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Items below are listed from most recently updated to least recently updated.
These are results 1 through 25 of 135 matches.
| General Information Research Vessel Parke Snavely |
| Research Project USGS Coral Reef Studies |
| General Information Staff Information for Western CMG |
| Publication General Information Product 57: South San Francisco Bay, California |
| Educational Materials Tsunami and Earthquake Research at the USGS |
| Publication General Information Product 87: Sea Floor off San Diego, California |
| Publication Open-File Report 2009-1100: High-Resolution Seismic-Reflection and Marine Magnetic Data Along the Hosgri Fault Zone, Central California |
Description: The topography of the Continental Shelf in the central portion of the Southern California Bight has rapid variations over relatively small spatial scales. The width of the shelf off the Palos Verdes peninsula, just northwest of Los Angeles, California, is only 1 to 3 km. About 7 km southeast of the peninsula, the shelf within San Pedro Bay widens to about 20 km. In 2000, the Los Angeles County Sanitation District began deploying a dense array of moorings in this complex region of the central Southern California Bight to monitor local circulation patterns. Moorings were deployed at 13 sites on the Palos Verdes shelf and within the northwestern portion of San Pedro Bay. At each site, a mooring supported a string of thermistors and an adjacent bottom platform housed an Acoustic Doppler Current Profiler. These instruments collected vertical profiles of current and temperature data continuously for one to two years. The variable bathymetry in the region causes rapid changes in the amplitudes and spatial structures of barotropic tidal currents, internal tidal currents, and in the associated nonlinear baroclinic currents that occur at approximate tidal frequencies. The largest barotropic tidal constituent is M2, the principal semidiurnal tide. The amplitude of this tidal current changes over fairly short along-shelf length scales. Tidal-current amplitudes are largest in the transition region between the two shelves; they increase from about 5 cm/s over the northern San Pedro shelf to nearly 10 cm/s on the southern portion of the Palos Verdes Shelf. Tidal-current amplitudes are then reduced to less than 2 cm/s over the very narrow section of the northern Palos Verdes shelf that lies just 6 km upcoast of the southern sites. Models suggest that the amplitude of the barotropic M2 tidal currents, which propagate toward the northwest primarily as a Kelvin wave, is adjusting to the short topographic length scales in the region. Semidiurnal sea-level oscillations are, as expected, independent of these topographic variations; they have a uniform amplitude and phase structure over the entire region. Because the cross-shelf angle of the seabed over most of the Palos Verdes shelf is 1 to 3 degrees, which is critical for the local generation and/or enhancement of nonlinear characteristics in semidiurnal internal tides, some internal tidal-current events have strong asymmetric current oscillations that are enhanced near the seabed. Near-bottom currents in these events are directed primarily offshore with amplitudes that exceed 30 cm/s. The spatial patterns in these energetic near-bottom currents have fairly short-length scales. They are largest over the inner shelf and in the transition region between the Palos Verdes and San Pedro shelves. This spatial pattern is similar to that found in the barotropic tidal currents. Because these baroclinic currents have an approximate tidal frequency, an asymmetric vertical structure, and a somewhat stable phase, they can produce a non-zero depth-mean flow for periods of a few months. These baroclinic currents can interact with the barotropic tidal current and cause an apparent increase (or decrease) in the estimated barotropic tidal-current amplitude. The apparent amplitude of the barotropic tidal current may change by 30 to 80 percent or more in a current record that is less than three months long. The currents and surficial sediments in this region are in dynamic equilibrium in that the spatial patterns in bottom stresses generated by near-bed currents from surface tides, internal tides, and internal bores partly control the spatial patterns in the local sediments. Coarser sediments are found in the regions with enhanced bottom stresses (that is, over the inner shelf and in the region between the Palos Verdes and San Pedro shelves). Finer sediments are found over the northwestern portion of the Palos Verdes shelf, where near-bottom currents are relatively weak. The nonlinear asymmetries in the internal tidal-period current oscillations cause a net transport of suspended material along and off the shelf, reinforcing the mean flow patterns that also carry sediment either into Santa Monica Bay or offshore and onto the adjacent slope.
| Publication Open-File Report 2009-1073: The Framework of a Coastal Hazards Model—A Tool for Predicting the Impact of Severe Storms |
| Map National Seafloor Mapping and Characterization |
| Research Project Potential San Francisco Bay Landslides During El Nino |
| Research Project Coastal Change Hazards: Hurricanes and Extreme Storms |
| Publication Open-File Report 2009-1029: Coastal processes study of Santa Barbara and Ventura Counties, California |
| Publication Open-File Report 98-139: Multibeam Data and Socio-Economic Issues in West-Central San Francisco Bay |
| Research Project WCMG Coastal Processes Studies |
| Research Project Southern California Coastal Hazards - USGS WCMG |
| Publication Open-File Report 2007-1112, Updated: The National Assessment of Shoreline Change: A GIS Compilation of Vector Cliff Edges and Associated Cliff Erosion Data for the California Coast |
| Research Project Coastal Processes: San Francisco Bight Coastal Processes Study - USGS WCMG |
| Research Project Santa Barbara-Ventura Coastal Processes Study - USGS WCMG |
| Publication Open-File Report 2008-1246: High-Resolution Chirp and Mini-Sparker Seismic-Reflection Data From the Southern California Continental Shelf—Gaviota to Mugu Canyon |
| Publication Open-File Report 2007-1437: The Uniform California Earthquake Rupture Forecast, Version 2 (UCERF 2) |
| General Information Contact Information for Western Coastal and Marine Geology |
| Publication Scientific Investigations Map 3007: Views of the Sea Floor in Northern Monterey Bay, California |
| Research Project Open-File Report 2007-1271: Seafloor Mapping and Benthic Habitat GIS for Southern California, Volume III - USGS WCMG |
| Publication Scientific Investigations Report 2007-5254: Sources, Dispersal, and Fate of Fine Sediment Supplied to Coastal California |
| These are results 1 through 25 of 135 matches. |