Metadata Report for BODC Series Reference Number 1905012
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
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 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 |
Operating frequencies | 1 or 2 kHz |
Single Beam frequencies | 12, 18, 33, 38, 50, 70, |
Dynamic range | 160 dB |
Further details can be found in the manufacturer's specification sheet.
Ashtech G12 Global Positioning System Receiver
The Ashtech G12 Global Positioning System (GPS) uses all-in-view tracking and 12 channels to provide real time three-dimensional positional measurements. It is Differential GPS (DGPS) ready, offering an accuracy of better than 40 cm, position latency better than 50 ms, and exact position latency to millisecond accuracy.
Specifications
Parameter | Values |
---|---|
Operating Temperature | -30°C to 70°C |
Sampling frequency | up to 10 Hz |
Receiver channels | 12 |
Real-Time Position Accuracy | Horizontal, DGPS: 40 cm Horizontal 95%: 90 cm Vertical 95%: 1.6 m |
Further details can be found in the manufacturer's specification sheet.
Ashtech GG24 receiver
The GG24 is an all-in-view Global Positioning System (GPS) and Global Navigation Satellite System (GLONASS) receiver that blends GPS and GLONASS into a single position solution. This receiver uses all available satellites from both systems to obtain the best position information.
The three-dimensional position and velocity are calculated when tracking any combination of five satellites. Up to five independent measurements are determined every second, with no interpolation or extrapolation from previous solutions.
Specifications
Parameter | Values |
Operating Temperature | -30°C to 55°C |
Sampling frequency | up to 5 Hz |
Receiver channels | 12 L1 GPS + 12 L1 GLONASS |
Real-Time Position Accuracy | 3.2 m (autonomous) 35.0 m (differential) |
Velocity Accuracy | 0.1 knots |
Further details can be found in the manufacturer's 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: | | |
Sampling frequency | 5 Hz | 5 Hz |
Receiver channels | 48 | 56 |
Accuracy: | | |
Circular Error Probability: | | |
Further details can be found in the manufacturer's specification sheets for the ADU2 andADU5.
Kongsberg Seatex Seapath 200 GPS and Gyrocompass
The Seapath 200 is a highly accurate, real-time heading, attitude and position information system that integrates the best signal characteristics of Inertial Measurement Units (IMU) and Global Positioning System (GPS), using a differential GPS method to acquire this data.
The high-rate motion data is obtained from the Seatex MRU5 inertial sensor and two fixed baseline GPS carrier-phase receivers. The raw data is integrated in a Kalman filter in the Seapath Processing Unit. The IMU contains an accurate linear accelerometer and Bosch Coriolis force angular rate gyros (CFG).
This system is equipped to utilise up to six different DGPS reference stations, it checks for consistency within measurements from the different sensors to ensure reliability and rejects noisy data or reports its inaccuracy. The data is available through various output protocols, RS-232, RS-422 and Ethernet.
This instrument is no longer in production; the main characteristics are presented below, and the specification sheet can be accessed here Kongsberg Seatex Seapath 200 .
Specifications
Scale factor error in pitch, roll and heading | 0.2% RMS |
Heave motion periods | 1 to 25 s |
Accuracy | |
Heading | 0.05° RMS (4 m baseline) 0.075° RMS (2.5 m baseline) |
Roll and Pitch | 0.03° EMS (± 5° amplitude) |
Heave | 5 cm or 5%, whichever is highest |
Position | 0.7 RMS or 1.5 m (95% CEP) with DGPS 0.15 m EMS or 0.4 m (95% CEP) with Searef 100 corrections |
Velocity | 0.03 m s-1 RMS or 0.07 m s-1 (95% CEP) with DGPS |
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.
DISCOVERY 2010 RRS James Clark Ross Cruise JR20090310 (JR200, JR200A, JR208) Underway Navigation Instrumentation Document
Navigation data were obtained through several different instruments. The following scientific navigational and bathymetry systems were fitted.
Instrument | Type | Manufacturer | Main role |
Ashtec ADU2 | GPS | Ashtec | Antenna 1 used to determine the ships' position, antennae 2-4 used to determine roll, pitch and yaw |
Seapath GPS200 | GPS | Seatex | Position and heading |
EA600 | Echosounder | Simrad | Bathymetry |
Gyrocompass | MK37 | Sperry Marine | Ship's heading |
DISCOVERY 2010 RRS James Clark Ross Cruise JR20090310 (JR200, JR200A, JR208) Underway Navigation Processing Procedures Document
Originator's Data Processing
The data used for this data set exhibit different processing statuses. Fully processed data were received at BODC, in separate files, one was merged from the navigation and oceanlogger systems and the anemometer data were sent in individual files.
The merged data had a 1 minute resolution starting on 10 March 2009 00:00 hours and ending on 17 April 2009 23:59 hours. The originator's merged file contained 14 channels, their variables and units are: time (seconds), time_jday (days), sst (°c90), psal (pss-78), fluor (µg l-1), par (µmol m-2 s-1), latitude (degrees), longitude (degrees), conductivity (s m-1), salintemp (degc90), fluortemp (degc90), flowrate (l min-1), sim500_depth (m).
This document describes the procedures applied to the navigation data.
Files delivered to BODC
Filename | Content description | Format | Interval | Start date/time (UTC) | End date/time (UTC) |
JR200_alldataCal_1min | Originator processed position | nc | 60s | 10/03/2009 00:00:58 | 17/04/2009 23:58:31 |
gyro070 to gyro108 | ship's orientation | nc | 1s | 10/03/2009 00:00:00 | 17/04/2009 23:59:59 |
BODC Data Processing
The files mentioned above were selected for data banking as they contain the best version of processed position, heading and bathymetry. Data were banked at BODC following standard data banking procedures, including reduction through averaging, checking navigation channels for improbable values, working out speed over ground, and screening the data for anomalous values.
The originator's variables were mapped to appropriate BODC parameter codes as follows:
JR200_alldataCal_1min
Originator's variable | Originator's units | BODC code | BODC units | Unit conversion | Comments |
latitude | decimal degrees | ALATGP01 | decimal degrees | - | - |
longitude | decimal degrees | ALONGP01 | decimal degrees | - | - |
sim500_depth* | metres | MBANZZ01 | metres | - | - |
* note that despite having this name on the original file, the data was actually collected by the EA600 echosounder, as mentioned on the instrumentation description.
The file also contained surface hydrography parameters, however these will be dealt with on the appropriate document.
gyro
Originator's variable | Originator's units | BODC code | BODC units | Unit conversion | Comments |
heading | degrees true | HEADCM01 | degrees true | - | - |
All 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.
Position
A check was run on the position data and no gaps were identified. Several speed fails were identified, for these instances, positions were interpolated using linear interpolation.
Ship's velocities
Ship's eastward and northward velocities were calculated from the main latitude and longitude channels.
Ship's heading
Data were loaded and screened for any anomalous values. No issues were found.
Distance RunDistance run was calculated from the main latitude and longitude channels, starting from the beginning of the cruise.
Bathymetry
Bathymetry data from the echosounder was loaded and screened. N flags were applied to missing data, but in general the data exibits good quality.
Project Information
DISCOVERY 2010
DISCOVERY 2010 will investigate and describe the response of an ocean ecosystem to climate variability, climate change and commercial exploitation. The programme builds on past studies by BAS on the detailed nature of the South Georgia marine ecosystem and its links with the large-scale physical and biological behaviour of the Southern Ocean.
The aim is to identify, quantify and model key interactions and processes on scales that range from microscopic life forms to higher predators (penguins, albatrosses, seals and whales), and from the local to the circumpolar.
Objectives
Assess the links between the status of local marine food webs and variability and change in the Southern Ocean. Develop a linked set of ecosystem models applying relevant marine physics and biology over scales from the local to that of the entire Southern Ocean.
Relevance to Global Science
Ocean ecosystems play a crucial role in maintaining biodiversity, in depositing carbon into the deep ocean, and as a source of protein for humans. However, fishing and climate change are having significant and often detrimental effects. To predict the future state of ocean ecosystems we must develop computer models capable of simulating biological and physical processes on a range of scales from the local to an entire ocean. Developing such predictive models is crucial to the sustainable management of world fisheries and requires integrated analyses of the way whole ecosystems work. DISCOVERY 2010 aims to take this work forward and at the same time help manage the South Georgia and South Sandwich Islands maritime zone. We will do this through providing information on the state of the ecosystem to the Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR), the international body that manages sustainable fishing in the Southern Ocean.
Delivering the Results
DISCOVERY 2010 will undertake an integrated programme of shipboard and land-based field studies of the marine food web, combined with modelling. We will pay particular attention to critical phases in the life cycles of key species, and to examining interactive effects in food webs. Interacting biological and physical processes will be modelled across a range of spatial scales to significantly improve our representation of the ocean ecosystem, upon which sustainable management and the prediction of future climate change can be based. DISCOVERY 2010 will link to BIOFLAME, ACES, and COMPLEXITY, two international programmes, and to a collaborative programme with the University of East Anglia on the role of the Southern Ocean in the global carbon cycle.
Component Projects
- DISCOVERY-OEM: Ocean Ecosystems and Management
- DISCOVERY-FOOD-WEBS: Scotia Sea FOOD-WEBS
- DISCOVERY-FLEXICON: FLEXIbility and CONstraints in life histories
- DISCOVERY-CEMI: Circumpolar Ecosystems; Modelling and Integration
Data Activity or Cruise Information
Cruise
Cruise Name | JR20090310 (JR200, JR200A, JR208) |
Departure Date | 2009-03-10 |
Arrival Date | 2009-04-17 |
Principal Scientist(s) | Rebecca Korb (British Antarctic Survey) |
Ship | RRS James Clark Ross |
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 |