Search the data

Metadata Report for BODC Series Reference Number 56330

Metadata Summary

Data Description

Data Category CTD or STD cast
Instrument Type
Neil Brown MK3 CTD  CTD; water temperature sensor; salinity sensor; dissolved gas sensors
SeaTech transmissometer  transmissometers
Instrument Mounting research vessel
Originating Country United Kingdom
Originator -
Originating Organization Institute of Oceanographic Sciences Wormley Laboratory (now National Oceanography Centre, Southampton)
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) -

Data Identifiers

Originator's Identifier WPRDI10573BW
BODC Series Reference 56330

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 1982-07-15 16:09
End Time (yyyy-mm-dd hh:mm) -
Nominal Cycle Interval -

Spatial Co-ordinates

Latitude 44.31500 N ( 44° 18.9' N )
Longitude 13.72660 W ( 13° 43.6' W )
Positional Uncertainty 0.1 to 0.5 n.miles
Minimum Sensor or Sampling Depth 0.3 m
Maximum Sensor or Sampling Depth 4952.41 m
Minimum Sensor or Sampling Height 33.59 m
Maximum Sensor or Sampling Height 4985.7 m
Sea Floor Depth 4986.0 m
Sea Floor Depth Source -
Sensor or Sampling Distribution Variable common depth - All sensors are grouped effectively at the same depth, but this depth varies significantly during the series
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


BODC CODERankUnitsTitle
DOXYPR011Micromoles per litreConcentration of oxygen {O2 CAS 7782-44-7} per unit volume of the water body [dissolved plus reactive particulate phase] by in-situ Beckmann probe
PPOPPR011PercentPotential transmittance (red light wavelength) per unit length of the water body by red light transmissometer and correction to a path length of 1m and for seawater compressibility
PRESPR011DecibarsPressure (spatial coordinate) exerted by the water body by profiling pressure sensor and correction to read zero at sea level
PSALPR011DimensionlessPractical salinity of the water body by conductivity cell and computation using UNESCO 1983 algorithm
TEMPST011Degrees CelsiusTemperature of the water body by CTD or STD

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

Public domain 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.

The recommended acknowledgment is

"This study uses data from the data source/organisation/programme, provided by the British Oceanographic Data Centre and funded by the funding body."

Narrative Documents

Neil Brown MK3 CTD

The Neil Brown MK3 conductivity-temperature-depth (CTD) profiler consists of an integral unit containing pressure, temperature and conductivity sensors with an optional dissolved oxygen sensor in a pressure-hardened casing. The most widely used variant in the 1980s and 1990s was the MK3B. An upgrade to this, the MK3C, was developed to meet the requirements of the WOCE project.

The MK3C includes a low hysteresis, titanium strain gauge pressure transducer. The transducer temperature is measured separately, allowing correction for the effects of temperature on pressure measurements. The MK3C conductivity cell features a free flow, internal field design that eliminates ducted pumping and is not affected by external metallic objects such as guard cages and external sensors.

Additional optional sensors include pH and a pressure-temperature fluorometer. The instrument is no longer in production, but is supported (repair and calibration) by General Oceanics.


These specification apply to the MK3C version.

Pressure Temperature Conductivity

6500 m

3200 m (optional)

-3 to 32°C 1 to 6.5 S cm-1

0.0015% FS

0.03% FS < 1 msec


0.003°C < 30 msec

0.0001 S cm-1

0.0003 S cm-1 < 30 msec

Further details can be found in the specification sheet.

SeaTech Transmissometer


The transmissometer is designed to accurately measure the the amount of light transmitted by a modulated Light Emitting Diode (LED) through a fixed-length in-situ water column to a synchronous detector.


  • Water path length: 5 cm (for use in turbid waters) to 1 m (for use in clear ocean waters).
  • Beam diameter: 15 mm
  • Transmitted beam collimation: <3 milliradians
  • Receiver acceptance angle (in water): <18 milliradians
  • Light source wavelength: usually (but not exclusively) 660 nm (red light)


The instrument can be interfaced to Aanderaa RCM7 current meters. This is achieved by fitting the transmissometer in a slot cut into a customized RCM4-type vane.

A red LED (660 nm) is used for general applications looking at water column sediment load. However, green or blue LEDs can be fitted for specilised optics applications. The light source used is identified by the BODC parameter code.

Further details can be found in the manufacturer's Manual.

RRS Discovery Cruise 130 CTD Data Documentation


This document covers the CTD data collected on RRS Discovery Cruise 130 (June - August 1982) by the Institute of Oceanographic Sciences (Deacon Laboratory) Godalming, Surrey, UK., under the direction of P. M. Saunders.


The instrument used was a Neil Brown Instrument Systems CTD which measured pressure, temperature and conductivity and was fitted with a Beckman dissolved oxygen electrode. The CTD was used alongside a General Oceanics Rosette Multisampler with 12 water bottles, a 10 kHz pinger, a bottom echo-sounder and a SeaTech transmissometer.

Sampling Protocols

Lowering and retrieval rates of 0.5 to 1.5 m/s were employed and the sensors were flushed with distilled water on recovery. Bottle samples and reversing thermometer measurements were made on ascent and the sea water samples were analysed using a Guildline Autolab salinometer. Reversing thermometers were calibrated before and after the cruise.

Stations 10560 to 10574 were shared between the CTD/Multisampler and a 14m long hydrophone employed in listening for moored sound sources. Listening was performed on lowering and both CTD and bottle sample data were obtained on recovery. For stations 10555, 10556 and 10575 to 10599 the hydrophone was removed and CTD data were gathered on lowering and bottle samples obtained on recovery.

On seven stations during the cruise (10575, 10576, 10585, 10587, 10592, 10593 and 10594) repeated lowerings were made between 4000m and the bottom.



The pressure sensor was calibrated in a laboratory in September 1980 and repeat calibrations of January and October 1982 showed the same slope. The deck pressure offset was stable and a value of 10db was assumed for all stations.

The table below shows differences between the pressures determined from pairs of reversing thermometers (protected and unprotected) and simultaneous observations of CTD pressure.

For stations where the bottom is flat the depth of the CTD can be estimated from the corrected water depth minus the height of the echosounder above the bottom. This is converted to pressure and compared with the measured CTD pressure. 11 such determinations gave the mean difference 3db (CTD lower) and an rms of 6db very similar to the reversing thermometer values.


Laboratory calibrations of January 1982 and October 1982 showed the CTD temperature sensor to be stable. By comparison with 57 reversing thermometer measurements between 2 and 23 °C the corrected CTD temperatures were determined from the equation:

T = 0.047 + 0.0005002 * RAWTEMP.


During the cruise, bottle salinities and reversing thermometer measurements revealed a linear potential temperature (POTT) - practical salinity (S) relationship for POTT less than 2.6 °C of:

S = 34.698 + 0.098 * POTT

The cell factor required to bring provisional CTD salinities into agreement with this relation was determined for each station.

The table below compares salinities derived from the rosette sampler and Guildline salinometer with the CTD values.

If a constant cell factor had been used the deviations from the POTT-S relation measured with the CTD may be plotted - this indicates that the stability of the CTD is good excluding 3 outliers. These are stations 10556, 10563 and 10567 and may be the result of partial fouling.


From a sample value of oxygen concentration (determined by the Winkler method) the fractional saturation content was obtained by normalising it by the appropriate saturation value. The Beckman oxygen cell also measures fractional saturation F, given by the equation:

ln F = ln I + ln C + aT + bp


I = oxygen probe current
T = temperature
p = pressure

A least squares fit of 46 data sets gave:

C = 1.47E-03
a = -0.035 per °C
b = 1.425E-04 per db

The electrode current exhibits a time dependent lag which has been corrected using the expression:

LAG (secs) = 70 e -0.1 x T (ambient) °C

This equation is a reasonable fit to the behaviour of the electrode from 3000m to 5000m where the water is nearly isothermal (2.5 °C - 3.0 °C).

There are some spikes in the oxygen profiles, particularly during the upcasts. These are probably the result halting recovery of the CTD while collecting a bottle sample. These spikes have not been flagged.


Potential transmittance, which takes account of the increasing mass of clear water in the 1m path of the instrument with increasing pressure, was calculated.

Fit of CTD Data to Rosette Sample Values

  Difference between CTD and Rosette Measurements
Variable Range Mean Difference R.M.S. Number
Pressure (db) 0-2000 db +3 7 14
  2000-5600 db -2 6 28
Temperature °C 5-23 °C +0.005 0.012 33
  2-5 °C -0.0005 0.005 24
Salinity (PSU) 0-2000 db 0.003 0.007 48
  2000-5600 db -0.002 0.003 39
Oxygen (ml/l) 0-2000 db 0.25 0.30 23
  2000-5600 db 0.0 0.16 23

The depth of the 5 °C isotherm is approximately 1800 db.

Data Processing

Original values were averaged over an interval of one second and calibration coefficients and correction factors applied. A time constant correction algorithm was employed to compensate for the slower response of the platinum resistance thermometer.

Differences between successive values of each parameter were examined; the mean difference and its standard deviation calculated and values greater than several standard deviations from the mean difference were checked. Genuinely suspect data were then replaced by interpolated values.

Derived quantities were computed from algorithms published by Fofonoff and Millard (1983).


Saunders, P.M. (1984).
CTD data from the north east Atlantic Ocean 31° N - 46° N, July 1982. RRS Discovery Cruise 130. Institute of Oceanographic Sciences, Report No. 165.

Fofonoff, N.P. and Millard Jr., R.C. (1983).
Algorithms for the computation of fundamental properties of sea water. UNESCO Technical Paper on Marine Science 44.

Project Information

No Project Information held for the Series

Data Activity or Cruise Information


Cruise Name D130B
Departure Date 1982-07-10
Arrival Date 1982-08-05
Principal Scientist(s)Peter M Saunders (Institute of Oceanographic Sciences Wormley Laboratory)
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