Metadata Report for BODC Series Reference Number 1364484
Metadata Summary
Problem Reports
Data Access Policy
Narrative Documents
Project Information
Data Activity or Cruise Information
Fixed Station Information
BODC Quality Flags
SeaDataNet Quality Flags
Metadata Summary
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Problem Reports
No Problem Report Found in the Database
Data Access Policy
Open Data
These data have no specific confidentiality restrictions for users. However, users must acknowledge data sources as it is not ethical to publish data without proper attribution. Any publication or other output resulting from usage of the data should include an acknowledgment.
If the Information Provider does not provide a specific attribution statement, or if you are using Information from several Information Providers and multiple attributions are not practical in your product or application, you may consider using the following:
"Contains public sector information licensed under the Open Government Licence v1.0."
Narrative Documents
FlowQuest 150 kHz Acoustic Doppler Current Profiler
FlowQuest 150 is a long-range Acoustic Current Profiler manufactured by LinkQuest Inc.
Specifications
Water Profiling Range and Depth | |
---|---|
Frequency | 150 kHz |
Maximum Range | 500 m |
Maximum Cell size | 16 m |
Standard Depth | 800 m |
Optional Depth | 1500, 3000 or 6000 m |
Maximum Transmit | 400 watts |
Blank Distance | 2.8 m |
Velocity Specifications | |
Accuracy | ± 1% ± 5 mm/s |
Cell size | 2-16 m |
Maximum Water Velocity | 20 knots |
Number of cells | 170 |
Maximum Ping Rate | 2/second |
Hardware | |
Transducer | 4 Beam Convex |
Transducer Beam Angle | 22 degrees |
Housing | Anodized Aluminum |
Communication | RS422 or RS232 |
Internal Compact Flash Card | 1 Gbytes (standard) 2 or 4 Gbytes (optional) |
Weight and Dimension | |
Frequency | 150 kHz |
Transducer Assembly Diameter | 40 cm |
Housing Diameter | 20 cm |
Overall Length | 25 cm |
Weight in Air | 22.7 kg |
Weight in Water | 13.6 kg |
Standard Sensors | |
Temperature | |
Accuracy | ± 0.4°C |
Accuracy (optional) | ± 0.1°C |
Range | -5° to 45°C |
Tilt | |
Accuracy | ± 0.5° |
Range | -15° to 15° |
Compass | |
Accuracy | ± 2° |
Maximum Tilt | ± 15° |
For more information about this model see the manufactures FlowQuest manual.
JC088 moored ADCPs (Sites SD, SE, SF and SG): Originator's data processing
Sampling Strategy
RRS James Cook cruise JC088 was the second of two cruises funded by the NERC 'Fluxes Across the Sloping Topography of the North East Atlantic (FASTNEt)' Consortium. JC088 was a 26 day cruise sailing on 28 June 2013 from King George V Dock, Govan to the Malin Shelf edge where inline/single point and bed frame moorings were deployed before returning to Southampton on 24 July 2013.
Setup Configuration
Site | Ping Interval | Ensemble | Pings per Ensemble | Bin Size |
---|---|---|---|---|
SE bed frame | 1.2 sec | 1.2 sec | 1 | 2 m |
SE inline/single point | 1.2 sec | 1.2 sec | 1 | 2 m |
SF2 | 1 sec | 60 sec | 60 | 2 m |
SG | 1 sec | 60 sec | 60 | 2 m |
SD | 2 sec | 180 sec | 67 | 4 m |
Data Processing
The Originator has supplied quality controlled data for moorings SD, SE, SF, SG in Matlab structure format from three different types of instruments.
Binary data from the RDI Workhorse sentinel instruments were exported into Matlab files using the WinADCP software (v1.14) and then converted into Matlab data structures. Binary data from the Flowquest instruments were converted to ascii using the Flowquest software and then converted into Matlab data structures.
Quality Control
SE bed frame
The following quality control has been applied by the Originator to the raw velocity data. Data were removed if the associated error velocity was > 0.15 m/s and if any of the beams were flagged as bad.
SE inline/single point
The following quality control has been applied by the Originator to the raw velocity data. Data were removed if the associated error velocity was > 0.15 m/s and if any of the beams were flagged as bad. The Originator removed data in bin 120 meters above the Sea Bed as this was contaminated.
SF2
The following quality control has been applied by the Originator. A correction for magnetic declination = -5.533° (magnetic north to the west of true north) has been applied. Velocity data contaminated by strong sea surface echos has been removed and the bin nearest the transducer due to high signal to noise ratios and suspect velocities has also been removed. The total water depth was created from the nearest SEACAT SBE 16plus (SN 4848).
SG
The Originator applied the following quality control to data at this site. A correction for magnetic declination = -5.4° (magnetic north to the west of true north) has been applied. Velocity data contaminated by strong sea surface echos have been removed and the bin nearest the transducer due to high signal to noise ratios and suspect velocities has also been removed. The total water depth was created from the nearest SEACAT SBE 16plus (SN 5309).
SD
The ADCP suffered a serious time drift over its deployment. This was estimated to be 8 seconds drift per 3 minute ensemble. This equated to the clock being approximately 20 hours behind once recovered. The Originator has therefore linearly stretched the time as best as possible to remove this error and supplied the corrected data in another Matlab structured file. The corrected file did not include all the parameters in the original file. The parameters not included were percentage good and temperature. These parameters are not being ingested by BODC, but are available (in the uncorrected drift files) upon request.
The Originator has applied a correction for magnetic declination = -5.75° (magnetic north to the west of true north). Poor quality velocity data was removed around 60 meters above the Sea bed. The total water depth was created from pressure data from the nearest MicroCAT (SN 9113).
Merged SE ADCP data
The Originator merged the bed frame and inline/single point 300 kHz ADCP data to provide the best possible full water column profile. Data were averaged onto coincident 1 min grids and then merged at 70 metres.
Lagged cross correlations reveal that the velocities recorded by the bed frame ADCP lag those from the in-line/single point instrument (a consequence of the frame and inline/single point mooring being 680 m apart). This lag was calculated by considering the whole time series and was applied before the data sets were merged. The Originator has applied a correction for magnetic declination = -5.63° (magnetic north to the west of true north). The total water depth was created from pressure data from the nearest SEACAT SBE 16plus (SN 4597).
The merged file for SE inline/single point and SE bed frame is not being ingested by BODC but is available on request.
The Originator states in all sites that further quality control has been left to the discretion of the end user.
Field Calibrations
No field calibrations were undertaken.
JC088 moored ADCPs (Sites SD, SE, SF and SG): Processing by BODC
Data from five ADCPs arrived at BODC in Matlab structured files. Data from two ADCPs were from short term inline/single point moorings (SE and SD) and three ADCPSs were fixed to bed frames (SE, SF2 and SG). The following table shows how the variables within the files were mapped to appropriate BODC parameter codes:
Originator's Variable | Units | Description | BODC Parameter Code | Units | Comment |
---|---|---|---|---|---|
Eastward velocity | m/s | Eastward current velocity (Eulerian) in the water body by moored acoustic doppler current profiler (ADCP) | LCEWAP01 | cm/s | Conversion from originators units to BODC units are applied during transfer. This channel applies to all sites. |
Northward velocity | m/s | Northward current velocity (Eulerian) in the water body by moored acoustic doppler current profiler (ADCP) | LCNSAP01 | cm/s | Conversion from originators units to BODC units are applied during transfer. This channel applies to all sites. |
Vertical velocity | m/s | Upward current velocity in the water body by moored acoustic doppler current profiler (ADCP) | LRZAAP01 | cm/s | Conversion from originators units to BODC units are applied during transfer. This channel applies to all sites. |
Error velocity | m/s | Current velocity error in the water body by moored acoustic doppler current profiler (ADCP) | LERRAP01 | cm/s | Conversion from originators units to BODC units are applied during transfer. This channel applies to sites SE inline and SE bedframe. |
Along beam echo intensity | dB | Signal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) (beam 1-4) | ASAMAP00, ASAMAP02, ASAMAP03, ASAMAP04 | dB | This channel applies to sites SE inline and SE bedframe. |
Along beam echo signal strength | dBm | Signal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) (beam 1-4) | ASAMAP00, ASAMAP02, ASAMAP03, ASAMAP04 | dB | This channel applies to sites SF2, SG and SD. |
Percentage of good data along each bin during ensemble | % | Acceptable proportion of signal returns by moored acoustic doppler current profiler (ADCP) beam 1, beam 2, beam 3 and beam 4 | PCGDAP01, PCGDAP02, PCGDAP03, PCGDAP04 | % | This channel applies to sites SE inline and SE bedframe. |
Percentage of good data along each bin during ensemble | % | Acceptable proportion of signal returns by moored acoustic doppler current profiler (ADCP) beam 1 | PCGDAP00 | % | This channel applies to sites SF2 and SG. |
Ensemble average pitch | Degrees | Orientation (pitch) of measurement platform by triaxial fluxgate compass | PTCHFG01 | Degrees | This channel applies to sites SE inline and SE bedframe. |
Ensemble average pitch | Degrees | Orientation (pitch) of measurement platform by unspecified GPS system | PTCHGP01 | Degrees | This channel applies to sites SF2, SG and SD. |
Ensemble average roll | Degrees | Orientation (roll angle) of measurement platform by unspecified GPS system | ROLLGP01 | Degrees | This channel applies to sites SF2, SG and SD. |
Ensemble average roll | Degrees | Orientation (roll angle) of measurement platform by triaxial fluxgate compass | ROLLFG01 | Degrees | This channel applies to sites SE inline and SE bedframe. |
Ensemble average heading | Degrees | Orientation (horizontal relative to magnetic north) of measurement platform {heading} by compass | HEADCMMG | Degrees | This channel applies to all sites. |
Ensemble average temperature | °C | Temperature of the water body | TEMPPR01 | °C | This channel applies to sites SF2 and SG. |
The reformatted data were visualised using BODC's in-house visualisation software. Suspect data were marked by adding an appropriate quality control flag, missing data by both setting the data to an appropriate absent data value and setting the quality control flag.
Project Information
Fluxes Across Sloping Topography of the North East Atlantic (FASTNEt)
Background
The FASTNEt consortium was funded to deliver NERC's Ocean Shelf Edge Exchange Programme. Commencing in October 2011, this four year study aims to couple established observational techniques, such as moorings and CTDs, with the very latest in autonomous sampling initiatives - including use of Autosub Long Range and gliders. With the aid of novel model techniques, these observations will be utilised to construct a new paradigm of Ocean/Shelf exchange.
Shelf edge regions mark the gateway between the world's deep oceans and shallower coastal seas, linking terrestrial, atmospheric and oceanic carbon pools and influencing biogeochemical fluxes. Shelf edge processes can influence near-shore productivity (and fisheries) and ultimately affect global climate.
FASTNEt brings together researchers from multiple UK organisations. Further collaboration has been established with five Project Partners: the UK Met Office, Marine Scotland Science, Agri-Food and Biosciences Institute, Marine Institute Ireland and Scripps Institution of Oceanography.
Scientific Objectives
- To determine the seasonality of physical gradients and exchange across the shelf edge by deploying new observational technologies (gliders, Autosub Long Range) and established techniques (long term moorings, drifters)
- To quantify key exchange mechanisms and to collect new data targeted at testing and improving high resolution models of the shelf edge, by carrying out detailed process studies in contrasting regions of the shelf edge of the NE Atlantic margin
- To develop a new parameterisation of shelf edge exchange processes suitable for regional-scale models, using improved resolution numerical, and new empirical models constrained by the observations
- To test the new parameterisations in a regional model in the context of making an assessment of inter-annual variability of ocean-shelf exchange.
Fieldwork
Three survey sites on the UK shelf edge have been selected for FASTNEt. These are a) the Celtic Sea shelf edge, b) Malin shelf and c) North Scotland shelf. Fieldwork is centred around two research cruises. The first, to the Celtic Sea, on RRS Discovery in June 2012. The second cruise visits the Malin shelf on RRS James Cook, during summer 2013. In addition to these dedicated cruises, opportunist cruise activity to the North Scotland shelf has been agreed with project partner Marine Scotland Science. Autonomous technologies will complement observations made during the cruises and provide knowledge of seasonal and inter-annual variability in exchange processes.
Instrumentation
Types of instruments/measurements:
- Gliders
- Autosub Long Range
- Drifter buoys
- Scanfish
- Microstructure profilers
- Moored CTD/CT loggers and ADCPs
- Shipboard measurements: CTD, underway, nutrients (and other discrete sampling), LADCP, ADCP.
Contacts
Collaborator | Organisation |
---|---|
Prof. Mark Inall (lead) | Scottish Association for Marine Science, U.K |
Dr. Jason Holt | National Oceanography Centre, U.K |
Dr. Peter Miller | Plymouth Marine Laboratory, U.K |
Dr. Mattias Green | Bangor University, U.K |
Prof. Jonathan Sharples | University of Liverpool, U.K |
Dr. Vasyl Vlasenko | University of Plymouth, U.K |
Data Activity or Cruise Information
Data Activity
Start Date (yyyy-mm-dd) | 2013-07-03 |
End Date (yyyy-mm-dd) | 2013-07-19 |
Organization Undertaking Activity | Scottish Association for Marine Science |
Country of Organization | United Kingdom |
Originator's Data Activity Identifier | JC088_SF2_(bed-frame) |
Platform Category | subsurface mooring |
FASTNEt bed frame mooring SF2
The short term mooring SF2 bed frame was deployed and recovered during cruise RRS James Cook JC088 as part of the Fluxes Across the Sloping Topography of the North East Atlantic (FASTNEt) project.
Instruments deployed on the mooring
Depth (m) | Instrument type | Serial number |
---|---|---|
128 | SBE16 + (Pumped conductivity and digiquartz pressure) | 4848 |
128 | Sontek ADVs | B285 |
128 | Nortek Aquadopps (2MHz Coherent Doppler) | P24977-2 |
128 | 150 kHz Flowquest ADCP | 11043 |
124 | Acoustic Release 1 | 72863 |
- | Acoustic Release 2 | 70356 |
Related Data Activity activities are detailed in Appendix 1
Cruise
Cruise Name | JC088 |
Departure Date | 2013-06-28 |
Arrival Date | 2013-07-24 |
Principal Scientist(s) | Mark E Inall (Scottish Association for Marine Science) |
Ship | RRS James Cook |
Complete Cruise Metadata Report is available here
Fixed Station Information
No Fixed Station Information held for the Series
BODC Quality Control Flags
The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:
Flag | Description |
---|---|
Blank | Unqualified |
< | Below detection limit |
> | In excess of quoted value |
A | Taxonomic flag for affinis (aff.) |
B | Beginning of CTD Down/Up Cast |
C | Taxonomic flag for confer (cf.) |
D | Thermometric depth |
E | End of CTD Down/Up Cast |
G | Non-taxonomic biological characteristic uncertainty |
H | Extrapolated value |
I | Taxonomic flag for single species (sp.) |
K | Improbable value - unknown quality control source |
L | Improbable value - originator's quality control |
M | Improbable value - BODC quality control |
N | Null value |
O | Improbable value - user quality control |
P | Trace/calm |
Q | Indeterminate |
R | Replacement value |
S | Estimated value |
T | Interpolated value |
U | Uncalibrated |
W | Control value |
X | Excessive difference |
SeaDataNet Quality Control Flags
The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:
Flag | Description |
---|---|
0 | no quality control |
1 | good value |
2 | probably good value |
3 | probably bad value |
4 | bad value |
5 | changed value |
6 | value below detection |
7 | value in excess |
8 | interpolated value |
9 | missing value |
A | value phenomenon uncertain |
B | nominal value |
Q | value below limit of quantification |
Appendix 1: JC088_SF2_(bed-frame)
Related series for this Data Activity are presented in the table below. Further information can be found by following the appropriate links.
If you are interested in these series, please be aware we offer a multiple file download service. Should your credentials be insufficient for automatic download, the service also offers a referral to our Enquiries Officer who may be able to negotiate access.
Series Identifier | Data Category | Start date/time | Start position | Cruise |
---|---|---|---|---|
1364459 | Currents -subsurface Eulerian | 2013-07-03 16:25:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364460 | Currents -subsurface Eulerian | 2013-07-04 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364472 | Currents -subsurface Eulerian | 2013-07-05 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364496 | Currents -subsurface Eulerian | 2013-07-07 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364503 | Currents -subsurface Eulerian | 2013-07-08 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364515 | Currents -subsurface Eulerian | 2013-07-09 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364527 | Currents -subsurface Eulerian | 2013-07-10 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364539 | Currents -subsurface Eulerian | 2013-07-11 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364540 | Currents -subsurface Eulerian | 2013-07-12 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364552 | Currents -subsurface Eulerian | 2013-07-13 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364564 | Currents -subsurface Eulerian | 2013-07-14 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364576 | Currents -subsurface Eulerian | 2013-07-15 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364588 | Currents -subsurface Eulerian | 2013-07-16 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364607 | Currents -subsurface Eulerian | 2013-07-17 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364619 | Currents -subsurface Eulerian | 2013-07-18 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |
1364620 | Currents -subsurface Eulerian | 2013-07-19 00:00:57 | 55.84105 N, 8.85087 W | RRS James Cook JC088 |