Publications
Scientific reports, journal articles, and information products produced by USGS Pacific Coastal and Marine Science Center scientists.
Filter Total Items: 1417
Macondo-1 well oil in sediment and tarballs from the northern Gulf of Mexico shoreline Macondo-1 well oil in sediment and tarballs from the northern Gulf of Mexico shoreline
From April 20 through July 15, 2010, an estimated 4.4 million barrels (1 barrel = 42 gallons [~700,000 cu m]) of crude oil spilled into the northern Gulf of Mexico (nGOM) from the ruptured British Petroleum (BP) Macondo-1 (M-1) well after the explosion of the drilling platform Deepwater Horizon. In addition, ~1.84 million gallons (~7,000 cu m) of hydrocarbon-based Corexit dispersants...
Authors
Florence L. Wong, Robert J. Rosenbauer, Pamela L. Campbell, Angela Lam, T.D. Lorenson, Frances D. Hostettler, Burt Thomas
Suspended sediment and organic contaminants in the San Lorenzo River, California, water years 2009-2010 Suspended sediment and organic contaminants in the San Lorenzo River, California, water years 2009-2010
This report presents analyses of suspended sediment and organic contaminants measured during a two-year study of the San Lorenzo River, central California, which discharges into the Pacific Ocean within the Monterey Bay National Marine Sanctuary. Most suspended-sediment transport occurred during flooding caused by winter storms; 55 percent of the sediment load was transported by the...
Authors
Amy E. Draut, Christopher H. Conaway, Kathy R. Echols, Curt D. Storlazzi, Andrew Ritchie
The dynamics of fine-grain sediment dredged from Santa Cruz Harbor The dynamics of fine-grain sediment dredged from Santa Cruz Harbor
In the fall and early winter of 2009, a demonstration project was done at Santa Cruz Harbor, California, to determine if 450 m3/day of predominantly (71 percent) mud-sized sediment could be dredged from the inner portion of the harbor and discharged to the coastal ocean without significant impacts to the beach and inner shelf. During the project, more than 7600 m3 of sediment (~5400 m3...
Authors
Curt D. Storlazzi, Christopher H. Conaway, M. Katherine Presto, Joshua B. Logan, Katherine Cronin, Maarten van Ormondt, Jamie Lescinski, E. Lynne Harden, Jessica R. Lacy, Pieter K. Tonnon
Recent scientific advances and their implications for sand management near San Francisco, California: The influences of the ebb tidal delta Recent scientific advances and their implications for sand management near San Francisco, California: The influences of the ebb tidal delta
Recent research in the San Francisco, California, U.S.A., coastal region has identified the importance of the ebb tidal delta to coastal processes. A process-based numerical model is found to qualitatively reproduce the equilibrium size and shape of the delta. The ebb tidal delta itself has been contracting over the past century, and the numerical model is applied to investigate the...
Authors
Daniel M. Hanes, Patrick L. Barnard, Kate Dallas, Edwin Elias, Li H. Erikson, Jodi Eshleman, Jeff Hansen, Tian Jian Hsu, Fengyan Shi
The influence of sea-level rise on fringing reef sediment dynamics: field observations and numerical modeling The influence of sea-level rise on fringing reef sediment dynamics: field observations and numerical modeling
While most climate projections suggest that sea level may rise on the order of 0.5-1.0 m by 2100, it is not clear how fluid flow and sediment transport on fringing reefs might change in response to this rapid sea-level rise. Field observations and numerical modeling suggest that an increase in water depth on the order of 0.5-1.0 m on a fringing reef flat would result in larger...
Authors
Curt D. Storlazzi, Michael E. Field, Edwin Elias, M. Katherine Presto
Does littoral sand bypass the head of Mugu Submarine Canyon? - a modeling study Does littoral sand bypass the head of Mugu Submarine Canyon? - a modeling study
A newly developed sand-tracer code for the process-based model Delft3D (Deltares, The Netherlands) was used to simulate the littoral transport near the head of the Mugu Submarine Canyon in California, USA. For westerly swells, which account for more than 90% of the wave conditions in the region, the sand tracers in the downcoast littoral drift were unable to bypass the canyon head. A...
Authors
Jingping Xu, Edwin Elias, Nicole Kinsman
A numerical model investigation of the formation and persistence of an erosion hotspot A numerical model investigation of the formation and persistence of an erosion hotspot
A Delft3D-SWAN coupled flow and wave model was constructed for the San Francisco Bight with high-resolution at 7 km-long Ocean Beach, a high-energy beach located immediately south of the Golden Gate, the sole entrance to San Francisco Bay. The model was used to investigate tidal and wave-induced flows, basic forcing terms, and potential sediment transport in an area in the southern...
Authors
Jeff E. Hansen, Edwin Elias, Jeffrey H. List, Patrick L. Barnard
Isostatic gravity map of the Point Sur 30' x 60' quadrangle and adjacent areas, California Isostatic gravity map of the Point Sur 30' x 60' quadrangle and adjacent areas, California
This isostatic residual gravity map is part of a regional effort to investigate the tectonics and water resources of the central Coast Range. This map serves as a basis for modeling the shape of basins and for determining the location and geometry of faults in the area. Local spatial variations in the Earth's gravity field (after removing variations caused by instrument drift, earth...
Authors
J. T. Watt, R. L. Morin, V.E. Langenheim
Flow speed estimated by inverse modeling of sandy sediment deposited by the 29 September 2009 tsunami near Satitoa, east Upolu, Samoa Flow speed estimated by inverse modeling of sandy sediment deposited by the 29 September 2009 tsunami near Satitoa, east Upolu, Samoa
Sandy deposits from the 29 September 2009 tsunami on the east coast of Upolu, Samoa were investigated to document their characteristics and used to apply an inverse sediment transport model to estimate tsunami flow speed. Sandy deposits 6 to 15 cm thick formed from ~ 25 to ~ 250 m inland. Sedimentary layers in the deposits, that are defined by vertical grain size variation and contacts...
Authors
Bruce E. Jaffe, Mark Buckley, Bruce M. Richmond, Luke Strotz, Samuel Etienne, Kate Clark, Steve Watt, Guy R. Gelfenbaum, James Goff
More than 100 Years of Background-Level Sedimentary Metals, Nisqually River Delta, South Puget Sound, Washington More than 100 Years of Background-Level Sedimentary Metals, Nisqually River Delta, South Puget Sound, Washington
The Nisqually River Delta is located about 25 km south of the Tacoma Narrows in the southern reach of Puget Sound. Delta evolution is controlled by sedimentation from the Nisqually River and erosion by strong tidal currents that may reach 0.95 m/s in the Nisqually Reach. The Nisqually River flows 116 km from the Cascade Range, including the slopes of Mount Rainier, through glacially...
Authors
Renee K. Takesue, Peter W. Swarzenski
Insights on the 2009 South Pacific tsunami in Samoa and Tonga from field surveys and numerical simulations Insights on the 2009 South Pacific tsunami in Samoa and Tonga from field surveys and numerical simulations
An Mw ≈ 8.1 earthquake south of the Samoan Islands on 29 September 2009 generated a tsunami that killed 189 people. From 4 to 11 October, an International Tsunami Survey Team surveyed the seven major islands of the Samoan archipelago. The team measured locally focused runup heights of 17 m at Poloa and inundation of more than 500 m at Pago Pago. A follow-up expedition from 23 to 28...
Authors
Hermann M. Fritz, Jose C. Borrero, Costas E. Synolakis, Emile A. Okal, Robert Weiss, Vasily V. Titov, Bruce E. Jaffe, Spyros Foteinis, Patrick J. Lynett, I-Chi Chan, Philip L-F. Liu