Search the data

Metadata Report for BODC Series Reference Number 1206695


Metadata Summary

Data Description

Data Category Currents -subsurface Eulerian
Instrument Type
NameCategories
Teledyne RDI Narrowband 150kHz ADCP  current profilers
Instrument Mounting subsurface mooring
Originating Country United Kingdom
Originator Dr Jo Hopkins
Originating Organization National Oceanography Centre, Liverpool
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) FASTNEt
 

Data Identifiers

Originator's Identifier D376_ST5_ADCP_24062012
BODC Series Reference 1206695
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2012-06-24 00:00
End Time (yyyy-mm-dd hh:mm) 2012-06-24 23:59
Nominal Cycle Interval 120.0 seconds
 

Spatial Co-ordinates

Latitude 48.76896 N ( 48° 46.1' N )
Longitude 9.40630 W ( 9° 24.4' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 24.02 m
Maximum Sensor or Sampling Depth 161.52 m
Minimum Sensor or Sampling Height 7.84 m
Maximum Sensor or Sampling Height 145.34 m
Sea Floor Depth 169.36 m
Sea Floor Depth Source DATAHEAD
Sensor or Sampling Distribution Sensor fixed with measurements made at multiple depths within a fixed range (e.g. ADCP) - The sensor is at a fixed depth, but measurements are made remotely from the sensor over a range of depths (e.g. ADCP measurements)
Sensor or Sampling Depth Datum Instantaneous - Depth measured below water line or instantaneous water body surface
Sea Floor Depth Datum Instantaneous - Depth measured below water line or instantaneous water body surface
 

Parameters

BODC CODERankUnitsTitle
DBINAA010MetresDepth (spatial coordinate) of ADCP bin relative to water surface {bin depth} in the water body
AADYAA011DaysDate (time from 00:00 01/01/1760 to 00:00 UT on day)
AAFDZZ011DaysTime (time between 00:00 UT and timestamp)
ACYCAA011DimensionlessSequence number
HEADCMMG1DegreesOrientation (horizontal relative to magnetic north) of measurement platform {heading} by compass
PTCHGP011DegreesOrientation (pitch) of measurement device by unspecified GPS system
ROLLGP011DegreesOrientation (roll angle) of measurement device by unspecified GPS system
ASAMAP002DecibelsSignal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) beam 1
ASAMAP022DecibelsSignal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) beam 2
ASAMAP032DecibelsSignal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) beam 3
ASAMAP042DecibelsSignal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) beam 4
LCEWAP012Centimetres per secondEastward velocity of water current (Eulerian measurement) in the water body by moored acoustic doppler current profiler (ADCP)
LCNSAP012Centimetres per secondNorthward velocity of water current (Eulerian measurement) in the water body by moored acoustic doppler current profiler (ADCP)
LERRAP012Centimetres per secondError velocity of water current in the water body by moored acoustic doppler current profiler (ADCP)
LRZAAP012Centimetres per secondUpward velocity of water current in the water body by moored acoustic doppler current profiler (ADCP)
PCGDAP002PercentAcceptable proportion of acoustic signal returns {percent good} from the water body by moored acoustic doppler current profiler (ADCP) beam 1
PCGDAP022PercentAcceptable proportion of acoustic signal returns {percent good} from the water body by moored acoustic doppler current profiler (ADCP) beam 2
PCGDAP032PercentAcceptable proportion of acoustic signal returns {percent good} from the water body by moored acoustic doppler current profiler (ADCP) beam 3
PCGDAP042PercentAcceptable proportion of acoustic signal returns {percent good} from the water body by moored acoustic doppler current profiler (ADCP) beam 4

Definition of Rank

  • Rank 1 is a one-dimensional parameter
  • Rank 2 is a two-dimensional parameter
  • Rank 0 is a one-dimensional parameter describing the second dimension of a two-dimensional parameter (e.g. bin depths for moored ADCP data)

Problem Reports

No Problem Report Found in the Database


Data Access Policy

Open Data supplied by Natural Environment Research Council (NERC)

You must always use the following attribution statement to acknowledge the source of the information: "Contains data supplied by Natural Environment Research Council."


Narrative Documents

RD Instruments 150kHz Narrow Band Acoustic Doppler Current Profiler

Specifications

Water velocity measurements relative to the ADCP
Accuracy (long term) 0.5 % of measured velocity ± 0.5 cm/s
Statistical uncertainty for one ping (cm/s) Depth cell length of 4, 8, 16 m = 26, 13, 6.5 respectively (for horizontal velocities using the standard transducer)
Ping rate (pings per second) 2 (100 pings averaged in ADCP)
Maximum profiling range (meters) 290
Minimum range to start of first depth cell (meters) 4
Number of depth cells 8 to 128
Velocity range ± 0.01 to 9.5 m/s (horizontal)
Velocity resolution (cm/s) 0.25 or 0.125
Velocity measurements relative to the bottom and measurement of bottom depth
Accuracy 0.5% of measured velocity ± 0.5 cm/s
Statistical uncertainty of one ping (percent of measured velocity) 3.5 (for horizontal velocities using the standard transducer)
Ping rate (pings per second) 0.9 (100 pings averaged in ADCP)
Depth range 290 (the maximum depth range can be up to 1.5 times greater than specified)
Bottom depth resolution (meters) 4
Velocity range ± 0.01 to 9.5 m/s (horizontal)
Velocity resolution (cm/s) 0.25 or 0.125
Measurement of echo intensity
Accuracy (with temperature correction) Before calibration : ± 8 dB, After calibration: ± 3 dB
Statistical uncertainty for one ping Approximately ± 5 dB
Ping rate (pings per second) 2 (100 pings averaged in ADCP)
Profiling range (meters less than for water velocity measurement) 64
Number of depth cells 8 to 128
Dynamic range 80 dB
Resolution 0.45 dB typical (temperature/system dependent)
Data communication
Interface Modified RS-232/422 serial at baud rates of 300-19,200
Data format Binary (8-bit) or ASCII (76-character) lines separated by a carriage return/line feed.
Data storage capacity 2 MB (standard); expandable to 40 MB in 1 and/or 2 MB increments
Power requirements
ADCP electronics Voltage range (VDC) 6-12; Standby current (amps) 0.0002; Operate current (amps) 0.24; Peak current (amps) 0.5
transmit and EPROM recorder Voltage range (VDC) 20-40; Standby current (amps) 0.0001; Operate current (amps) 0.10; Peak current (amps) 2.0
CTD sensors Voltage range (VDC) 12-20; Standby current (amps) 0.0001; Operate current (amps) 0.022; Peak current (amps) 0.05
Temperature sensor
Accuracy ± 0.2°C
Time constant Approximately 2 minutes
Range -5° to 45°C
Resolution 0.012°C
Environmental
Operating temperature -5°C to 40°C
Humidity Must be non-condensing
Depth capability 35 meters (transducer only)
Physical characteristics
Weight in air 67.6 kg
Weight in water 25.0
Diameter 45.9 cm
Length 141.4 cm

RRS Discovery short term mooring instrument description

Sampling Strategy

Short term mooring ADCP data were collected on cruise RRS Discovery D376 using the instrumentation detailed below.

Instrument Serial #
75kHz RDI ADCP 9201
300kHz RDI ADCP 14449
600kHz RDI ADCP 7301
150kHz RDI ADCP 1149
150kHz Flowquest ADCP 11043
150kHz Flowquest ADCP 11625

No manufacturer's calibration information is available.

The ADCP's configuration has been setup in the following ways.

Site Ping interval (sec) Ensemble (sec) Pings per ensemble Bin size (m) Number of bins
ST1 6 60 10 8 80
ST2LW 1.33 60 45 2 49
ST2UW 1 60 60 2 25
ST3 1 60 60 2 -
ST4 1 60 60 2 -
ST5 4 120 30 2.5 80

No changes to the mooring instrumentation were recorded during these cruises.

D376 moored instrumentation: Originator's data processing

Sampling Strategy

The RRS Discovery D376 was the first of two cruises funded by the NERC Consortium grant for the Fluxes Across the Sloping Topography of the North East Atlantic (FASTNEt) project. D376 was a 19 day cruise sailing on 11 June 2012 from Swansea dry dock to the Celtic Sea shelf edge where a total of six short term ADCPs were deployed before returning to Southampton on 2 July 2012.

Data Processing

The originator has done the following quality control on the data before submitting to BODC.

Data contaminated by the stronger surface echo has been removed from ST3 and ST4 by calculating the maximum range for acceptable current readings based on the following:

Rmax = D cos(θ)

where D = distance from ADCP to surface, θ = ADCP beam angle.

All data above this level has been removed (after additional visual inspection).

At ST5 and ST1 a cut off at 147.8 mab (metres above bottom) and 624.56 mab was applied.

No data was removed from the two ADCPs at ST2 since they stopped profiling a considerable distance from the surface.

No data has been removed from within the water column at any of the sites and quality control here has been left to the discretion of the user.

All the velocity data (est_vel, nrt_vel) has been corrected for magnetic declination. The appropriate declination was calculated using the GeoMag 7.0 software.

All files supplied to BODC have undergone trimming to remove data cycles from before the ADCP was deployed and from after it had been recovered.

ST1

The binary data from the instrument was exported into a MATLAB file using the WinADCP software (v1.14). This data was then converted into a MATLAB structure. The originator has applied a correction for magnetic declination = -4.3667° (magnetic north to the west of true north).

ST2 (ST2UW and ST2LW)

The binary data from the instrument was exported into a MATLAB file using the WinADCP software (v1.14). This data was then converted into a MATLAB structure. The originator has applied a correction for magnetic declination = -4.35° (magnetic north to the west of true north).

ST3

The binary data from the instrument was initially converted to ASCII using the Flowquest software. This data was then converted into a MATLAB structure. The originator has applied a correction for magnetic declination = -4.33° (magnetic north to the west of true north).

ST4

The binary data from the instrument was initially converted to ASCII using the Flowquest software. This data was then converted into a MATLAB structure. The originator has applied a correction for magnetic declination = -4.25° (magnetic north to the west of true north).

ST5

The binary data from the instrument was initially converted to ASCII using the Flowquest software. This data was then converted into a MATLAB structure. The originator has applied a correction for magnetic declination = -4.40° (magnetic north to the west of true north). The originator has stated that there may be potential contamination in the bottom 3 bins caused by the recovery line on the frame. A three beam solution is possible after identification of the contaminated beam using error velocity, echo amplitude, percentage good and correlation.

Field Calibrations

The originator has stated that no field calibrations were undertaken.

Processing by BODC of RRS Discovery short term ADCP data

Data from 6 ADCPs arrived at BODC in MATLAB files. Data from three ADCP's were from short term in-line moorings (ST1, ST2UW and ST2LW) and three ADCP's were fixed to bedframes (ST3, ST4 and ST5). The data have been converted to BODC's internal QXF format.

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. These channels apply to all sites (ST1-ST5).
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. These channels apply to all sites (ST1-ST5).
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. These channels apply to all sites (ST1-ST5).
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. These channels apply to sites ST1, ST2UW, ST2LW and ST5.
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 These channels apply to sites ST1, ST2UW, ST2LW and ST5.
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 These channels apply to sites ST3 and ST4.
Percentage of good transformations (error velocity threshold not exceeded) % Acceptable proportion of signal returns by acoustic doppler current profiler (ADCP) PCGDAP01 % These channels apply to sites ST1, ST2UW and ST2LW.
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 PCGDAP00, PCGDAP02, PCGDAP03, PCGDAP04 % These channels apply to sites ST3, ST4 and ST5.
Ensemble average pitch Degrees Orientation (pitch) of measurement platform by triaxial fluxgate compass PTCHFG01 Degrees These channels apply to sites ST1, ST2UW, ST2LW and ST5.
Ensemble average pitch Degrees Orientation (pitch) of measurement platform by unspecified GPS system PTCHGP01 Degrees These channels apply to sites ST3 and ST4.
Ensemble average roll Degrees Orientation (roll angle) of measurement platform by unspecified GPS system ROLLGP01 Degrees These channels apply to sites ST3 and ST4.
Ensemble average roll Degrees Orientation (roll angle) of measurement platform by triaxial fluxgate compass ROLLFG01 Degrees These channels apply to sites ST1, ST2UW, ST2LW and ST5.
Ensemble average heading Degrees (-180 to 180) Orientation (horizontal relative to magnetic north) of measurement platform {heading} by compass HEADCMMG Degrees (0 to 360) Conversion from Originators units to BODC units are applied during transfer. These channels apply to all sites (ST1-ST5).
Ensemble average temperature °C Temperature of the water body TEMPPR01 °C These channels apply to sites ST1, ST2UW, ST2LW, ST3 and ST4.
Pressure of instrument Decibars Pressure (measured variable) exerted by the water body by fixed in-situ pressure sensor and corrected to read zero at sea level PRESPS01 Decibars These channels apply to sites ST1, ST2UW and ST2LW.

The reformatted data were visualised using the in-house EDSERPLO software. Suspect data were marked by adding an appropriate quality control flag, missing data by both setting the data to an appropriate value and setting the quality control flag.

Due to the inherently noisy nature of ADCP data, only obvious spikes were looked at in closer detail and flagged if necessary.

General Data Screening carried out by BODC

BODC screen both the series header qualifying information and the parameter values in the data cycles themselves.

Header information is inspected for:

  • Irregularities such as unfeasible values
  • Inconsistencies between related information, for example:
    • Times for instrument deployment and for start/end of data series
    • Length of record and the number of data cycles/cycle interval
    • Parameters expected and the parameters actually present in the data cycles
  • Originator's comments on meter/mooring performance and data quality

Documents are written by BODC highlighting irregularities which cannot be resolved.

Data cycles are inspected using time or depth series plots of all parameters. Currents are additionally inspected using vector scatter plots and time series plots of North and East velocity components. These presentations undergo intrinsic and extrinsic screening to detect infeasible values within the data cycles themselves and inconsistencies as seen when comparing characteristics of adjacent data sets displaced with respect to depth, position or time. Values suspected of being of non-oceanographic origin may be tagged with the BODC flag denoting suspect value; the data values will not be altered.

The following types of irregularity, each relying on visual detection in the plot, are amongst those which may be flagged as suspect:

  • Spurious data at the start or end of the record.
  • Obvious spikes occurring in periods free from meteorological disturbance.
  • A sequence of constant values in consecutive data cycles.

If a large percentage of the data is affected by irregularities then a Problem Report will be written rather than flagging the individual suspect values. Problem Reports are also used to highlight irregularities seen in the graphical data presentations.

Inconsistencies between the characteristics of the data set and those of its neighbours are sought and, where necessary, documented. This covers inconsistencies such as the following:

  • Maximum and minimum values of parameters (spikes excluded).
  • The occurrence of meteorological events.

This intrinsic and extrinsic screening of the parameter values seeks to confirm the qualifying information and the source laboratory's comments on the series. In screening and collating information, every care is taken to ensure that errors of BODC making are not introduced.


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) 2012-06-13
End Date (yyyy-mm-dd) 2012-06-29
Organization Undertaking ActivityNational Oceanography Centre, Liverpool
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierST5 Bedframe
Platform Categorysubsurface mooring

FASTNEt bedframe mooring ST5

The short term mooring ST5 was deployed and recovered during cruise RRS Discovery D376 which took place between 11 June 2012 to 2 July 2012 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
170 150kHz RDI ADCP 1149
170 SBE 37 SMP MicroCAT 7769

Related Data Activity activities are detailed in Appendix 1

Cruise

Cruise Name D376
Departure Date 2012-06-11
Arrival Date 2012-07-02
Principal Scientist(s)Mark E Inall (Scottish Association for Marine Science)
Ship RRS Discovery

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: ST5 Bedframe

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 IdentifierData CategoryStart date/timeStart positionCruise
1199236Hydrography time series at depth2012-06-13 13:25:0148.7665 N, 9.40287 WRRS Discovery D376
1206566Currents -subsurface Eulerian2012-06-13 13:37:4448.76896 N, 9.4063 WRRS Discovery D376
1206578Currents -subsurface Eulerian2012-06-14 00:01:0548.76896 N, 9.4063 WRRS Discovery D376
1206591Currents -subsurface Eulerian2012-06-15 00:00:1248.76896 N, 9.4063 WRRS Discovery D376
1206609Currents -subsurface Eulerian2012-06-16 00:01:1948.76896 N, 9.4063 WRRS Discovery D376
1206610Currents -subsurface Eulerian2012-06-17 00:00:2648.76896 N, 9.4063 WRRS Discovery D376
1206622Currents -subsurface Eulerian2012-06-18 00:01:3248.76896 N, 9.4063 WRRS Discovery D376
1206634Currents -subsurface Eulerian2012-06-19 00:00:3948.76896 N, 9.4063 WRRS Discovery D376
1206646Currents -subsurface Eulerian2012-06-20 00:01:4648.76896 N, 9.4063 WRRS Discovery D376
1206658Currents -subsurface Eulerian2012-06-21 00:00:5348.76896 N, 9.4063 WRRS Discovery D376
1206671Currents -subsurface Eulerian2012-06-22 00:02:0048.76896 N, 9.4063 WRRS Discovery D376
1206683Currents -subsurface Eulerian2012-06-23 00:01:0648.76896 N, 9.4063 WRRS Discovery D376
1206702Currents -subsurface Eulerian2012-06-25 00:01:2048.76896 N, 9.4063 WRRS Discovery D376
1206714Currents -subsurface Eulerian2012-06-26 00:00:2748.76896 N, 9.4063 WRRS Discovery D376
1206726Currents -subsurface Eulerian2012-06-27 00:01:3448.76896 N, 9.4063 WRRS Discovery D376
1206738Currents -subsurface Eulerian2012-06-28 00:00:4048.76896 N, 9.4063 WRRS Discovery D376
1206751Currents -subsurface Eulerian2012-06-29 00:01:4748.76896 N, 9.4063 WRRS Discovery D376