Olympic Committee (IOC) to create a guide to incorporating nature into urban sports, from the development of Olympic cities to the design and management of the many sport fields throughout the urban landscape. We applied the Urban Biodiversity Framework developed in Making Nature’s City to the world of sports, with case studies drawn from international sport federations, Olympic cities, and individual sport teams and venues around the world. The guide is part of IUCN’s ongoing collaboration with IOC to develop best practices around biodiversity for the sporting industry.

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McKnight, K.; Lowe, J.; Plane, E. 2020. Special Study on Bulk Density. SFEI Contribution No. 975. San Francisco Estuary Institute: Richmond, CA. p 43.

Sediment bulk density is the total mass of mineral and organic sediment within a defined volume. It is a key variable in many research questions pertaining to Bay sediment studies but one that is often poorly quantified and can be misinterpreted. The motivation for this report comes from a recommendation by Schoellhamer et al. (2018) to compile more accurate estimates of bulk density of Bay sediments to convert between volume and mass with a higher level of certainty. Through funding and guidance from the Bay Regional Monitoring Program Sediment Work Group, this report is a first step towards compiling the available data on sediment bulk densities across Bay habitats and along salinity gradients to provide better information for resource managers and others working on sediment-related issues. This report discusses the need to know the bulk density of Bay soils to convert between sediment mass and soil volume; clarifies general definitions and common points of confusion related to sediment bulk density; compiles primary sources of bulk density measurements, secondary sources of bulk density estimates, and standard engineering estimates of bulk density for different habitats in San Francisco Bay; and, provides a database where practitioners can track, analyze, and share bulk density measurements.
 

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Abu-Saba, K. E. 1998. Spatial and Temporal Variability in the Aquatic Cycling of Chromium. SFEI Contribution No. 220. University of California: Santa Cruz, CA.
Greenfield, B. K. 2008. Spatial and temporal patterns in food web accumulation of Hg. San Francisco Bay Mercury Coordination Meeting.
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Collins, J. N.; Wittner, E.; Grosso, C. 2003. South Bay Updates Modern Baylands Habitat Coverage Bay Area EcoAtlas Information System. SFEI Contribution No. 282. San Francisco Estuary Institute: Oakland, CA.
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Davis, J. A.; Connor, M. S.; Flegal, A. R.; Conaway, C. H. 2007. Sources, transport, fate and toxicity of pollutants in the San Francisco Bay estuary. Environmental Research : A Multidisciplinary Journal of Environmental Sciences, Ecology and Public Health 105, 1-4.
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Oram, J. J.; McKee, L. J. .; Davis, J. A.; Sedlak, M.; Yee, D. 2008. Sources, Pathways and Loadings Workgroup: Five-Year Workplan (2008-12). SFEI Contribution No. 567. San Francisco Estuary Institute: Oakland.
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McKee, L. J. . 2005. Sources, Pathways, and Loadings: 5-Year Work Plan (2005-2009). SFEI Contribution No. 406. San Francisco Estuary Institute. p 25.
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Grossinger, R. M.; Dawson, A. 2002. Sonoma Valley Historical Ecology Project, Phase 1 Final Report. SFEI Contribution No. 254. Sonoma County Water Agency and the SF Estuary Project. p 8 pp. plus apps.
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Sonoma Land Trust and partners. 2020. Sonoma Creek Baylands Strategy. Prepared by Sonoma Land Trust, San Francisco Estuary Institute, Point Blue Conservation Science, Environmental Science Associates, Ducks Unlimited, U.S. Fish and Wildlife Service.
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Mckee, L.; Gilbreath, A.; Sabin, L. 2022. Small Tributaries Pollutants of Concern Reconnaissance Monitoring: Application of Storm-event Loads and Yields-Based and Congener-Based PCB Site Prioritization Methodologies. SFEI Contribution No. 1067.

Stormwater agencies in the San Francisco Bay Area are identifying watershed areas that are polluted with PCBs in order to prioritize management efforts to reduce impairment in the Bay caused by PCBs carried in stormwater. Water sampling during storms has been used to characterize PCB concentrations but management prioritization based on the comparison of concentrations between watersheds is made difficult due to variations in flow and sediment erosion between storms and in relation to varying land use. In addition, identifying PCB source areas within priority watersheds has proven complex and costly. To address these challenges, the San Francisco Bay Regional Monitoring Program (RMP) has developed two new interpretive methods based on storm-event PCB yields (PCBs mass per unit area per unit time) and fingerprints of Aroclors (commercial PCB mixtures) that make existing data more useful for decision-making. 

The objectives of this study were to: 

  • Apply the yield method to the regional stormwater dataset and provide new rankings, 
  • Estimate the presence of Aroclors in samples where congener data are available
  • Evaluate data weaknesses and recommend watersheds to resample, and
  • Classify watersheds into high, medium, and low categories for potential management.
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Greenfield, B. K.; Davis, J. A. 2004. A Simple Mass Balance Model for PAH Fate in the San Francisco Estuary. SFEI Contribution No. 115. San Francisco Estuary Institute: Oakland, CA.
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Flegal, A. R.; Smith, G. J. 1993. Silver in San Francisco Bay estuarine waters. Estuaries 16, 547-558 . SFEI Contribution No. 175.
Flegal, A. R.; Sanudo-Wilhelmy, S. A.; Rivera-Duarte, I. 1996. Silver contamination in aquatic environments. Reviews of Environmental Contamination and Toxicology 148, 139-162 . SFEI Contribution No. 192.
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Beagle, J.; Salomon, M.; Grossinger, R. M.; Baumgarten, S.; Askevold, R. A. 2015. Shifting Shores: Marsh Expansion and Retreat in San Pablo Bay. SFEI Contribution No. 751.

EXECUTIVE SUMMARY
As sea level rise accelerates, our shores will be increasingly vulnerable to erosion. Particular concern centers around the potential loss of San Francisco Bay’s much-valued tidal marshes, which provide natural flood protection to our shorelines, habitat for native wildlife, and many other ecosystem services. Addressing this concern, this study is the first systematic analysis of the rates of marsh retreat and expansion over time for San Pablo Bay, located in the northern part of San Francisco Bay.

Key findings:
• Over the past two decades, more of the marshes in San Pablo Bay have expanded (35% by length) than retreated (6%).
• Some areas have been expanding for over 150 years.
• Some marsh edges that appear to be retreating are in fact expanding rapidly at rates of up to 8 m/yr.
• Marsh edge change may be a useful indicator of resilience, identifying favorable sites for marsh persistence.
• These data can provide a foundation for understanding drivers of marsh edge expansion and retreat such as wind direction, wave energy, watershed sediment supply, and mudflat shape.
• This understanding of system dynamics will help inform management decisions about marsh restoration and protection.
• This study provides a baseline and method for tracking marsh edge response to current and future conditions, particularly anticipated changes in sea level, wave energy, and sediment supply.


Recommended next steps:
• This pilot study for San Pablo Bay marshes should be extended to other marshes in San Francisco Bay.
• These initial marsh expansion and retreat findings should be further analyzed and interpreted to improve our understanding of system drivers and identify management responses.
• A program for repeated assessment should be developed to identify and track changes in shoreline position, a leading indicator of the likelihood marsh survival.

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Whipple, A.; Grossinger, R. M.; Davis, F. W. 2010. Shifting Baselines in a California Oak Savanna: Nineteenth Century Data to Inform Restoration Scenarios. Restoration Ecology 19 (101), 88-101 . SFEI Contribution No. 593.

For centuries humans have reduced and transformed Mediterranean-climate oak woodland and savanna ecosystems, making it difficult to establish credible baselines for ecosystem structure and composition that can guide ecological restoration efforts. We combined historical data sources, with particular attention to mid-1800s General Land Office witness tree records and maps and twentieth century air photos, to reconstruct 150 years of decline in extent and stand density of Valley oak (Quercus lobata Neé) woodlands and savannas in the Santa Clara Valley of central coastal California. Nineteenth century Valley oak woodlands here were far more extensive and densely stocked than early twentieth century air photos would suggest, although reconstructed basal areas (7.5 m2/ha) and densities (48.9 trees/ha) were not outside the modern range reported for this ecosystem type. Tree densities and size distribution varied across the landscape in relation to soil and topography, and trees in open savannas were systematically larger than those in denser woodlands. For the largest woodland stand, we estimated a 99% decline in population from the mid-1800s to the 1930s. Although most of the study area is now intensely developed, Valley oaks could be reintroduced in urban and residential areas as well as in surrounding rangelands at densities comparable to the native oak woodlands and savannas, thereby restoring aspects of ecologically and culturally significant ecosystems, including wildlife habitat and genetic connectivity within the landscape.

Cohen, A. N.; Zabin, C. J. 2006. Shells as vectors. Proceedings of the 2006 West Coast Native Oyster Restoration Workshop.
Cohen, A. N.; Schaeffer, K.; Cosentino-Manning, N. 2007. Shellfish Beds in Report on the Subtidal Habitats and Associated Biological Taxa in San Francisco Bay. In Report on the Subtidal Habitats and Associated Biological Taxa in San Francisco Bay. Report on the Subtidal Habitats and Associated Biological Taxa in San Francisco Bay. NOAA National Marine Fisheries Service: Santa Rosa, CA. pp 50-55.
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May, C. L.; Mohan, A.; Plane, E.; Ramirez-Lopez, D.; Mak, M.; Luchinsky, L.; Hale, T.; Hill, K. 2022. Shallow Groundwater Response to Sea-Level Rise: Alameda, Marin, San Francisco, and San Mateo Counties. Pathways Climate Institute and San Francisco Estuary Institute.

The response of shallow groundwater to sea-level rise is a relatively new field of study. For low-lying coastal communities, sea-level rise adaptation efforts must consider the potential for groundwater rise to avoid maladaptation. The need to better understand this slow and chronic threat was identified as a critical data gap in the San Francisco Bay Area’s (Bay Area’s) adaptation efforts during the Bay Area Groundwater and Sea-Level Rise Workshop in 2019.

Pathways Climate Institute LLC (Pathways) and the San Francisco Estuary Institute (SFEI) gathered and analyzed multiple data sets and collaborated with city and county partners to analyze and map the existing “highest annual” shallow groundwater table and its likely response to future sea-level rise. This effort covers four counties (Alameda, Marin, San Francisco, San Mateo) and was funded by the Bay Area Council’s California Resilience Challenge. The study focused on the San Francisco Bay side of each county and does not include the Pacific coastline of Marin, San Francisco, nor San Mateo Counties. An advisory committee composed of city and county representatives provided essential support by gathering data and reviewing depth-to-groundwater maps. Additional academic and agency advisors participated in project team meetings and informed project direction. This effort produced the following publicly available data and online tools to support adaptation efforts:

  • Existing and future condition depth to groundwater GIS data available for download (geodatabase format).
  • A StoryMap providing background information and graphical representations of the processes and impacts of groundwater rise.
  • Web maps showing: (1) existing depth to groundwater; and (2) a comparison of the extent of emergent groundwater to the extent of coastal flooding under various sea-level-rise scenarios.
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Flegal, A. R.; Conaway, C. H.; Kerin, E. 2002. Sequential Extraction of Mercury from Sediments in San Francisco Bay Estuary. Environmental Science and Technology . SFEI Contribution No. 126.
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Sun, J.; Davis, J. A.; Stewart, R.; Palace, V. 2019. Selenium in White Sturgeon from North San Francisco Bay: The 2015-2017 Sturgeon Derby Study. SFEI Contribution No. 897. San Francisco Estuary Institute: Richmond, CA.

This report presents the findings from a study evaluating selenium concentrations in white sturgeon (Acipenser transmontanus) tissues collected during the 2015-2017 Sturgeon Derby events in North San Francisco Bay. The goal of this study was to investigate the distribution of selenium among sturgeon tissues to inform the toxicological and regulatory interpretation of selenium measured in non-lethally collected tissues, including muscle plugs and fin rays. This technical report provides documentation of the study and presents its major findings.

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Jabusch, T. W. 2010. Selenium in the Grasslands Watershed. San Francisco Estuary Institute: Oakland, CA. pp 267-294.
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Sun, J.; Davis, J.; Stewart, R. 2018. Selenium in Muscle Plugs of White Sturgeon from North San Francisco Bay, 2015-2017. SFEI Contribution No. 929. San Francisco Estuary Institute : Richmond, CA.
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Foley, M. M.; Davis, J. A.; Buzby, N. 2024. Selenium Concentrations in Water and Clams in North San Francisco Bay, 2019-2020. SFEI Contribution No. 1116. San Francisco Estuary Institute: Richmond, CA.

The Regional Monitoring Program for Water Quality in San Francisco Bay (RMP) started implementing a new design for North Bay selenium (Se) sampling in 2019 after a long-term USGS program was terminated in 2017. To determine if the RMP sampling and analysis methods are producing similar results to the USGS study, we compared Se concentrations and stable isotope values in clams at two stations in Suisun Bay, California, that were sampled by the USGS long-term monitoring program from 1995-2010 and the RMP in 2019-2020. We also compared Se concentrations in water (dissolved and particulate) from the RMP Status and Trends sampling in Suisun Bay (1993-2019) to the samples collected as part of this study. 

Spatial patterns in clam Se concentrations between the USGS and RMP studies were similar, with lower concentrations at Station 4.1 (Suisun Bay) than at Station 8.1 (Carquinez Strait). Se concentrations at both stations were consistently lower for the RMP samples than those reported in the long-term USGS dataset. Stable isotope values for δ13C and δ15N were similar for the USGS and RMP samples with δ13C and δ15N more enriched at Station 8.1 than 4.1. However, there was not close alignment of the RMP samples to the USGS long-term average, particularly at Station 8.1. Average dissolved Se concentrations in water were consistently lower than the long-term average at Station 4.1 and similar to or above the long-term RMP Status and Trends (S&T) average at Station 8.1. Particulate Se concentrations at Stations 4.1 and 8.1 were nearly one-third of the long-term S&T average in Suisun Bay, likely due to a change in methods for calculating particulate Se. 

Additional information is needed to evaluate whether the lower Se concentrations measured in clams as part of the RMP study could be suggestive of declining Se concentrations in North Bay clams between 2010 and 2019 or an artifact of the new analytical lab. Additional data from samples collected by the USGS from 2011-2017 should be examined to fill the gap between the datasets. Continued RMP monitoring will also be valuable in evaluating long-term trends.

 

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Gunther, A. J. 1987. The Segmentation of the San Francisco Bay/Delta. SFEI Contribution No. 135. San Francisco Estuary Institute: Richmond, CA. p 18.
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Grossinger, R. M. 1999. Seeing Time: A Historical Approach to Restoration. Ecological Restoration 17, 251-2. . SFEI Contribution No. 328.
Warner, J. C.; Burau, J. R.; Schoellhamer, D. H. 1997. A sediment transport pathway in the back of a nearly semienclosed subembayment of San Francisco Bay, California. Environmental and Coastal Hydraulics: Protecting the Aquatic Habitat(Proceedings of Theme B., F.M. Holly, A. Alsaffar, S.S.Y. Wang, T. Carstens eds.) 2, 1096-1101 . SFEI Contribution No. 29.
Barnard, P. L.; Schoellhamer, D. H.; Jaffe, B. E.; McKee, L. J. . 2013. Sediment transport in the San Francisco Bay Coastal System: An overview. Marine Geology Special Issue: A multi-discipline approach for understanding sediment transport and geomorphic evolution in an estuarine-coastal system.
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Schoellhamer, D.; McKee, L.; Pearce, S.; Kauhanen, P.; Salomon, M.; Dusterhoff, S.; Grenier, L.; Marineau, M.; Trowbridge, P. 2018. Sediment Supply to San Francisco Bay. SFEI Contribution No. 842. San Francisco Estuary Institute : Richmond, CA.
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