Identifier | 2020-621-FA | ||||||||
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Also known as | CSF20 | ||||||||
Purpose | Determine variability in settling velocity between channel and shoals and investigate its causes | ||||||||
Location | South San Francisco Bay, CA | ||||||||
Summary | Bed sediments were sampled during deployment. Data collection was successful. | ||||||||
Info derived | Wave properties, currents, suspended-sediment concentration, salinity, water level, bed sediment grains size, and suspended sediment size | ||||||||
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Platform |
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Vehicles | MarFac; Dodge Ram truck G43-1698S
MarFac; Ford F350 MT use only; pickup - white; G43-2784H
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Itinerary |
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Marine operations | Yes |
Organization |
2885 Mission Street
Santa Cruz, CA95060
(831) 460-7401
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Principal investigators | Jessica R LacyRachel M Allen | ||||||||||||
Crew members |
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Information specialist(s) |
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Affiliate principal | Daniel Livsey (CAWSC) |
Data category: | Location-Elevation, Time Series |
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Data type: | Navigation, Mooring (physical oceanography) |
Equipment | Usage description | Data types | Datasets |
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GPS | Navigation | (no data reported) | |
instrumentmooring | Mooring (physical oceanography) | 1 |
Dataset name | Equipment | Description | Dataset contact |
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Hydrodynamic timeseries data from south San Francisco Bay, California, summer 2020 | instrumentmooring | Hydrodynamic and sediment transport time-series data, including water depth, velocity, turbidity, suspended particle size, conductivity, and temperature, were collected by the U.S. Geological Survey (USGS) Pacific Coastal and Marine Science Center at two locations in south San Francisco Bay. Data were collected in the channel (one platform) and in the shallows (three co-located platforms) for 2 weeks in July 2020. Data files are grouped by site (channel or shallows). Each site contained instrumentation to collect the data listed, with slight instrument and setup variations between the two sites due to logistics. Users are advised to assess data quality carefully, and to check metadata for instrument information, as platform deployment times and data-processing methods varied. | Rachel M Allen |