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Metadata Report for BODC Series Reference Number 2308861


Metadata Summary

Data Description

Data Category Water sample data
Instrument Type
NameCategories
Niskin bottle  discrete water samplers
Chelsea Technologies Group Aquatracka III fluorometer  fluorometers
Instrument Mounting lowered unmanned submersible
Originating Country United Kingdom
Originator Dr Sue Hartman
Originating Organization National Oceanography Centre, Southampton
Processing Status banked
Online delivery of data Download available - Ocean Data View (ODV) format
Project(s) AtlantiS
 

Data Identifiers

Originator's Identifier JC278_CTD_PIGX_699:JC278_CTD004
BODC Series Reference 2308861
 

Time Co-ordinates(UT)

Start Time (yyyy-mm-dd hh:mm) 2025-06-02 05:53
End Time (yyyy-mm-dd hh:mm) -
Nominal Cycle Interval -
 

Spatial Co-ordinates

Latitude 48.51100 N ( 48° 30.7' N )
Longitude 9.93133 W ( 9° 55.9' W )
Positional Uncertainty 0.0 to 0.01 n.miles
Minimum Sensor or Sampling Depth 4.9 m
Maximum Sensor or Sampling Depth 2129.8 m
Minimum Sensor or Sampling Height 16.2 m
Maximum Sensor or Sampling Height 2141.1 m
Sea Floor Depth 2146.0 m
Sea Floor Depth Source DATAHEAD
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
 

Parameters

BODC CODERankUnitsTitle
ADEPZZ011MetresDepth (spatial coordinate) relative to water surface in the water body
BOTTFLAG1Not applicableSampling process quality flag (BODC C22)
CPHLPM011Milligrams per cubic metreConcentration of chlorophyll-a {chl-a CAS 479-61-8} per unit volume of the water body [particulate >unknown phase] by in-situ chlorophyll fluorometer and manufacturer's calibration applied
ROSPOSID1DimensionlessBottle rosette position identifier
SAMPRFNM1DimensionlessSample reference number

Definition of BOTTFLAG

BOTTFLAGDefinition
0The sampling event occurred without any incident being reported to BODC.
1The filter in an in-situ sampling pump physically ruptured during sample resulting in an unquantifiable loss of sampled material.
2Analytical evidence (e.g. surface water salinity measured on a sample collected at depth) indicates that the water sample has been contaminated by water from depths other than the depths of sampling.
3The feedback indicator on the deck unit reported that the bottle closure command had failed. General Oceanics deck units used on NERC vessels in the 80s and 90s were renowned for reporting misfires when the bottle had been closed. This flag is also suitable for when a trigger command is mistakenly sent to a bottle that has previously been fired.
4During the sampling deployment the bottle was fired in an order other than incrementing rosette position. Indicative of the potential for errors in the assignment of bottle firing depth, especially with General Oceanics rosettes.
5Water was reported to be escaping from the bottle as the rosette was being recovered.
6The bottle seals were observed to be incorrectly seated and the bottle was only part full of water on recovery.
7Either the bottle was found to contain no sample on recovery or there was no bottle fitted to the rosette position fired (but SBE35 record may exist).
8There is reason to doubt the accuracy of the sampling depth associated with the sample.
9The bottle air vent had not been closed prior to deployment giving rise to a risk of sample contamination through leakage.

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

Data access conditions (generic)

Access to these data is currently restricted and the data may not be released by BODC without obtaining specific permission from the data originator.


Narrative Documents

Niskin Bottle

The Niskin bottle is a device used by oceanographers to collect subsurface seawater samples. It is a plastic bottle with caps and rubber seals at each end and is deployed with the caps held open, allowing free-flushing of the bottle as it moves through the water column.

Standard Niskin

The standard version of the bottle includes a plastic-coated metal spring or elastic cord running through the interior of the bottle that joins the two caps, and the caps are held open against the spring by plastic lanyards. When the bottle reaches the desired depth the lanyards are released by a pressure-actuated switch, command signal or messenger weight and the caps are forced shut and sealed, trapping the seawater sample.

Lever Action Niskin

The Lever Action Niskin Bottle differs from the standard version, in that the caps are held open during deployment by externally mounted stainless steel springs rather than an internal spring or cord. Lever Action Niskins are recommended for applications where a completely clear sample chamber is critical or for use in deep cold water.

Clean Sampling

A modified version of the standard Niskin bottle has been developed for clean sampling. This is teflon-coated and uses a latex cord to close the caps rather than a metal spring. The clean version of the Levered Action Niskin bottle is also teflon-coated and uses epoxy covered springs in place of the stainless steel springs. These bottles are specifically designed to minimise metal contamination when sampling trace metals.

Deployment

Bottles may be deployed singly clamped to a wire or in groups of up to 48 on a rosette. Standard bottles and Lever Action bottles have a capacity between 1.7 and 30 L. Reversing thermometers may be attached to a spring-loaded disk that rotates through 180° on bottle closure.

Chelsea Technologies Group Aquatracka MKIII fluorometer

The Chelsea Technologies Group Aquatracka MKIII is a logarithmic response fluorometer. Filters are available to enable the instrument to measure chlorophyll, rhodamine, fluorescein and turbidity.

It uses a pulsed (5.5 Hz) xenon light source discharging along two signal paths to eliminate variations in the flashlamp intensity. The reference path measures the intensity of the light source whilst the signal path measures the intensity of the light emitted from the specimen under test. The reference signal and the emitted light signals are then applied to a ratiometric circuit. In this circuit, the ratio of returned signal to reference signal is computed and scaled logarithmically to achieve a wide dynamic range. The logarithmic conversion accuracy is maintained at better than one percent of the reading over the full output range of the instrument.

Two variants of the instrument are available, both manufactured in titanium, capable of operating in depths from shallow water down to 2000 m and 6000 m respectively. The optical characteristics of the instrument in its different detection modes are visible below:

Excitation Chlorophyll a Rhodamine Fluorescein Turbidity
Wavelength (nm) 430 500 485 440*
Bandwidth (nm) 105 70 22 80*
Emission Chlorophyll a Rhodamine Fluorescein Turbidity
Wavelength (nm) 685 590 530 440*
Bandwidth (nm) 30 45 30 80*

* The wavelengths for the turbidity filters are customer selectable but must be in the range 400 to 700 nm. The same wavelength is used in the excitation path and the emission path.

The instrument measures chlorophyll a, rhodamine and fluorescein with a concentration range of 0.01 µg l-1 to 100 µg l-1. The concentration range for turbidity is 0.01 to 100 FTU (other wavelengths are available on request).

The instrument accuracy is ± 0.02 µg l-1 (or ± 3% of the reading, whichever is greater) for chlorophyll a, rhodamine and fluorescein. The accuracy for turbidity, over a 0 - 10 FTU range, is ± 0.02 FTU (or ± 3% of the reading, whichever is greater).

Further details are available from the Aquatracka MKIII specification sheet.

CTD upcast data at time of bottle firing for JC278

Acquisition description:

Sampling methodology

19 stainless steel CTD (Conductivity, Temperature, Depth) casts were undertaken during the RRS James Cook cruise 278 (JC278), between the 30th of May 2025 to 23rd June 2025, at the Porcupine Abyssal Plain - Sustained Observatory (PAP-SO) site in the North East Atlantic ocean. An NMF (National Marine Facilities) 24-way Stainless Steel CTD frame was used with 20 litre Niskin water samplers. The CTD was deployed on CTD wire storage drum 2, and was operated out of the water bottle annex by the ship’s crew, using the winch belly box. Once over the side, the CTD was lowered to a depth of 10 metres, allowing time for the SBE (Sea-Bird Electronics) 5T pumps to prime. The winch system Active Heave Compensation (ACH) was used throughout JC278 (when below 100 metres) with no issues. The Niskin water samplers were fired to collect samples, and the upcast data was recorded at the time of bottle firing. Dual Sea-Bird SBE 43 dissolved oxygen sensors were used. The primary temperature (Sea-Bird SBE 3plus (SBE 3P)), conductivity (Sea-Bird SBE 4C) and dissolved oxygen (Sea-Bird SBE 43) sensors were fitted to the Sea-Bird SBE 9Plus, with the secondary sensors mounted on the vane. The shallowest cast was CTD001 at 125 metres and the deepest was CTD013 at 4840 metres. Between casts, the whole CTD package was rinsed with fresh water, with particular attention paid to the SBE 32 latch assembly. After each cast, the primary and secondary sensors were flushed three times with Milli-Q. Periodically, the optical sensors were also cleaned with Milli-Q and optic prep wipes.

Analytical methodology

There were no major technical issues with the Stainless Steel CTD suite during JC278. During the first 2 casts, it was noticed the oxygen differences were ranging from 8 – 12 % saturation (Sea-Bird recommends below 4%). Once the oxygen sampling data had been received, the issue was pinpointed to the primary sensor. The sensor was changed and from then onwards saturation was below 1%.

Instrument description

Further information can be found in the JC278 CTD Instrumentation document.

JC278 Cruise report

Further information can be found in the JC278 Cruise report.

BODC Data Processing Procedures

Data received were loaded into the BODC database using established BODC data banking procedures. A parameter mapping table is provided below:

Originator's Variable Originator's Units BODC Parameter Code BODC's Units Comments
T090C degC TEMPCU01 Degrees (UAAA)
T190C degC TEMPCU02 Degrees Celsius (UPAA)
Sal00 PSU PSALCU01 Dimensionless (UUUU)
Sal11 PSU PSALCU02 Dimensionless (UUUU)
Sbeox0Mm/L Mm/L DOXYSU01 Micromoles per litre (UPOX)
sbeox1Mm/L Mm/L DOXYSU02 Micromoles per litre (UPOX)
CStarTr0 Percent POPTDR01 Percent (UPCT)
turbWETbb0 m^1/sr BVSFO650 per metre per steradian (PMSR)
par umol photons/m^2/sec IRRUUV01 MicroEinsteins per square metre per second (UMES) Units are equivalent.
par1 umol photons/m^2/sec IRRDUV01 MicroEinsteins per square metre per second (UMES) Units are equivalent.
flC ug/l CPHLPM01 Milligrams per cubic metre (UMMC) Units are equivalent.

Data Quality Report

28 values of BVSFO650 were below 0 /m/sr and BODC flag 'M' was applied to each occurrence, indicating there may be a problem with the data.

BODC flag 'M' was also applied to data points that were significantly different from the trend of the data, this occurred in parameters DOXYSU01, POPTDR01, BVSFO650 and DOXYSU02.


Project Information

Marine LTSS: AtlantiS (Atlantic Climate and Environment Strategic Science)

Introduction

AtlantiS is a five year (2024 to 2029) programme, funded by the Natural Environment Research Council (NERC).

Scientific Rationale

The global ocean is the largest part of the Earth's climate system and acts as a major buffer to climate changes resulting from human activities. By absorbing 90% of excess heat and nearly a quarter of carbon resulting from anthropogenic greenhouse gas emissions, the ocean has already substantially mitigated climate change in the atmosphere and on land. However, this service has come at a cost to the health and resilience of the ocean and by extension the people who depend on it. Significant damage has been caused to biodiversity and productivity of marine ecosystems, to shelf seas and coastal environments, and to inland areas through extremes of weather. The futures of regional climate and ecological systems depend on the response of the ocean to multiple anthropogenic stressors. Understanding and predicting the response is fundamental for sustainable development and to guide adaptation and mitigation.

The challenge is that the ocean is so large and variable that it cannot be completely and fully observed. Achieving adequate knowledge on all scales requires international coordination of observing and modelling over decades. It requires advancement in technology to expand our ability to observe beyond individual ships. It requires expanding the range of variables measured to include biogeochemistry and ecology. The opportunity now is to lead new capability to combine observations from a widening range of platforms and sensors, next-generation ocean and coupled models, and innovation in digital tools to meet the goal above. A range of national and international reviews have identified priority knowledge gaps related to natural and anthropogenically driven changes in the global ocean and the Atlantic and its shelf seas, and their impacts on marine ecosystems and human society:

  • how natural and anthropogenic drivers of basin and decadal changes alter the Atlantic ecosystem, and the consequences for ecosystem functioning and services;
  • the importance of ocean-shelf-coast connectivity in shaping ecosystems, biodiversity, natural hazards and impacts on society;
  • the implications and feedbacks associated with climate mitigation strategies, and the need for improved assessments and advice to policy makers;
  • the sensitivity and timescales of feedbacks that determine the ability of the ocean to continue to mitigate climate change by absorbing excess heat and carbon.

The aim of the AtlantiS programme is to provide evidence, tools and knowledge to support the ambition for healthy, biologically diverse and resilient marine environments, a sustainable blue economy and communities safe from natural hazards. The objectives are to strengthen the capacity of UK marine science to observe, model and predict the ocean through a step change in capability to maximise the value inherent in marine data; to transform the ocean from being data poor to data rich; to provide global syntheses of iconic climate change indicators; to lead an increase in public and government understanding of the role of the ocean in climate; and to communicate actionable knowledge effectively. AtlantiS is the continuation and development of the CLASS programme, enhancing the long-term, large-scale ocean observation systems and the ocean value-chain that contributes to key national and international programmes and priorities.


Data Activity or Cruise Information

Data Activity

Start Date (yyyy-mm-dd) 2025-06-02
End Date (yyyy-mm-dd) Ongoing
Organization Undertaking ActivityNational Oceanography Centre, Southampton
Country of OrganizationUnited Kingdom
Originator's Data Activity IdentifierJC278_CTD_JC278_CTD004
Platform Categorylowered unmanned submersible

BODC Sample Metadata Report for JC278_CTD_JC278_CTD004

Sample reference number Nominal collection volume(l) Bottle rosette position Bottle firing sequence number Minimum pressure sampled (dbar) Maximum pressure sampled (dbar) Depth of sampling point (m) Bottle type Sample quality flag Bottle reference Comments
3534608   20.00 1   2158.40 2159.40 2129.70 Niskin bottle No problem reported    
3534611   20.00 2   2158.50 2159.50 2129.80 Niskin bottle No problem reported    
3534614   20.00 5    686.00  687.00  679.50 Niskin bottle No problem reported    
3534617   20.00 6    686.00  687.00  679.50 Niskin bottle No problem reported    
3534620   20.00 9    685.90  686.90  679.50 Niskin bottle No problem reported    
3534623   20.00 10    685.90  686.90  679.50 Niskin bottle No problem reported    
3534626   20.00 13     41.10   42.10   41.30 Niskin bottle No problem reported    
3534629   20.00 14     40.70   41.70   40.80 Niskin bottle No problem reported    
3534632   20.00 15     41.00   42.00   41.20 Niskin bottle No problem reported    
3534635   20.00 16     40.70   41.70   40.80 Niskin bottle No problem reported    
3534638   20.00 17     41.00   42.00   41.20 Niskin bottle No problem reported    
3534641   20.00 18     40.50   41.50   40.60 Niskin bottle No problem reported    
3534644   20.00 19     40.70   41.70   40.80 Niskin bottle No problem reported    
3534647   20.00 20     40.50   41.50   40.70 Niskin bottle No problem reported    
3534650   20.00 21      4.40    5.40    4.90 Niskin bottle No problem reported    
3534653   20.00 22      4.50    5.50    5.00 Niskin bottle No problem reported    
3534656   20.00 23      4.50    5.50    5.00 Niskin bottle No problem reported    
3534659   20.00 24      4.60    5.60    5.10 Niskin bottle No problem reported    

Please note:the supplied parameters may not have been sampled from all the bottle firings described in the table above. Cross-match the Sample Reference Number above against the SAMPRFNM value in the data file to identify the relevant metadata.

Related Data Activity activities are detailed in Appendix 1

Cruise

Cruise Name JC278
Departure Date 2025-05-30
Arrival Date 2025-06-23
Principal Scientist(s)Andrew R Gates (National Oceanography Centre, Southampton)
Ship RRS James Cook

Complete Cruise Metadata Report is available here


Fixed Station Information

Fixed Station Information

Station NameWhittard Canyon - The Canyons Marine Conservation Zone
CategoryOffshore area
Latitude48° 6.00' N
Longitude10° 18.00' W
Water depth below MSL3600.0 m

Fixed Station - Whittard Canyon - The Canyons Marine Conservation Zone

The Canyons MCZ is located in the far south-west corner of the UK continental shelf, more than 330 km from Land's End, Cornwall. It encompasses the steep part of the shelf break where the seabed drops from a depth of 100 m to the oceanic abyssal plain at 2000 m. It is unique within the context of England's largely shallow seas due to its depth, sea-bed topography and the coral features it contains.

There are two large canyons within the site, which add to its topographic complexity: the Explorer Canyon to the north and the Dangaard Canyon below it. The wider Whittard Canyon area encapsulates the Canyons MCZ and also includes a network of submarine canyons to the West. The MCZ, also known as a Marine Protected Area (MPA), was designated in November 2013 under the Marine and Coastal Access Act (2009). The Canyons MCZ covers an area of 661 km2, which extends to approximately 5200 km2 when Whittard Canyon is included.

On the northernmost wall of the Explorer Canyon is a patch of live Cold-water coral reef (Lophelia pertusa) and Coral gardens, both of which are a OSPAR threatened and/or declining habitat. This is the only known example of living Cold-water coral reef recorded within England's seas, making it unique in these waters.

Cold-water corals and Coral gardens typically support a range of other organisms. The coral provides a three-dimensional structure and a variety of microhabitats that provide shelter and an attachment surface for other species. Both Cold-water corals and Coral gardens can be long-lived but are extremely slow growing (at about 6 mm a year), making protection important for their conservation. Another reef-forming cold-water coral, Madrepora oculata, is also present in the site.

The variety of deep-sea bed communities present are indicative of the range of substrates found in and around the canyons, including bedrock, biogenic reef, coral rubble, coarse sediment, mud and sand. These biological communities include cold-water coral communities (Lophelia pertusa and Madrepora oculata), Coral gardens, feather star (Leptometra celtica) assemblages and Sea-pen and burrowing megafauna communities (including, burrowing anemone fields, squat lobster (Munida sp.) assemblages, barnacle assemblages and deep-sea sea-pen (Kophobelemnon sp.) fields).


BODC image

Sampling History

JC035 (2009) JC125 (2015) JC166/7 (2018)
ROV video/photography Y Y Y
AUV video/photography N Y Y
Shipboard Multibeam Bathymetry Y Y Y
AUV Multibeam Bathymetry N Y Y
AUV Sidescan Sonar N Y Y
TOBI Sidescan Sonar Y Y Y
ROV vibrocorer N Y N
CTD casts N Y N
SAPS N Y N

Related Fixed Station activities are detailed in Appendix 2


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: JC278_CTD_JC278_CTD004

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
2308664Water sample data2025-06-02 05:53:3548.511 N, 9.93133 WRRS James Cook JC278

Appendix 2: Whittard Canyon - The Canyons Marine Conservation Zone

Related series for this Fixed Station 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
2026920Bathymetry2009-06-09 00:00:0047.1792 N, 11.2483 WRRS James Cook JC035
2026932Bathymetry2009-06-09 00:00:0048.4273 N, 11.2343 WRRS James Cook JC035
2202723CTD or STD cast2009-06-22 14:25:0548.15317 N, 10.53967 WRRS James Cook JC036
2202735CTD or STD cast2009-07-09 18:58:1948.81283 N, 11.15917 WRRS James Cook JC036
2202747CTD or STD cast2009-07-10 23:22:1548.2835 N, 10.314 WRRS James Cook JC036
2202759CTD or STD cast2009-07-12 00:52:4848.26533 N, 10.182 WRRS James Cook JC036
2202760CTD or STD cast2009-07-18 05:48:1748.60333 N, 9.9665 WRRS James Cook JC036
2202772CTD or STD cast2009-07-26 03:59:1848.653 N, 10.033 WRRS James Cook JC036
2202803CTD or STD cast2015-08-13 21:32:1247.9595 N, 10.217 WRRS James Cook JC125 (JC124, JC126)
2027020Bathymetry2015-08-14 01:23:0047.5404 N, 11.2236 WRRS James Cook JC125 (JC124, JC126)
2027032Bathymetry2015-08-15 02:05:0048.4621 N, 9.9608 WRRS James Cook JC125 (JC124, JC126)
2202815CTD or STD cast2015-08-15 15:56:3648.38949 N, 9.99615 WRRS James Cook JC125 (JC124, JC126)
2202827CTD or STD cast2015-08-16 17:12:5648.65512 N, 10.03444 WRRS James Cook JC125 (JC124, JC126)
2202839CTD or STD cast2015-08-20 03:56:2848.65348 N, 10.03337 WRRS James Cook JC125 (JC124, JC126)
2202840CTD or STD cast2015-08-20 10:30:0948.76099 N, 10.4609 WRRS James Cook JC125 (JC124, JC126)
2202852CTD or STD cast2015-08-25 10:31:4648.46176 N, 9.63347 WRRS James Cook JC125 (JC124, JC126)
2202864CTD or STD cast2015-08-25 12:17:3048.46583 N, 9.63871 WRRS James Cook JC125 (JC124, JC126)
2202876CTD or STD cast2015-08-25 13:59:1848.4682 N, 9.64339 WRRS James Cook JC125 (JC124, JC126)
2202888CTD or STD cast2015-08-26 10:01:4348.47488 N, 9.6532 WRRS James Cook JC125 (JC124, JC126)
2202907CTD or STD cast2015-08-26 13:34:1548.46164 N, 9.63353 WRRS James Cook JC125 (JC124, JC126)
2202919CTD or STD cast2015-08-26 15:00:4748.46574 N, 9.63858 WRRS James Cook JC125 (JC124, JC126)
2202920CTD or STD cast2015-08-26 18:36:1848.46819 N, 9.64337 WRRS James Cook JC125 (JC124, JC126)
2202932CTD or STD cast2015-08-26 20:04:1848.47199 N, 9.64881 WRRS James Cook JC125 (JC124, JC126)
2202944CTD or STD cast2015-08-26 21:54:2148.48103 N, 9.6606 WRRS James Cook JC125 (JC124, JC126)
2202956CTD or STD cast2015-08-26 23:32:1048.49106 N, 9.67511 WRRS James Cook JC125 (JC124, JC126)
2202968CTD or STD cast2015-09-01 08:36:1048.47488 N, 9.65322 WRRS James Cook JC125 (JC124, JC126)
2202981CTD or STD cast2015-09-06 02:27:1348.65368 N, 10.03353 WRRS James Cook JC125 (JC124, JC126)
2202993CTD or STD cast2015-09-06 12:37:1548.48615 N, 10.04908 WRRS James Cook JC125 (JC124, JC126)
2026993Bathymetry2018-06-23 23:02:0047.4704 N, 10.586 WRRS James Cook JC166 (JC167)
2027007Bathymetry2018-06-24 19:43:0048.2761 N, 9.8577 WRRS James Cook JC166 (JC167)
2205929Hydrography time series at depth2019-07-08 06:25:0948.62615 N, 10.00373 WRRS Discovery DY103
2222318Currents -subsurface Eulerian2019-07-08 06:55:0048.62615 N, 10.00373 WRRS Discovery DY103
2222306Currents -subsurface Eulerian2019-07-08 07:00:0048.62615 N, 10.00373 WRRS Discovery DY103
2205917Hydrography time series at depth2019-07-08 07:12:2148.62615 N, 10.00373 WRRS Discovery DY103
2222343Currents -subsurface Eulerian2020-11-13 12:18:0048.626 N, 10.004 WRRS Discovery DY116
2222331Currents -subsurface Eulerian2020-11-13 12:30:0048.626 N, 10.004 WRRS Discovery DY116
2205930Hydrography time series at depth2020-11-13 13:00:0148.3756 N, 10.024 WRRS Discovery DY116
2205942Hydrography time series at depth2020-11-13 13:00:0148.3756 N, 10.024 WRRS Discovery DY116
2222367Currents -subsurface Eulerian2021-03-29 12:09:0248.626 N, 9.996 WRRS Discovery DY130
2206761Hydrography time series at depth2021-03-29 12:10:3348.626 N, 9.996 WRRS Discovery DY130
2206773Hydrography time series at depth2021-03-29 12:13:0648.626 N, 9.996 WRRS Discovery DY130
2222355Currents -subsurface Eulerian2021-03-29 12:24:5148.626 N, 9.996 WRRS Discovery DY130
2222379Currents -subsurface Eulerian2022-01-01 00:25:3248.626 N, 9.996 WRRS Discovery DY130
2225469Bathymetry2022-07-10 00:00:0047.8623 N, 10.8343 WRRS Discovery DY152
2225494Bathymetry2022-08-06 00:00:0048.1325 N, 10.6492 WRRS James Cook JC237
2202483CTD or STD cast2022-08-08 01:20:2547.89354 N, 10.17301 WRRS James Cook JC237
2202495CTD or STD cast2022-08-09 16:07:1048.25988 N, 9.67387 WRRS James Cook JC237
2202502CTD or STD cast2022-08-11 14:57:4348.68134 N, 10.05642 WRRS James Cook JC237
2202514CTD or STD cast2022-08-12 10:37:5248.6533 N, 10.03587 WRRS James Cook JC237
2202526CTD or STD cast2022-08-15 09:51:3448.75935 N, 10.4597 WRRS James Cook JC237
2202538CTD or STD cast2022-08-19 06:12:5548.39767 N, 9.83574 WRRS James Cook JC237
2202551CTD or STD cast2022-08-19 07:32:0848.3976 N, 9.83558 WRRS James Cook JC237
2202563CTD or STD cast2022-08-19 08:45:4748.3977 N, 9.83563 WRRS James Cook JC237
2202575CTD or STD cast2022-08-19 10:03:4748.39771 N, 9.83557 WRRS James Cook JC237
2202587CTD or STD cast2022-08-19 11:32:1848.39793 N, 9.83535 WRRS James Cook JC237
2202599CTD or STD cast2022-08-19 13:46:1848.398 N, 9.83528 WRRS James Cook JC237
2202606CTD or STD cast2022-08-19 15:41:2048.39802 N, 9.83522 WRRS James Cook JC237
2202618CTD or STD cast2022-08-19 17:15:0748.39802 N, 9.83522 WRRS James Cook JC237
2202631CTD or STD cast2022-08-21 13:43:3348.52944 N, 9.93624 WRRS James Cook JC237
2202643CTD or STD cast2022-08-21 18:33:0848.6527 N, 10.03528 WRRS James Cook JC237
2202655CTD or STD cast2022-08-21 20:59:1148.73153 N, 10.09842 WRRS James Cook JC237
2202667CTD or STD cast2022-08-22 18:40:0448.41286 N, 9.83279 WRRS James Cook JC237
2202679CTD or STD cast2022-08-23 13:46:4648.57121 N, 9.93517 WRRS James Cook JC237
2202692CTD or STD cast2022-08-31 10:55:2348.65286 N, 10.03526 WRRS James Cook JC237
2202711CTD or STD cast2022-09-01 15:18:2748.31993 N, 9.79096 WRRS James Cook JC237
2243704Water sample data2023-05-07 11:43:0248.6033 N, 9.9683 WRRS James Cook JC247
2242910Bathymetry2023-06-18 00:00:0048.02085 N, 11.15677 WRRS Discovery DY166
2308640Water sample data2025-05-31 19:57:0048.404 N, 9.695 WRRS James Cook JC278
2308836Water sample data2025-05-31 19:57:0048.404 N, 9.695 WRRS James Cook JC278
2308652Water sample data2025-06-01 05:56:3648.4385 N, 9.74433 WRRS James Cook JC278
2308848Water sample data2025-06-01 05:56:3648.4385 N, 9.74433 WRRS James Cook JC278
2308664Water sample data2025-06-02 05:53:3548.511 N, 9.93133 WRRS James Cook JC278