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Metadata Report for BODC Series Reference Number 2207611


Metadata Summary

Data Description

Data Category Platform orientation and velocity
Instrument Type
NameCategories
Kongsberg Simrad EA600 echosounder  single-beam echosounders
Kongsberg Simrad EM 120 multibeam echosounder  multi-beam echosounders
Trimble Applanix POSMV global positioning system  Differential Global Positioning System receivers; inertial navigation systems; Kinematic Global Positioning System receivers
Sperry Marine MK37 series gyrocompasses  platform attitude sensors
Instrument Mounting research vessel
Originating Country United Kingdom
Originator Prof Stuart Cunningham
Originating Organization National Oceanography Centre, Southampton
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) RAPID-WATCH
 

Data Identifiers

Originator's Identifier JC064_NAV
BODC Series Reference 2207611
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2011-09-10 12:00
End Time (yyyy-mm-dd hh:mm) 2011-10-06 23:59
Nominal Cycle Interval 30.0 seconds
 

Spatial Co-ordinates

Southernmost Latitude 23.69850 N ( 23° 41.9' N )
Northernmost Latitude 28.48033 N ( 28° 28.8' N )
Westernmost Longitude 52.01683 W ( 52° 1.0' W )
Easternmost Longitude 13.33617 W ( 13° 20.2' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth -
Maximum Sensor or Sampling Depth -
Minimum Sensor or Sampling Height -
Maximum Sensor or Sampling Height -
Sea Floor Depth -
Sea Floor Depth Source -
Sensor or Sampling Distribution -
Sensor or Sampling Depth Datum -
Sea Floor Depth Datum -
 

Parameters

BODC CODERankUnitsTitle
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
APDAZZ011Degrees TrueDirection of motion of measurement platform relative to ground surface {course made good}
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
APSAZZ011Metres per secondSpeed of measurement platform relative to ground surface {speed over ground}
DSRNCV011KilometresDistance travelled
HEADCM011DegreesOrientation (horizontal) of measurement device relative to True North {heading}
MBANGB081MetresBathymetric depth of seafloor relative to Mean Sea Level datum {sea-floor depth} in the water body by derivation from GEBCO_08 30 arc-second global grid

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

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

RRS James Cook Cruise JC064 Underway Document

Cruise details

Dates 10th Sept. 2011 to 9th Oct. 2011
Principal Scientific Officer Dr Stuart Cunningham (NOCS)

JC064 formed the second leg of the cruise, while JC063 was referred to as the first. The JC064 cruise departed on 10 September 2011 from Santa Cruz de Tenerife and arrived again in Santa Cruz de Tenerife on 9 October 2011 where the cruise terminated. The purpose of the cruise was to refurbish a mooring array on the Mid-Atlantic Ridge and at the Easter Boundary of the Atlantic near the Moroccan Coast at a nominal latitude of 26.5°N. The moorings are part of the RAPIDMOC mooring array, monitoring the Atlantic Meridional Overturning Circulation and Heat Flux.

Kongsberg EA600 Single Beam Echosounder

The EA600 is a single beam echosounder with full ocean depth capability designed for bathymetric surveys. It measures water depth by monitoring the travel time of an acoustic signal that is transmitted from the ship, reflected off the seabed and received back at the ship.

The main components of the system are hull-mounted transducers linked to general purpose transceivers (GPTs). Up to four GPTs, each controlling one or more transducers, may be operated simultaneously. The GPT generates a signal, which is transmitted into the water column as an acoustic pulse by the transducer array, and the returning echo is recorded by the GPT. GPTs are in turn linked to a combined display and processor, where adjustments (such as sound-speed corrections) may be applied to the data. Available frequencies span from 12 to 710 kHz, and each GPT may operate at a separate frequency. A variety of transducers is available for water depths up to 11,000 m.

The EA600 stores all data internally but has a USB port which allows the possibility of connecting a CD-ROM/DVD drive to read and write the data. All echo data can be stored as files: bitmap, sample, depth or sidescan data.

In deeper waters, the EA600 supports a multipulse function, allowing for a higher pinger rate. While on passive mode, the pinger is normally attached to a device, with the purpose of tracking and displaying its current depth.

The EA600 replaced the EA500 in 2000.

Specifications

Maximum Ping rate 20 Hz
Resolution 1 cm
Accuracy

1 cm at 710 and 200 kHz
2 cm at 120 kHZ
5 cm at 38 kHz
10 cm at 18 kHz
20 cm at 12kHz

Operating frequencies 1 or 2 kHz
Single Beam frequencies

12, 18, 33, 38, 50, 70,
120, 200, 210 or 710 kHz

Dynamic range 160 dB

Further details can be found in the manufacturer's specification sheet.

Kongsberg EM120 Multibeam Echosounder

The EM120 is a low frequency (12 kHz) multibeam echosounder with full ocean depth capability designed for bathymetric surveys. It measures water depth by monitoring the travel time of an acoustic signal that is transmitted from the ship, reflected off the seabed and received back at the ship.

The main system units of the EM120 are transducer arrays (separate for reception and transmission), preamplifier unit, transceiver unit and operator unit. Sub-bottom profiling capability is an optional extra. For both transmit and receive arrays standard beamwidth is 1° or 2°, and 4° beamwidth is available for the receive array.

The system has 191 beams with pointing angles automatically adjusted according to achievable coverage or operator defined limits. The beam spacing is normally equidistant, corresponding to 1% of depth at 90° angular coverage, 2% at 120° and 3% at 140°. The transmit fan is split into several individual sectors, each of which is corrected independently for vessel roll, pitch and yaw, which places all soundings on a "best fit" to a line perpendicular to the survey line.

The EM120 supersedes the EM12 and was itself superseded by the EM122 in 2008.

Specifications

Frequency 12 kHz
Maximum ping rate 5 Hz
Range sampling rate 2 kHz
Swath coverage sector up to 150°
Swath width up to 5.5 x water depth
Depth resolution 10 to 40 cm
Depth range 20 to 11,000 m
Pulse length 2, 5 and 15 ms
Number of beams 191
Beam width

1° x 1°
1° x 2°
2° x 2°
2° x 4°

Beam spacing (at angular coverage)

1% of depth at 90°
2% of depth at 120°
3% of depth at 140°

Further details can be found in the manufacturer's specification sheet.

Sperry Marine MK-37 Gyrocompass

A family of instruments that contain a controlled gyroscope which seeks and aligns itself with the meridian and points to true north. They use the properties of the gyroscope in combination with the rotation of the earth and the effect of gravity. The effects of varying speed and latitude are compensated for by the use of manually operated controls. Models MOD I, MOD O, MOD D, MOD D/E are all with an analog output Step or/and Syncro. MOD VT is the latest model with NMEA Data output as well.

Further specifications for MOD VT can be found in the manufacturer's specification document.

Further information for MOD D/E can be found in the user manual.

Trimble Applanix Position and Orientation Systems for Marine Vessels (POSMV)

The Position and Orientation Systems for Marine Vessels (POSMV) is a real time kinematic (RTK) and differential global positioning system (DGPS) receiver for marine navigation. It includes an inertial system that provides platform attitude information. The instrument provides accurate location, heading, velocity, attitude, heave, acceleration and angular rate measurements.

There are three models of Applanix POSMV, the POS MV 320, POS MV Elite and the POS MV WaveMaster. POS MV 320 and POS MV WaveMaster are designed for use with multibeam sonar systems, enabling adherence to IHO (International Hydrographic Survey) standards on sonar swath widths of greater than ± 75 degrees under all dynamic conditions. The POS MV Elite offers true heading accuracy without the need for dual GPS installation and has the highest degree of accuracy in motion measurement for marine applications.

Specifications

POS MV 320
Componenet DGPS RTK GPS Outage
Position 0.5 - 2 m 1 0.02 - 0.10 m 1 <2.5 m for 30 seconds outages, <6 m for 60 seconds outages
Roll and Pitch 0.020° 0.010° 0.020°
True Heading 0.020° with 2 m baseline
0.010° with 4 m baseline
- Drift <1° per hour (negligible for outages <60 seconds)
Heave 5 cm or 5% 2 5 cm or 5% 2 5 cm or 5% 2
POS MV WaveMaster
Accuracy DGPS RTK GPS Outage
Position 0.5 - 2 m 1 0.02 - 0.10 m 1 <3 m for 30 seconds outages, <10 m for 60 seconds outages
Roll and Pitch 0.030° 0.020° 0.040°
True Heading 0.030° with 2 m baseline - Drift <2° per hour
Heave 5 cm or 5% 2 5 cm or 5% 2 5 cm or 5% 2
POS MV Elite
Accuracy DGPS RTK GPS Outage
Position 0.5 - 2 m 1 0.02 - 0.10 m 1 <1.5 m for 60 seconds outages DGPS, <0.5 m for 60 seconds outage RTK
Roll and Pitch 0.005° 0.005° 0.005°
True Heading 0.025° 0.025° Drift <0.1° per hour (negligible for outages <60 seconds)
Heave 3.5 cm or 3.5% 2 3.5 cm or 3.5% 2 3.5 cm or 3.5% 2

1 One Sigma, depending on quality of differential corrections
2 Whichever is greater, for periods of 20 seconds or less

Further details can be found in the manufacturer's specification sheet.

RRS James Cook Cruise JC064 Navigation Instrumentation

The following scientific navigational and bathymetric systems were fitted.

Manufacturer Model Function Comments
Applanix POS MV GPS (latitude, longitude, and heading) Primary source of position for science.
Seatex Seapath 200 GPS (latitude, longitude, and attitude) Secondary source of position for science.
Kongsberg Maritime DPS116 GPS (latitude, longitude) -
Ashtech Ashtech GPS System GPS (latitude, longitude, and attitude) -
C & C Technologies CNAV GPS (latitude, longitude) -
Sperry Marine gyrocompass GPS (heading) -
Kongsberg Maritime Simrad EA600 Singlebeam hydrographic echosounder Shut off during communication with moorings.
Kongsberg Maritime EM120 Multibeam sonar Shut off during communication with moorings.

RRS James Cook Cruise JC064 Navigation Data Processing Procedures

Originator's Data Processing

All navigational data were downloaded from the TECHSAS system. The Applanix POSMV was the primary GPS system used for science. Data were removed that were not in the correct chronological order. Data from the Ashtech GPS was used to correct the heading given by the gyro compass. The differences were calculated and then cleaned to produce a correction. This was then applied to the heading from the gyro compass.

BODC Data processing

The underway navigation data for cruise JC064 were supplied to BODC as .mstar files and reformatted to BODC's internal NetCDF format (QXF). Data were averaged at 30 second intervals.

During transfer the originator's variables were mapped to unique BODC parameter codes. The following table shows the parameter mapping:

Original File Originator's Parameter Originator's Units Description BODC Parameter Code BODC Units Comments
met_jc064_true.nc lat ° (+ve N) Latitude ALATGP01 ° (+ve N) -
met_jc064_true.nc long ° (+ve E) Longitude ALONGP01 ° (+ve E) -
met_jc064_true.nc cmg ° true Ship's direction of movement over ground APDAZZ01 ° true -
met_jc064_true.nc ship_u ms -1 Ship's eastward velocity APEWGP01 cm -1 Unit conversion: * 100
met_jc064_true.nc ship_v ms -1 Ship's northward velocity APNSGP01 cm -1 Unit conversion: * 100
met_jc064_true.nc smg ms -1 Ship's speed over ground APSAZZ01 ms -1 -
met_jc064_true.nc distrun km Distance travelled DSRNCV01 km Calculated by BODC
met_jc064_true.nc heading_av ° Ship's heading HEADCM01 ° Orientation of vessel by gyrocompass
- - - Bathymetric depth MBANGB08 m No bathymetry parameter supplied by originator, bathymetric depth generated from GEBCO.

Following transfer, all data were screened using BODC in-house visualisation software. Suspect data values were assigned the appropriate BODC data quality flags. Missing data values, where present, were changed to a BODC data value and assigned a data quality flag.


Project Information

RAPID- Will the Atlantic Thermohaline Circulation Halt? (RAPID-WATCH)

RAPID-WATCH (2007-2014) is a continuation programme of the Natural Environment Research Council's (NERC) Rapid Climate Change (RAPID) programme. It aims to deliver a robust and scientifically credible assessment of the risk to the climate of UK and Europe arising from a rapid change in the Atlantic Meridional Overturning Circulation (MOC). The programme will also assess the need for a long-term observing system that could detect major MOC changes, narrow uncertainty in projections of future change, and possibly be the start of an 'early warning' prediction system.

The effort to design a system to continuously monitor the strength and structure of the North Atlantic MOC is being matched by comparative funding from the US National Science Foundation (NSF) for the existing collaborations started during RAPID for the observational arrays.

Scientific Objectives

  • To deliver a decade-long time series (2004-2014) of calibrated and quality-controlled measurements of the Atlantic MOC from the RAPID-WATCH arrays.
  • To exploit the data from the RAPID-WATCH arrays and elsewhere to determine and interpret recent changes in the Atlantic MOC, assess the risk of rapid climate change, and investigate the potential for predictions of the MOC and its impacts on climate.

This work will be carried out in collaboration with the Hadley Centre in the UK and through international partnerships.

Mooring Arrays

The RAPID-WATCH arrays are the existing 26°N MOC observing system array (RAPIDMOC) and the WAVE array that monitors the Deep Western Boundary Current. The data from these arrays will work towards meeting the first scientific objective.

The RAPIDMOC array consists of moorings focused in three geographical regions (sub-arrays) along 26.5° N: Eastern Boundary, Mid-Atlantic Ridge and Western Boundary. The Western Boundary sub-array has moorings managed by both the UK and US scientists. The other sub-arrays are solely led by the UK scientists. The lead PI is Dr Stuart Cunningham of the National Oceanography Centre, Southampton, UK.

The WAVE array consists of one line of moorings off Halifax, Nova Scotia. The line will be serviced in partnership with the Bedford Institute of Oceanography (BIO), Halifax, Canada. The lead PI is Dr Chris Hughes of the Proudman Oceanographic Laboratory, Liverpool, UK.

All arrays will be serviced (recovered and redeployed) either on an annual or biennial basis using Research Vessels from the UK, US and Canada.

Modelling Projects

The second scientific objective will be addressed through numerical modelling studies designed to answer four questions:

  • How can we exploit data from the RAPID-WATCH arrays to obtain estimates of the MOC and related variables?
  • What do the observations from the RAPID-WATCH arrays and other sources tell us about the nature and causes of recent changes in the Atlantic Ocean?
  • What are the implications of RAPID-WATCH array data and other recent observations for estimates of the risk due to rapid change in the MOC?
  • Could we use RAPID-WATCH and other observations to help predict future changes in the MOC and climate?

Data Activity or Cruise Information

Cruise

Cruise Name JC064
Departure Date 2011-09-10
Arrival Date 2011-10-09
Principal Scientist(s)Stuart A Cunningham (National Oceanography Centre, Southampton)
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