Metadata Report for BODC Series Reference Number 1809811
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
RRS Discovery D376 navigation quality control report
Quality control report
Bathymetry
As part of the Matlab processing, the originator has removed spikes.
Navigation
No data quality issues concerning navigation were found. (BODC assessment)
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
Kongsberg Simrad EA500 bathymetric echosounder
The EA500 is a bathymetric echosounder that can be used in water as deep as 10,000 m. It features triple frequency operation with a separate digitiser for each channel and high transmitted power with an instantaneous dynamic range of 160 dB. The instrument can operate with several pulses in the water simultaneously and has bottom tracking capabilities. A wide range of transducers (single beam, split beam or side-looking) is available and the ping rate is adjustable up to 10 pings per second. The split beam operation measures the athwartships inclination angle of the seabed.
This instrument was introduced in June 1989 and and replaced by the EA 600 in 2000.
Specifications
Operational range | 1, 5, 10, 15, 25, 50, 100, 150, 250, 500, 750, 1000, 2500, 5000 and 10000 m |
Phasing | 0 to 10000 m in 1 m increments (manual or automatic) |
Non saturated instantaneous input range | -160 to 0 dB |
Output power regulation | 0 to 20 dB relative to full power |
Noise figure | 10 dB |
Operating temperature | 0 to 55°C |
Ping rate | max 10 pings per second (adjustable) |
Further details can be found in the manufacturer's specification sheet.
Fugro SeaSTAR 9200-G2 Receiver
The SeaSTAR 9200-G2 is a dual frequency (L1/L2) receiver that incorporates global positioning system (GPS) and global navigation satellite system (GLONASS) reception capability while tracking the Fugro L-Band satellite broadcast of Differential Global Satellite Navigation System (DGSNS) corrections. These corrections can also be received via internet, as a backup.
The SeaSTAR 9200-G2 can be used in conjunction with other services as HP (GPS network solution), XP (GPS or orbit and clock solution) and G2 (Composite GPS/GLONASS orbit and clock solution). These are also dual frequency carrier phase solutions, which allows for a decimeter level accuracy.
The 72 channels received by the SeaSTAR include GPS- L1 C/A code and L1/L2/L2C full cycle carrier, GLONASS- L1/L2 full cycle carrier, Satellite Based Augmentation System (SBAS) and the Fugro L-Band service.
Specifications
Position Accuracy | Horizontal | Vertical |
HP | 10 cm (95%) | 15 cm (95%) |
XP | 15 cm (95%) | 20 cm (95%) |
G2 | 15 cm (95%) | 20 cm (95%) |
Further details can be found in the manufacturer's specification sheet.
RRS Discovery D376 navigation instrumentation
Instrumentation
The following scientific navigational and bathymetric systems were fitted.
Please note that no information on the type of Gyrocompass used on cruise D376 was supplied to BODC and therefore BODC have assumed that the instrumentation was the same as used on D379.
Instrument | Type | Main role | Comments |
GPS | Fugro SeaSTAR 9200-G2 | Navigation | ship's primary position instrument in the RVS Level-C |
Gyrocompass | Sperry Marine | Heading | - |
Kongsberg Maritime | EA500 | Single-beam echo sounder (hull) | Corrected for local sound velocities. |
RRS Discovery D376 navigation data processing procedures
Originator's Data Processing
The data were logged by the TECHSAS (TECHnical and Scientific sensors Acquisition System) system into daily NetCDF files. The TECHSAS system is used as the main data logging system on NMF-SS operated research vessels. Data were additionally logged into the RVS Level-C format files.
Each Level-C file was read into Matlab so that further processing, calibration and quality control could be performed on selected variables.
GPS data were logged from the Trimble 4000 differential GPS, the Ashtech GPS and Seastar 9200. Ship's gyrocompass readings and echosounder depth were also logged. Data from all instruments were logged to the RVS Level-C system. Standard navigation processing steps were then carried out using the relmov, bestnav and prodep programs.
Any headings in either AshHeading or Heading > 360 or <0 were removed. Heading readings from the gyrocompass between 23/06/2012 18:37:09 and 24/06/2012 00:10:33 were noisey and were also removed. Subsequent comparison of the headings recorded by the ships gyro and the AshTech GPS revealed a median offset of -0.622 degrees (gyro > AshTech).
Corrected depths were obtained from the processing routine prodep. The programme corrects the raw depths recorded by the hull mounted, single beam echo sounder (Simrad EA500) for local variations in sound velocity using values from the Carter tables published by the Hydrographic Office. These tables divide the world's oceans into areas of similar water masses and provide depth corrections for each area. The program uses a navigation file to find the position of each depth record and applies the relevant correction.
The Matlab navigation and bathymetry files provided to BODC were used for BODC processing. Data were additionally logged into the RVS Level-C format files and TECHSAS which have been archived at BODC.
For more detailed information on the Originator's underway data processing, please see the cruise report
Files delivered to BODC
Filename | Content description | Format | Interval | Start date/time (UTC) | End date/time (UTC) | Comments |
D376_NAV1_1sec.mat | Position (latitude and longitude) (from Seastar 9200 G2) and True heading (from Gyrocompass) | Matlab | 1 second | 11/06/2012 14:35:40 | 30/06/2012 23:00:00 | - |
D376_NAV2_1sec.mat | Depths from EA500 single-beam echosounder | Matlab | 1 second | 11/06/2012 14:35:40 | 30/06/2012 23:00:00 |
BODC Data Processing
Underway data files were merged into a single file using time as the primary linking key. Data were banked using BODC standard banking procedures. Data resolution were reduced to 60 second intervals.
The originator's variables were mapped to appropriate BODC parameter codes as follows:
D376_NAV1_1sec.mat
Originator's variable | Originator's units | Description | BODC Code | BODC Units | Unit conversion | Comments |
date | dd/mm/yyyy hh24miss | Measure timestamp | Not transferred | |||
daynum | Decimal Julian day number | Measure timestamp | Not transferred | |||
dd | Matlab serial date number | Measure timestamp | Not transferred | |||
Latitude | degree_north | Latitude north | ALATGP01 | degree_north | - | |
Longitude | degree_east | Longitude east | ALONGP01 | decimal degrees | none | |
SMG | knots | Speed over the ground (speed made good) | m/s | *0.51444 | Not transferred. | |
CMG | degrees | Course over the ground (course made good) | degrees | Not transferred. Used gyro heading. | ||
distrun | Distance travelled | DSRNCV01 | km | BODC derived. | ||
heading | degrees | True heading | HEADCM01 | degrees | ||
AshHeading | degrees | GPS heading | Not transferred. Used gyro heading. | |||
Eastward velocity (over ground) of measurement platform by unspecified GPS system | APEWGP01 | cm/s | Channel derived after transfer using BODC Matlab routine 'velcal' | |||
Northward velocity (over ground) of measurement platform by unspecified GPS system | APNSGP01 | cm/s | Channel derived after transfer using BODC Matlab routine 'velcal' | |||
Distance traveled | DSRNCV01 | meters | Channel derived using Matlab routine from navigation channels |
D376_NAV2_1sec.mat
Originator's variable | Originator's units | Description | BODC Code | BODC Units | Unit conversion | Comments |
daynum | Decimal Julian day number | Measure timestamp | Not transferred | |||
dd | Matlab serial date number | Measure timestamp | Not transferred | |||
Latitude | degree_north | Latitude north | Not transferred | |||
Longitude | degree_east | Longitude east | Not transferred | |||
CorDepth | meters | Depth in meters | MBANZZ01 | meters | none | EA500 single-beam |
Screening
All the reformatted data were visualised using the in-house EDSERPLO software. Suspect data were marked by adding an appropriate quality control flag.
Position
A check was run on positional data to identify gaps and improbable values (through the calculation of speed). There were gaps in the positional data and these gaps were present due to a crash in the TECHSAS system. During BODC processing, these gaps were linearly interpolated to remove them.
Ship Velocities
Ship velocities were calculated from the main latitude and longitude channels using standard BODC procedures creating channels - APEWGP01 and APNSGP01.
Distance Run
Distance run was calculated from the main latitude and longitude channels, starting from the beginning of the file, using BODC standard procedures creating channel - DSRNCV01.
Bathymetry
The EA500 echo-sounder has been corrected for local sound velocities. Bathymetry data were screened independently as well as against GEBCO bathymetry measurements.
Calibration
No field calibrations have been applied to the data at BODC.
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 |