Eastward and northward components of ocean current and water temperature collected from moorings in the vicinity of Quinault Canyon in the North East Pacific Coast from 1979-04-28 to 1979-08-28 (NCEI Accession 0163893)
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title: Eastward and northward components of ocean current and water temperature collected from moorings in the vicinity of Quinault Canyon in the North East Pacific Coast from 1979-04-28 to 1979-08-28 (NCEI Accession 0163893)
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Anchor: https://www.ncei.noaa.gov/archive/archive-management-system/OAS/bin/prd/jquery/person/details/216 Hickey, Barbara M.
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abstract: The University of Washington deployed 9 current meter moorings in the vicinity of Quinault Canyon. Of those 9 moorings, 6 moorings were recovered with useful data: QC1, QC2, QC5, QC7, QC8, and QC10. QC3 was not deployed and QC4 and QC6 were not recovered. One instrument from QC9 was found on the beach at Brandon, OR, July 12 but it leaked and no data was recovered. Current meters used were primarily Aanderaa (AA) meters and 2 Vector Measuring Current Meters (VMCM) instruments. Unfiltered data from the VMCM instruments is not available and therefore not included in this set. The AA data was sampled in 20 minute intervals. Speed and direction were measured and rotated to true North. Data was first edited for spurious values, then speed and direction were independently filtered with a 5 point binomial filter spanning approximately 1.5 hours and resolved into u and v components. Results from this project can be found in: Hickey, B.M. (1989) Patterns and processes of shelf and slope circulation. In: Landry, M.R. and B.M. Hickey (eds.), Coastal Oceanography of Washington and Oregon, pp. 41-115, Elsevier Science, Amsterdam, The Netherlands. Data file format is plain text.
purpose: The purpose of this study was to provide information about the circulation in and around canyons and discover to what extent canyons affect the regional shelf circulation. This is important because Astoria and Quinault Canyon, located on the Washington coast, provide the primary conduits by which land derived sediments and pollutants reach the deep ocean. Canyons also enhance upwelling.
credit: The Quinault Canyon 1979 project was sponsored by the United States Department of Energy Contract DE-AT06-76-EV-71025 to Dr. B. Hickey at the University of Washington.
credit: Related Funding Agency: United States Department of Energy
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beginPosition: 1979-04-28
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description: Data Type: u and v components of velocity (calculated); Units: cm/sec; Observation Type: in situ; Sampling Instrument: Aanderaa current meters (AA); Sampling and Analyzing Method: AA current meters measured current directions and magnitudes. Directions were rotated into degrees true north. Data was sampled in 20 minute intervals, then edited for spurious values. Speed and direction were independently filtered with a 5 point binomial filter spanning approximately 1.5 hours then resolved into u and v components.; Data Quality Information: Data were plotted and visually inspected for spurious values.
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