Oceanographic water temperature, salinity, and velocity collected from Rogue River Mooring off the coast of Oregon from 2000-09-17 to 2004-09-08 (NCEI Accession 0137120)
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title: Oceanographic water temperature, salinity, and velocity collected from Rogue River Mooring off the coast of Oregon from 2000-09-17 to 2004-09-08 (NCEI Accession 0137120)
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abstract: A single mooring measuring temperature, salinity, and velocity was deployed on the 73 m isobath off the Oregon coast. The mooring was located at 42° 26.49' N, 124° 34.47' W, 11 km off Gold Beach, OR and was in the water from May 2000 to October 2004. The currents were sampled using an upward-looking RD Instruments 300 kHz broadband ADCP instrument burst-sampling 40 1-s pings every 15 minutes in 4-m depth bins. The taut-wire mooring had Seabird SBE-37IM MicroCAT temperature, conductivity, and pressure instruments at 20, 36, and 66 m sampling every 5 minutes and Seabird SBE-39 temperature only sensors at 26, 42, 50, and 58 m also sampling every 5 minutes. The MicroCATs represent the mid-depth and as close to the surface and bottom as possible given the mooring design. The 1.8 m (45) steel top sphere was moored at 17 m to avoid mooring motion induced by the extremely large (>12 m) surface waves which sometimes occur during winter storms off the Oregon coast. At tidal frequencies, typical blow-down at the top MicroCAT was less than 2 m with pitch and roll at the ADCP of less than 6 degrees. The worst-case mooring performance was during the severe winter storms of November and December 2002, when the blow-down was about 7 m and the pitch briefly hit 25 degrees. The mooring was recovered and redeployed every six months for four years. The early data revealed the need to sample closer to the surface than the original mooring design allowed. To facilitate this, a light-weight pennant consisting of a 30 cm plastic float on a thin spectra line was flown off the top of the 1.8 m sphere. A Star-Oddi Starmon mini temperature pod was taped to the line to sample temperature every 5 minutes at 6 m depth. This simple system worked surprisingly well starting with the fall 2001 deployment. Funding was provided by the NOAA Coastal Ocean Program.
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DateTime: 2015-10-28T21:00:08Z
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sourceCitation: (CI_Citation)
title: NCEI Accession 0137120 v1.1
date: (CI_Date)
date: (inapplicable)
dateType: (CI_DateTypeCode) publication
citedResponsibleParty: (CI_ResponsibleParty)
individualName: (inapplicable)
contactInfo: (CI_Contact)
onlineResource: (CI_OnlineResource)
linkage: https://www.ncei.noaa.gov/archive/accession/0137120/1.1
protocol: HTTPS
name: NCEI Accession 0137120 v1.1
description: published 2015-10-28T21:00:08Z
function: (CI_OnLineFunctionCode) download
role: (inapplicable)
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dataQualityInfo: (DQ_DataQuality)
scope: (DQ_Scope)
level: (MD_ScopeCode) dataset
lineage: (LI_Lineage)
processStep: (LE_ProcessStep)
description: Data Type: WATER TEMPERATURE (measured); Units: degrees C; Observation Type: in situ; Sampling Instrument: CTD - moored CTD.
processStep: (LE_ProcessStep)
description: Data Type: water salinity (measured); Units: psu; Observation Type: in situ; Sampling Instrument: CTD - moored CTD.
processStep: (LE_ProcessStep)
description: Data Type: water velocity (measured); Units: cm/s; Observation Type: in situ; Sampling Instrument: ADCP.
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metadataMaintenance: (MD_MaintenanceInformation)
maintenanceAndUpdateFrequency: (MD_MaintenanceFrequencyCode) asNeeded
maintenanceNote: Metadata are developed, maintained and distributed by NCEI. Updates are performed as needed to maintain currentness.
contact: (CI_ResponsibleParty)
organisationName: NOAA National Centers for Environmental Information
role: (CI_RoleCode) custodian
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acquisitionInformation: (MI_AcquisitionInformation)
instrument: (MI_Instrument)
identifier: (MD_Identifier)
code: ADCP
type: ADCP
description: Acoustic Doppler Current Profiler The Acoustic Doppler Current Profiler (ADCP) measures currents beneath a ship while underway. Sound signals sent from the moving ship bounce back to receivers aboard the ship. This provides a profile of water movement relative to the ship-precise modern navigation, allowing the ship's motion to be subtracted from the data. These devices are also used on moorings and profilers and, along with acoustic backscattering, measure animal biomass. Particles in the path of the sound waves, mostly plankton, reflect a small part of the sound energy back toward receivers, allowing researchers to make remote estimates of the sizes and numbers of animals present in the water column. Before the 1970's, the most technologically advanced instrument used to measure water velocity was known as a Doppler speed log. This evolved into the first commercial ADCP, produced in the mid-1970's, which used averaging. Later in the 1970's, the first vessel-mounted ADCP was developed to measure water velocity more accurately and to allow measurement in range cells over a depth profile. As instruments evolved, so did new techniques in Doppler signal processing. Initially, Doppler speed logs used simple analog signal processing methods, which are still used in some commercial speed logs today. However, the first ADCPs incorporated analog-to-digital signal conversion over a narrow communication bandwidth. Around 1990, this technique was developed into broadband signal processing. Since then, broadband ADCPs have been able to generate very accurate, real-time velocity measurements.
instrument: (MI_Instrument)
identifier: (MD_Identifier)
code: CTD
type: CTD
description: Conductivity-Temperature-Depth probe
instrument: (MI_Instrument)
identifier: (MD_Identifier)
code: mooring
type: mooring
description: use as an observation type