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Metadata Report for BODC Series Reference Number 1204467


Metadata Summary

Data Description

Data Category Currents -subsurface Eulerian
Instrument Type
NameCategories
Teledyne RDI Ocean Surveyor 75kHz vessel-mounted ADCP  current profilers
Ashtech ADU5 Global Positioning System receiver  Differential Global Positioning System receivers
Instrument Mounting research vessel
Originating Country United Kingdom
Originator Mr Sam Jones
Originating Organization Scottish Association for Marine Science
Processing Status banked
Online delivery of data Download not available
Project(s) FASTNEt
 

Data Identifiers

Originator's Identifier D376_OS7500X_000000_11_ABS
BODC Series Reference 1204467
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2012-06-17 05:52
End Time (yyyy-mm-dd hh:mm) 2012-06-22 13:50
Nominal Cycle Interval 120.0 seconds
 

Spatial Co-ordinates

Start Latitude 48.01660 N ( 48° 1.0' N )
End Latitude 48.31457 N ( 48° 18.9' N )
Start Longitude 9.77973 W ( 9° 46.8' W )
End Longitude 9.52871 W ( 9° 31.7' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 21.27 m
Maximum Sensor or Sampling Depth 813.29 m
Minimum Sensor or Sampling Height -
Maximum Sensor or Sampling Height -
Sea Floor Depth -
Sea Floor Depth Source -
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 -
 

Parameters

BODC CODERankUnitsTitle
BINNUMBR0DimensionlessBin number
AADYAA011DaysDate (time from 00:00 01/01/1760 to 00:00 UT on day)
AAFDZZ011DaysTime (time between 00:00 UT and timestamp)
ACYCAA011DimensionlessSequence number
ALATGP011DegreesLatitude north relative to WGS84 by unspecified GPS system
ALONGP011DegreesLongitude east relative to WGS84 by unspecified GPS system
APDAGP011Degrees TrueDirection of motion of measurement platform relative to ground surface {course made good} by unspecified GPS system
APEWGP011Centimetres per secondEastward velocity of measurement platform relative to ground surface by unspecified GPS system
APNSGP011Centimetres per secondNorthward velocity of measurement platform relative to ground surface by unspecified GPS system
ASAMAS012DecibelsSignal return amplitude from the water body by shipborne acoustic doppler current profiler (ADCP)
DBINAA012MetresDepth (spatial coordinate) of ADCP bin relative to water surface {bin depth} in the water body
LCEWAS012Centimetres per secondEastward velocity of water current (Eulerian measurement) in the water body by shipborne acoustic doppler current profiler (ADCP)
LCNSAS012Centimetres per secondNorthward velocity of water current (Eulerian measurement) in the water body by shipborne acoustic doppler current profiler (ADCP)
LERRAS012Centimetres per secondError velocity of water current in the water body by shipborne acoustic doppler current profiler (ADCP)
LREWAS012Centimetres per secondEastward velocity of water current relative to moving platform in the water body by shipborne acoustic doppler current profiler (ADCP)
LRNSAS012Centimetres per secondNorthward velocity of water current relative to moving platform in the water body by shipborne acoustic doppler current profiler (ADCP)
LRZAAS012Centimetres per secondUpward velocity of water current in the water body by shipborne acoustic doppler current profiler (ADCP)
PCGDAP012PercentAcceptable proportion of acoustic signal returns {percent good} from the water body by acoustic doppler current profiler (ADCP)

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- Ocean Surveyor 75kHz Vessel mounted ADCP.

Long-Range Mode
Vertical Resolution Cell Size3 Max. Range (m)1 Precision (cm/s)2
8m 520 - 650 30
16m 560 - 700 17
High-Precision Mode
Vertical Resolution Cell Size3 Max. Range (m)1 Precision (cm/s)2
8m 310 - 430 12
16m 350 - 450 9

1 Ranges at 1 to 5 knots ship speed are typical and vary with situation.
2 Single-ping standard deviation.
3 User's choice of depth cell size is not limited to the typical values specified.

Profile Parameters

  • Velocity long-term accuracy (typical): ±1.0%, ±0.5cm/s
  • Velocity range: -5 to 9m/s
  • # of depth cells: 1 - 128
  • Max ping rate: 0.7

Bottom Track

Maximum altitude (precision <2cm/s): 950m

Echo Intensity Profile

Dynamic range: 80dB
Precision: ±1.5dB

Transducer and Hardware

Beam angle: 30°
Configuration: 4-beam phased array
Communications: RS-232 or RS-422 hex-ASCII or binary output at 1200 - 115,200 baud
Output power: 1000W

Standard Sensors

Temperature (mounted on transducer)

  • Range: -5° to 45°C
  • Precision: ±0.1°C
  • Resolution: 0.03°

Environmental

Operating temperature: -5° to 40°C (-5° to 45°C)*
Storage temperature: -30° to 50°C (-30° to 60°C)*

*later instruments have greater range.

Web Page

Further details can be found on the manufacturer's website or in the specification sheet

Ashtech Global Positioning System receivers (ADU series)

The ADU series of Global Positioning System (GPS) receivers are designed to give real-time three-dimensional position and attitude measurements. Attitude determination is based on differential carrier phase measurements between four antennas connected to a receiver, providing heading, pitch and roll, along with three-dimensional position and velocity.

The ADU2 model receives information from 48 channels, while the upgraded model (ADU5) uses 56 channels. The ADU5 also features a unique Kalman filter with user selectable dynamic modes to match operating conditions. It also incorporates signals from Satellite Based Augmentation Systems (SBAS) and features an embedded 2-channel 300 kHz beacon receiver for easy differential GPS (DGPS) operations.

Specifications

Parameter ADU2 ADU5

Operational Temperature range:
Antenna
Receiver


-40°C to 65°C
-20°C to 55°C


-40°C to 65°C
-20°C to 55°C

Sampling frequency 5 Hz 5 Hz
Receiver channels 48 56

Accuracy:
Heading
Pitch/Roll


0.2° rms (dynamic) - 0.4° rms (static)
0.4° rms (dynamic) - 0.8° rms (static)


0.02° to 0.2° rms
0.04° to 0.4° rms

Circular Error Probability:
Autonomous
Differential


5.0 m
1.0 m


3.0 m
0.4 to 1.0 m

Further details can be found in the manufacturer's specification sheets for the ADU2 andADU5.

D376 75 kHz and 150 kHz VMADCP Originator Processing

The following information is an adapted summary of the D376 cruise report on the vessel-mounted ADCP (VMADCP).

Configuration and acquisition

RRS Discovery was fitted with a RD Instruments 75kHz (OS75) and 150 kHz (OS150) Ocean Surveyor ADCP at a depth of 5.3m. Positional and attitude information were provided via an Ashtech ADU5 multi-receiver GPS attitude sensor. The RDI proprietary software VMDAS was used to configure the ADCP and perform velocity mapping to the reference frame of the vessel. Bottom tracking was enabled where possible. A suite of MATLAB routines were used to perform data screening and transformation to absolute velocities in Earth coordinates. A summary of the configuration and processing steps is given below.

OS75 VMADCP Configuration:

  • No. of bins = 100
  • Bin size = 8 m
  • Blank after transmit = 8 m
  • Transducer depth = 5.3 m
  • Bottom track (when on) maximum depth 1100 m
  • Time between pings = as fast as possible (typically 5s)
  • Low-resolution long-range processing mode

OS150 VMADCP Configuration:

  • No. of bins = 96
  • Bin size = 4 m
  • Blank after transmit = 4 m
  • Transducer depth = 5.3 m
  • Bottom track (when on) maximum depth 500 m
  • Time between pings = as fast as possible (typically 5s)
  • Low-resolution long-range processing mode

Summary of Matlab processing steps

The RDI binary file with extension ENX (single-ping ADCP ship referenced data from VMDAS) and extension N2R (ascii NMEA output from ADU5 saved by VMDAS) were read into the MATLAB environment. Ensembles with no ADCP data were removed and ensembles with bad or missing ADU5 GPS heading data were identified and the substituted for the ship's GYRO heading.

The attitude information was time-merged with single ping data and the heading data was used to rotate single ping ADCP velocities from the vessel centreline reference to the True North reference. The transducer misalignment error was corrected for (derived from the misalignment determination - see 'Calibration' below).

The ship's velocity was derived from ADU5 positional information.

Further data screening was performed:

  • Max heading change between pings (10 degrees per ping) excluded
  • Max ship velocity change between pings (>2ms-1 pingrate-1) excluded
  • Error velocity greater than double the standard deviation of error velocities of the single ping profile excluded
  • All data averaged into 120-second super-ensembles (user selectable - note that the cruise report states 600-second super-ensembles but the data are at 120 second spacing)
  • Absolute water velocities were determined from either bottom track derived ship velocity or ADU5 GPS derived ship velocity, dependent on depth

Calibration

D376 operated both on and off the continental shelf so bottom tracking was possible on some program runs. Alignment and amplitude corrections were calculated for and applied to subsets of the data. They were as follows:

OS75 VMADCP Calibration:

  • Files 2-6:
    • Misalignment = -3.2881o
    • Amplitude = 0.996432
  • Files 7-11:
    • Misalignment = -3.2512o
    • Amplitude = 0.995536
  • Files 12-16:
    • Misalignment = -3.3509o
    • Amplitude = 0.996260

OS150 VMADCP Calibration:

  • Files 2-6:
    • Misalignment = 0.7324o
    • Amplitude = 1.006998
  • Files 7-11:
    • Misalignment = 0.6319o
    • Amplitude = 1.007483
  • Files 12-16:
    • Misalignment = 0.6601o
    • Amplitude = 1.007250

D376 75 kHz and 150 kHz VMADCP Processing by BODC

The data to be banked by BODC were received as 6 MATLAB files as follows:

For the 75 KHz VMADCP:

  • D376_OS7500x_000000_6_abs.mat; series 2 to 6; 18:47 on 11/06/2012 to 05:52 on 17/06/2012 (Departure from Swansea to start of the Scanfish line to Jones Bank).
  • D376_OS7500x_000000_11_abs.mat; series 7 to 11; 05:52 on 17/06/2012 to 13:53 on 22/06/2013 (Start of the Scanfish line to end of the VMP survey).
  • D376_OS7500x_000000_16_abs.mat; series 12 to 16; 13:53 on 22/06/2013 to 09:47 on 01/07/2012 (End of the VMP survey to the end of science work).

For the 150 KHz VMADCP:

  • D376_OS15000x_000000_6_abs.mat; series 2 to 6; 18:47 on 11/06/2012 to 05:52 on 17/06/2012 (Departure from Swansea to start of the Scanfish line to Jones Bank).
  • D376_OS15000x_000000_11_abs.mat; series 7 to 11; 05:52 on 17/06/2012 to 13:53 on 22/06/2013 (Start of the Scanfish line to end of the VMP survey).
  • D376_OS15000x_000000_16_abs.mat; series 12 to 16; 13:53 on 22/06/2013 to 09:47 on 01/07/2012 (End of the VMP survey to the end of science work).

The file number corresponds to the highest series number contained therein. Whilst the *_abs.mat files should be sufficient for most purposes, BODC has archived all of the originators source and intermediate files which are available upon request.

Parameter Code Mapping

The received files were reformatted to BODC's internal file format which is a NetCDF subset. Due to the large size of both files *16_abs.mat, it was split into two separate files with the split occurring at midnight on the 26th/27th June.

Note: Despite the files being labelled *OS75* and *OS150*, the variables in both sets of files were named OS75*.

The following table shows how the variables within the *.mat files were mapped to appropriate BODC parameter codes:

Originator's Identifier Originator's Units Description BODC Parameter BODC Units Comments
OS75_abs.nav.txy2(1,:) Day of the year Day of the year and day fraction AADYAA01 Days -
AAFDZZ01 Days Time elapsed between 00:00 UT on the corresponding date
OS75_abs.nav.txy2(2,:) o Longitude east ALONGP01 o -
OS75_abs.nav.txy2( 3,:) o Latitude north ALATGP01 o -
OS75_ave_ping.ship_velocity(1,:) m s-1 Eastward velocity of the ship APEWGP01 cm s-1 -
OS75_ave_ping.ship_velocity(2,:) m s-1 Northward velocity of the ship APNSGP01 cm s-1 -
OS75_ave_ping.heading o Ship's heading APDAGP01 o -
N/A N/A Monotonically increasing bin number, with 1 being closest to the ADCP BINNUMBER dimensionless Auto-generated by transfer
OS75_abs.depth m Depth below sea surface (ADCP bin) DBINAA01 m -
OS75_abs.vel(:,1,:) m s-1 Eastward current velocity (Eulerian) in the water column by VMADCP LCEWAS01 cm s-1 -
OS75_abs.vel(:,2,:) m s-1 Northward current velocity (Eulerian) in the water column by VMADCP LCNSAS01 cm s-1 -
OS75_ave_ping.vel(:,1,:) m s-1 Eastward current velocity (relative to moving platform) in the water body by VMADCP LREWAS01 cm s-1 -
OS75_ ave_ping.vel(:,2,:) m s-1 Northward current velocity (relative to moving platform) in the water body by VMADCP LRNSAS01 cm s-1 -
OS75_ ave_ping.vel(:,3,:) m s-1 Upward current velocity in the water body by VMADCP LRZAAS01 cm s-1 -
OS75_ ave_ping.err_vel m s-1 Current velocity error in the water body by VMADCP LERRAS01 cm s-1 -
OS75_ ave_ping.amp dB Signal return amplitude from the water body by VMADCP ASAMAS01 dB -
OS75_ ave_ping.pg % Acceptable proportion of signal returns by VMADCP PCGDAP01 % -

The following variables were not included in the transferred data:

OS75_abs.nav.txy1 ship's position from the first fix after the previous ADCP ping
OS75_abs.ref reference velocity layer, not required
OS75_ave_ping.nav.txy1 ship's position from the first fix after the previous ADCP ping
OS75_ave_ping.nav same as OS75_abs.nav
OS75_ave_ping.att ship's attitude data, not required
OS75_ave_ping.ref reference velocity layer, not required
OS75_ave_ping.bt bottom track data, not required
OS75_ave_ping.depth 2D bin depths, not required
bindepth duplication of OS75_abs.depth

Screening

No quality control flags were provided by the originator. The reformatted data were visualised using the in-house EDSERPLO software. Improbable data values were flagged 'M'. Between 1830 and 2330 hours on 23rd June 2012 a period of high water velocity (see LCEWAS01, LCNSAS01) across all bins in the 75 kHz data the were noted by the originators as being erroneous, and these have been flagged as improbable. Some water body velocity channels in the 75 kHz and 150 kHz data (see LCEWAS01, LCNSAS01, LRZAAS01) have a small number of individual bins that exceed the parameter limits and were flagged as improbable, however it may be possible that these may be valid observations which result from intense tidally driven flows over the shelf-break.

In all the files some data cycles were entirely blank including the time and position channels, and these have been deleted. In addition to intermittent absent data cycles, there was a longer period between 04:54:27 on 12/06/2012 and 14:48:25 on 13/06/2012 when data was absent. No other data were edited or deleted.

The cruise report notes that rough weather caused the frequent presence of air bubbles under the hull and across the transducer face resulting in water profiles that were often poor (less than 50% good at depths as shallow as 180 m).

Banking

Once quality control screening was complete, the data were archived in the BODC National Oceanographic Database and the associated metadata were loaded into an ORACLE Relational Database Management System.


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

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