Search the data

Metadata Report for BODC Series Reference Number 1728868


Metadata Summary

Data Description

Data Category Currents -subsurface Eulerian
Instrument Type
NameCategories
Teledyne RDI Workhorse Sentinel-300 ADCP  current profilers
Instrument Mounting subsurface mooring
Originating Country United Kingdom
Originator Dr Phil Hosegood
Originating Organization University of Plymouth School of Marine Science and Engineering
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) FASTNEt
 

Data Identifiers

Originator's Identifier SC2_ADCP300_10072013_6358
BODC Series Reference 1728868
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2013-07-10 00:00
End Time (yyyy-mm-dd hh:mm) 2013-07-10 23:59
Nominal Cycle Interval 15.0 seconds
 

Spatial Co-ordinates

Latitude 55.90383 N ( 55° 54.2' N )
Longitude 9.28223 W ( 9° 16.9' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 278.48 m
Maximum Sensor or Sampling Depth 366.48 m
Minimum Sensor or Sampling Height 29.51 m
Maximum Sensor or Sampling Height 117.51 m
Sea Floor Depth 396.0 m
Sea Floor Depth Source CRREP
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
ASAMAP012DecibelsSignal return amplitude from the water body by moored acoustic doppler current profiler (ADCP)
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)

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

JC088 short-term (in-line) moored ADCP (sites LA, LB, SB, SC1 and SC2): Data Quality Report

The ADCP data have been through quality control screening and some flagging of data have been made. Due to the inherently noisy nature of ADCP data, only obvious spikes were looked at in closer detail and flagged if necessary.


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 300kHz Workhorse Sentinel Acoustic Doppler Current Profiler

Specifications

Water velocity measurements relative to the ADCP
Maximum velocity 10 m.s-1
Standard deviation 130, 45, 25, 12, 5 mm.s-1 for depth cell sizes of 1, 2, 4, 8, 16 m, respectively
Minimum time between pings 0.07 s
Maximum profiling range* 110, 120, 130, 150, 165 m for depth cell sizes of 1, 2, 4, 8, 16 m, respectively
Minimum range to start of first depth cell 3 m
Number of depth cells 1 - 128 cells
Depth cell size 1 - 16 cm
Echo Intensity measurements
Uncertainty ± 1.5 dB
Sampling Uses same depth cells and time intervals as velocity
Sensors
Water level resolution 0.25 m
Water level accuracy ± 5 m over 0-200 m depth
Temperature range -5°C to + 45°C
Temperature uncertainty ± 0.4°C
Tilt range ± 20°
Tilt uncertainty ± 2°
Compass uncertainty ± 5° at 60° magnetic dip angle
Compass maximum tilt 20°
Physical and Environmental
Maximum depth 200 m
Operating temperature -5°C to 60°C
Storage Temperature -5°C to 80°C

The manufacturer's specification document can be found here

JC088 moored ADCPs (Sites LA short and long term, LB, SB, SC1 and SC2): 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.

Data Processing

The Originator has supplied short term inline/single point ADCP mooring data for short term sites LA, LB, SB, SC1 and SC2 and long term site LA in Matlab structured format from two types of ADCP instruments.

Binary data from the ADCP RDI Workhorse instruments were exported into Matlab files using the WinADCP software (v1.14) and then converted into Matlab data structures.

The Matlab files were topped/tailed to only include data when the instrument was settled at its nominal depth.

No quality control have been applied to the files.

Field Calibrations

No field calibrations were undertaken.

References

Inall.M.E. et al. , (2013). RRS James Cook JC088, Glasgow to Southampton. FASTNEt Cruise to the Malin Shelf Edge. 28 th June to 24 th July 2013. A FASTNEt Cruise led by The Scottish Association for Marine Science.

JC088 moored ADCPs (Sites LA short and long term, LB, SB, SC1 and SC2): Processing by BODC

Data from 11 ADCP's arrived at BODC in Matlab structured files. Included were data from five short term inline/single point moorings and one long term mooring. 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
U - 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.
V - 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.
W - 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.
E - 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.
echo - Echo Amplitude arbitrary units Signal return amplitude from the water body by moored acoustic doppler current profiler (ADCP) ASAMAP01 dB -
Pressure dB Pressure (measured variable) exerted by the water body by fixed in-situ pressure sensor and corrected to read zero at sea level PRESPS01 dB Only applies to short term sites LA 75 kHz S/N 17194 and 14788, LB 75 kHz S/N 12893 and SB 300 kHz S/N 2666.
Bin depth m Depth below sea surface (ADCP bin) DBINAA01 m -

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) 2013-07-18
Organization Undertaking ActivityScottish Association for Marine Science
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierJC088_SC2
Platform Categorysubsurface mooring

FASTNEt short term inline/single point mooring SC2

The short term mooring SC2 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

Instrument codes

ADCP - RDI ADCP (U, V, W, Temperature and Pressure)

NIOZ_t - Thermistor on NIOZ chain (Temperature)

A/R - Acoustic Release

Nominal depth (m) Instrument type Instrument serial number Comments
252.5 subsurface float - -
274.5 ADCP 300KHz 6358 -
275.5 NIOZ_t 251 -
276.5 NIOZ_t 252 -
277.5 NIOZ_t 253 -
278.5 NIOZ_t 254 -
279.5 NIOZ_t 255 -
280.5 NIOZ_t 256 -
281.5 NIOZ_t 257 -
282.5 NIOZ_t 258 -
283.5 NIOZ_t 259 -
284.5 NIOZ_t 260 -
285.5 NIOZ_t 261 -
286.5 NIOZ_t 262 -
287.5 NIOZ_t 263 -
288.5 NIOZ_t 264 -
289.5 NIOZ_t 265 -
290.5 NIOZ_t 266 -
291.5 NIOZ_t 267 -
292.5 NIOZ_t 268 -
293.5 NIOZ_t 269 -
294.5 NIOZ_t 270 -
295.5 NIOZ_t 271 -
296.5 NIOZ_t 272 -
297.5 NIOZ_t 273 -
298.5 NIOZ_t 274 -
299.5 NIOZ_t 275 -
300.5 NIOZ_t 276 -
301.5 NIOZ_t 277 -
302.5 NIOZ_t 278 -
303.5 NIOZ_t 279 -
304.5 NIOZ_t 281 -
305.5 NIOZ_t 282 -
306.5 NIOZ_t 283 -
307.5 NIOZ_t 284 -
308.5 NIOZ_t 285 -
309.5 NIOZ_t 286 -
310.5 NIOZ_t 287 -
311.5 NIOZ_t 288 -
312.5 NIOZ_t 289 -
313.5 NIOZ_t 290 -
314.5 NIOZ_t 291 -
315.5 NIOZ_t 292 -
316.5 NIOZ_t 293 -
317.5 NIOZ_t 294 -
318.5 NIOZ_t 295 -
319.5 NIOZ_t 297 -
320.5 NIOZ_t 298 -
321.5 NIOZ_t 299 -
322.5 NIOZ_t 300 lost
323.5 NIOZ_t 301 dragged up the line by 0.5m
324.5 NIOZ_t 302 -
325.5 NIOZ_t 303 -
326.5 NIOZ_t 304 may be sensor 48 dragged up instead
327.5 NIOZ_t 305 -
328.5 NIOZ_t 306 lost
329.5 NIOZ_t 307 lost
330.5 NIOZ_t 308 lost
331.5 NIOZ_t 309 lost
332.5 NIOZ_t 310 lost
333.5 NIOZ_t 311 lost
334.5 NIOZ_t 312 lost
335.5 NIOZ_t 313 lost
336.5 NIOZ_t 314 lost
337.5 NIOZ_t 316 lost
338.5 NIOZ_t 317 lost
339.5 NIOZ_t 318 lost
340.5 NIOZ_t 319 lost
341.5 NIOZ_t 320 lost
342.5 NIOZ_t 321 lost
343.5 NIOZ_t 322 lost
344.5 NIOZ_t 323 dragged to position 28 in a clump
345.5 NIOZ_t 324 dragged to position 28 in a clump
346.5 NIOZ_t 325 dragged to position 28 in a clump
347.5 NIOZ_t 326 dragged to position 28 in a clump
348.5 NIOZ_t 327 dragged to position 28 in a clump
349.5 NIOZ_t 328 lost
350.5 NIOZ_t 329 -
351.5 NIOZ_t 331 -
352.5 NIOZ_t 332 -
353.5 NIOZ_t 333 -
354.5 NIOZ_t 334 -
355.5 NIOZ_t 335 -
356.5 NIOZ_t 336 -
357.5 NIOZ_t 337 -
358.5 NIOZ_t 338 lost
359.5 NIOZ_t 340 -
360.5 NIOZ_t 341 lost
361.5 NIOZ_t 342 -
362.5 NIOZ_t 343 lost
363.5 NIOZ_t 344 put back in position but displaced on recovery
364.5 NIOZ_t 345 -
365.5 NIOZ_t 346 -
366.5 NIOZ_t 347 -
367.5 NIOZ_t 348 -
368.5 NIOZ_t 349 -
369.5 NIOZ_t 350 lost
370.5 NIOZ_t 351 lost
371.5 NIOZ_t 352 lost
372.5 NIOZ_t 353 lost
373.5 NIOZ_t 354 -
374.5 NIOZ_t 355 lost
375.5 NIOZ_t 356 -
376.5 NIOZ_t 357 -
377.5 A/R 073 -
389.5 anchor - -

The depths are based on the original positions of the thermistors on the line, as it is believed the entanglement of the line and subsequent shift of some sensors occurred at recovery.

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_SC2

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
1728788Currents -subsurface Eulerian2013-07-03 11:37:0855.90383 N, 9.28223 WRRS James Cook JC088
1728807Currents -subsurface Eulerian2013-07-04 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728819Currents -subsurface Eulerian2013-07-05 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728820Currents -subsurface Eulerian2013-07-06 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728832Currents -subsurface Eulerian2013-07-07 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728844Currents -subsurface Eulerian2013-07-08 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728856Currents -subsurface Eulerian2013-07-09 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728881Currents -subsurface Eulerian2013-07-11 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728893Currents -subsurface Eulerian2013-07-12 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728900Currents -subsurface Eulerian2013-07-13 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728912Currents -subsurface Eulerian2013-07-14 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728924Currents -subsurface Eulerian2013-07-15 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728936Currents -subsurface Eulerian2013-07-16 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728948Currents -subsurface Eulerian2013-07-17 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088
1728961Currents -subsurface Eulerian2013-07-18 00:00:0855.90383 N, 9.28223 WRRS James Cook JC088