Metadata Report for BODC Series Reference Number 947397
All data from this channel should be used with caution as the values measured were unrealistic during this and several other cruises. Readings taken by the probe indicated that the sensor was constantly saturated. It is advised that the data should only be used for relative comparisons.
Data quality notes
LISST transmission and scattering
Users should be aware that the clear water values measured on different cruises are observed to increase and decrease at times, which is not consistent behaviour. In addition, the clear water scattering values are also sometimes less than and sometimes greater than those measured by the manufacturer at the time of last calibration (October 2006). This may be due to a problem with the instrument or the method in which the clear water values are measured.
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."
Sea Bird Electronics SBE13 Dissolved Oxygen Sensor
The SBE 13 was designed as an auxiliary sensor for Sea Bird SBE 9plus, but can fitted in custom instrumentation applications. When used with the SBE 9 Underwater Unit, a flow-through plenum improves the data quality, as the pumping water over the sensor membrane reduces the errors caused by oxygen depletion during the periods of slow or intermittent flushing and also reduces exposure to biofouling.
The output voltage is proportional to membrane current (oxygen current) and to the sensor element's membrane temperature (oxygen temperature), which is used for internal temperature compensation.
Two versions of the SBE 13 are available: the SBE 13Y uses a YSI polarographic element with replaceable membranes to provide in situ measurements up to 2000 m depth and the SBE 13B uses a Beckman polarographic element to provide in situ measurements up to 10500 m depth, depending on the sensor casing. This sensor includes a replaceable sealed electrolyte membrane cartridge.
The SBE 13 instrument has been out of production since 2001 and has been superseded by the SBE 43.
|Measurement range||0 to 15 mL L-1|
|Accuracy||0.1 mL L-1|
|Time response|| |
2 s at 25°C
5 s at 0°C
|Depth range|| |
2000 m (SBE 13Y- housing in anodized aluminum)
6800 m (SBE 13B- housing in anodized aluminum)
105000 m (SBE 13B- housing in titanium)
Further details can be found in the manufacturer's specification sheet.
Prince Madog cruise PD09_08 CTD Instrumentation
The CTD unit was a Sea-Bird Electronics 911plus system (SN P23655-0620), with dissolved oxygen sensor. The CTD was fitted with a red (660 nm) beam transmissometer, a fluorometer, a Sequoia Scientific Laser In-Situ Scattering and Transmissometry (LISST) particle analyser and a LI-COR Underwater Quantum Sensor. Also attached was a Sea-Bird SBE-35 Temperature Logger to supply an independent check of temperature. All instruments were attached to a Sea-Bird SBE 32 compact carousel. The table below lists more detailed information about the various sensors.
|Sensor||Model||Serial Number||Calibration (UT)||Comments|
|Pressure transducer||Paroscientific Digiquartz 42A-105||76076||2004-01-21||-|
|Conductivity sensor||SBE 4||2543||2004-01-14||-|
|Temperature sensor||SBE 3||P4100||2004-01-21||-|
|Dissolved oxygen||SBE 13 Beckmann||130580||2004-01-05||-|
|Transmissometer 660 nm||SeaTech T1000||T1021||1998-03-03||0.2 m path|
|Fluorometer||Turner SCUFA II||262||-||-|
|LISST||25A||120||2006-10-26||Range: 1.25 - 250 µm|
|LI-COR (contains CEFAS in-house electronics)||LI 192SB||CEFAS #26||-||-|
Change of sensors during cruise: None reported.
Rosette sampling system equipped with 5 l sampling bottles (manufactured by Ocean Test Equipment Inc.).
Sea-Bird Electronics SBE 911 and SBE 917 series CTD profilers
The SBE 911 and SBE 917 series of conductivity-temperature-depth (CTD) units are used to collect hydrographic profiles, including temperature, conductivity and pressure as standard. Each profiler consists of an underwater unit and deck unit or SEARAM. Auxiliary sensors, such as fluorometers, dissolved oxygen sensors and transmissometers, and carousel water samplers are commonly added to the underwater unit.
The CTD underwater unit (SBE 9 or SBE 9 plus) comprises a protective cage (usually with a carousel water sampler), including a main pressure housing containing power supplies, acquisition electronics, telemetry circuitry, and a suite of modular sensors. The original SBE 9 incorporated Sea-Bird's standard modular SBE 3 temperature sensor and SBE 4 conductivity sensor, and a Paroscientific Digiquartz pressure sensor. The conductivity cell was connected to a pump-fed plastic tubing circuit that could include auxiliary sensors. Each SBE 9 unit was custom built to individual specification. The SBE 9 was replaced in 1997 by an off-the-shelf version, termed the SBE 9 plus, that incorporated the SBE 3 plus (or SBE 3P) temperature sensor, SBE 4C conductivity sensor and a Paroscientific Digiquartz pressure sensor. Sensors could be connected to a pump-fed plastic tubing circuit or stand-alone.
Temperature, conductivity and pressure sensors
The conductivity, temperature, and pressure sensors supplied with Sea-Bird CTD systems have outputs in the form of variable frequencies, which are measured using high-speed parallel counters. The resulting count totals are converted to numeric representations of the original frequencies, which bear a direct relationship to temperature, conductivity or pressure. Sampling frequencies for these sensors are typically set at 24 Hz.
The temperature sensing element is a glass-coated thermistor bead, pressure-protected inside a stainless steel tube, while the conductivity sensing element is a cylindrical, flow-through, borosilicate glass cell with three internal platinum electrodes. Thermistor resistance or conductivity cell resistance, respectively, is the controlling element in an optimized Wien Bridge oscillator circuit, which produces a frequency output that can be converted to a temperature or conductivity reading. These sensors are available with depth ratings of 6800 m (aluminium housing) or 10500 m (titanium housing). The Paroscientific Digiquartz pressure sensor comprises a quartz crystal resonator that responds to pressure-induced stress, and temperature is measured for thermal compensation of the calculated pressure.
Optional sensors for dissolved oxygen, pH, light transmission, fluorescence and others do not require the very high levels of resolution needed in the primary CTD channels, nor do these sensors generally offer variable frequency outputs. Accordingly, signals from the auxiliary sensors are acquired using a conventional voltage-input multiplexed A/D converter (optional). Some Sea-Bird CTDs use a strain gauge pressure sensor (Senso-Metrics) in which case their pressure output data is in the same form as that from the auxiliary sensors as described above.
Deck unit or SEARAM
Each underwater unit is connected to a power supply and data logging system: the SBE 11 (or SBE 11 plus) deck unit allows real-time interfacing between the deck and the underwater unit via a conductive wire, while the submersible SBE 17 (or SBE 17 plus) SEARAM plugs directly into the underwater unit and data are downloaded on recovery of the CTD. The combination of SBE 9 and SBE 17 or SBE 11 are termed SBE 917 or SBE 911, respectively, while the combinations of SBE 9 plus and SBE 17 plus or SBE 11 plus are termed SBE 917 plus or SBE 911 plus.
Specifications for the SBE 9 plus underwater unit are listed below:
|Parameter||Range||Initial accuracy||Resolution at 24 Hz||Response time|
|Temperature||-5 to 35°C||0.001°C||0.0002°C||0.065 sec|
|Conductivity||0 to 7 S m-1||0.0003 S m-1||0.00004 S m-1||0.065 sec (pumped)|
|Pressure||0 to full scale (1400, 2000, 4200, 6800 or 10500 m)||0.015% of full scale||0.001% of full scale||0.015 sec|
Further details can be found in the manufacturer's specification sheet.
Turner Designs Self-Contained Underwater Fluorescence Apparatus (SCUFA)
The Turner Designs SCUFA is a submersible fluorometer for chlorophyll and dye tracing operations that has been designed to operate in a wide range of concentrations, environmental conditions as well as operational modes (profiling or moored deployments). The instrument includes an integrated temperature probe and software which allow for automatic correction of fluorescence data from temperature effects. The superior ambient light rejection eliminates the effects of sunlight and allows the SCUFA to be used in surface waters without the need for external pumps or light shields.
Each instrument can be customised to meet user requirements. Users can choose one of the following channels: chlorophyll a, cyanobacteria (phycocyanin or phycoerythrin pigments), rhodamine WT, fluorescein and turbidity. Instrument options include turbidity, internal data logging and automatic temperature correction.
Three versions of the SCUFA are available: SCUFA I, II and III. SCUFA I and II are used for chlorophyll a applications, while SCUFA III is used for Rhodamine WT. Models II and III include a turbidity channel that is not present on model I. The SCUFA has been out of production since 2008.
|Depth rating||600 m|
|Temperature range||-2 to 40°C|
|Maximum sampling rate|| |
5 Hz- analog
12 bit- digital
1.2 mV- analog
|Fluorescence||4 orders of magnitude|
|Turbidity||3 orders of magnitude|
The table below presents the specifications for the different channels.
|Light source||Blue|| |
595/670 (phycocyanin, PC)
528/573 (phycoerythrin, PE)
|Minimum detection Limit|
|Fluorescence||0.02 µg L-1||150 cells mL-1||0.04 ppb|
|Turbidity||0.05 NTU||0.05 NTU||0.05 NTU|
Further details can be found in the manufacturer's brochure.
LI-COR LI-192 Underwater Quantum Sensor
The LI-192 Underwater Quantum Sensor is used to measure photosynthetic photon flux density and is cosine corrected. The sensor is often referred to as LI-192SA or LI-192SB (the LI-192SB model was superseded by LI-192SA). One of the main differences is that the LI-192SA model includes a built-in voltage output for interfacing with NexSens iSIC and SDL data loggers.
(Specifications apply to both models unless otherwise stated)
|Absolute Calibration||± 5 % in air traceable to NBS.|
|Sensitivity||Typically 3 µA per 1000 µmol s-1 m-2 for LI-192SB and 4 µA per 1000 µmol s-1 m-2 for LI-192SA in water.|
|Linearity||Maximum deviation of 1 % up to 10,000 µmol s-1 m-2.|
|Stability||< ± 2 % change over a 1 year period.|
|Response Time||10 µs.|
|Temperature Dependence||± 0.15 % per °C maximum.|
|Cosine Correction||Optimized for both underwater and atmospheric use.|
|Azimuth||< ± 1 % error over 360 ° at 45 ° elevation.|
|Detector||High stability silicon photovoltaic detector (blue enhanced).|
|Sensor Housing||Corrosion resistant metal with acrylic diffuser for both saltwater and freshwater applications. Waterproof to withstand 800 psi (5500 kPa) (560 meters).|
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.
Sequoia Laser In-situ Sediment Size Transmissometer (LISST)
The Sequoia LISST measures particle size distribution of suspended sediments by laser diffraction. This technique allows particles of various compositions to be measured with a single device and, because the particle volume is roughly of the same order for all sizes, the required dynamic range of the sensors is reduced compared with single-particle counters.
The instrument includes optics for producing a collimated laser beam, a detector array, electronics for signal amplification and processing, a data storage and scheduling computer and a battery system. The primary measurement is the scattering of laser light at a number of angles, which is mathematically inverted to give a grain size distribution, and also scaled to obtain the volume scattering function. The size distribution is presented as concentration in each of 32 logarithmically-spaced grain-size class bins. Optical transmission, water depth and temperature are recorded as supporting measurements.
Several models are available and although the principals of operation are the same, their specifications vary slightly. The specifications for model LISST-100 are provided below.
|Optical path length|| |
5 cm (standard)
2.5 cm (optional)
|Optical transmission||12 bit resolution|
|Particle size range|| |
Type B: 1.25 to 250 micron diameter
Type C: 2.5 to 500 micron diameter
|Resolution||32 size classes, log-spaced|
|VSF angle range||1.7 to 340 mrad|
|Maximum sample speed||4 size distributions per second (standard)|
|Temperature range||-10 to 45 °C|
|Temperature resolution||0.01 °C|
|Pressure range||0 to 300 m|
|Pressure resolution||8 cm|
Further details can be found in the manufacturer's manual.
Prince Madog Cruise PD09_08 CTD Processing
A total of 17 CTD casts were performed during the cruise throughout Liverpool Bay. Rosette bottles were fired throughout the water column on the upcast of most profiles. Independent temperature data were recorded at the time of each bottle firing. Data were measured at 24 Hz, averaged to 1 Hz by the deck unit and logged onto a PC running SEASAVE, Sea-Bird's data acquisition software. The raw Sea-Bird data, configuration and bottle files were supplied to BODC for further processing.
BODC post-processing and screening
The raw CTD files were processed through the Sea-Bird SBE Data Processing software version 7.14c. Binary (.HEX) files were converted to engineering units and ASCII format (.CNV) using the DATCNV program.
Sea-Bird bottle files (.BTL), with information on pressure and other logged readings at the time of bottle firing, were also generated during the data conversion process.
Sea-Bird software program ALIGN CTD was run to advance conductivity by 0 s and oxygen by 3 s (within the typical range given in the Sea-Bird manual). No adjustment was made to the temperature channel as the fast sensor response time renders this unnecessary, according to the Sea-Bird literature.
To compensate for conductivity cell thermal mass effects, the data files were run through CELLTM, using alpha = 0.03, 1/beta = 7, typical values for this CTD model given in the Sea-Bird literature. After running WILD EDIT, FILTER was run on the pressure channel using the recommended time filter of 0.15 s. Next, a minimum CTD velocity of 0.0 m s-1 was used for LOOP EDIT in order to exclude scans where the CTD was travelling backwards due to ship's heave. Salinity, density (Sigma-theta kg m-3) and oxygen concentration (ml l-1) were then calculated and added to the output files using the DERIVE program.
The data were converted from ASCII format into BODC internal format (QXF) using BODC transfer function 357. The following table shows how the variables within the ASCII files were mapped to appropriate BODC parameter codes:
Originator's Parameter Name Units Description BODC Parameter Code Units Comments Pressure, Digiquartz dbar CTD pressure PRESPR01 dbar - Oxygen, Beckman/YSI ml l-1 Dissolved oxygen concentration from Beckmann probe DOXYPR01 µmol l-1 ml l-1 * 44.66 Salinity - Practical salinity of the water body by CTD PSALCU01 - Not banked by BODC. Data are un-calibrated. Used as source data for PSALCC01 Temperature [ITS-90] °C Temperature of water column by CTD TEMPCU01 °C Not banked by BODC. Data are un-calibrated. Used as source data for TEMPCC01 Voltage 2 Un-adjusted volts Voltage from CTD PAR Sensor LVLTLD01 Un-adjusted volts Not banked by BODC. These data are used as source data for the calculation of IRRDUV01. Voltage 3 Un-adjusted volts Beam transmissometer voltage TVLTCR01 Un-adjusted volts Not banked by BODC. These data are used as source data for the calculation of ATTNMR01. Voltage 4 Un-adjusted volts Voltage from CTD SCUFA Turner fluorometer FVLTWS01 Un-adjusted volts - Voltage 6 Un-adjusted volts LISST scatterometer voltage output NVLTLS01 Un-adjusted volts - Voltage 7 Un-adjusted volts LISST transmissometer voltage output TVLTZR01 Un-adjusted volts - - - Potential temperature POTMCV01 °C Generated by BODC using UNESCO Report 38 (1981) algorithm with parameters PSALCC01 and TEMPCC01 - - Sigma-theta SIGTPR01 kg m-3 Generated by BODC using the Fofonoff and Millard (1982) algorithm - - PAR IRRDUV01 µE m-2 s-1 Generated by BODC from calibration of LVLTLD01 - - Beam Attenuation ATTNMR01 m-1 Generated by BODC from calibration of TVLTCR01 - - Salinity PSALCC01 - Generated by BODC from calibration of PSALCU01 - - Temperature TEMPCC01 °C Generated by BODC from calibration of TEMPCU01 - - Oxygen saturation OXYSBB01 % Generated by BODC during transfer using the Benson and Krause (1984) algorithm.
Benson, B.B. and Krause, D., 1984. The concentration and isotopic fractionation of oxygen dissolved in freshwater and seawater in equilibrium with the atmosphere. Limnol. Oceanogr., 29(3), 620-632
Fofonoff, N.P. and Millard, R.C., 1983. Algorithms for computations of fundamental properties of seawater. UNESCO Technical Papers in Marine Science No. 44, 53pp.
UNESCO, 1981. Background papers and supporting data on the International Equation of State of Seawater 1980. UNESCO Technical Papers in Marine Science No. 38, 192pp
Reformatted CTD data were transferred onto a graphics work station for visualisation using the in-house editor EDSERPLO. Downcasts and upcasts were differentiated and the limits manually flagged. No data values were edited or deleted. Flagging was achieved by modification of the associated quality control flag to 'M' for suspect values and 'N' for nulls.
Once quality control screening was complete, the CTD downcasts were banked. Finally, the data were binned against pressure at 0.5 dbar increments.
16 independent salinity samples, obtained from the CTD rosette, were used to calibrate the CTD. Four data points were identified as outliers and removed from the analysis. The offset between CTD salinity and independent salinity samples was found. A regression analysis comparing the offset and independent salinity values did not show a relationship to be significant at 95% confidence. A calibration equation was derived from the mean offset as follows, based on 12 observations: calibrated salinity = CTD salinity - 0.01453. The RMS error is 0.00118743. The standard deviation for this dataset is 0.01240.
53 independent temperature values were compared to pressure and CTD temperature. Four data points were identified as outliers and were removed from the analysis. The temperature offset (SBE-35 temperature - CTD temperature) was found, using regression analysis, not to be significantly related to SBE-35 temperature at the 95% confidence level. The mean offset is -0.001323 °C. The standard deviation for this dataset is 0.002907 °C. This is at the lowest level of accuracy for both the SBE-35 and Sea-Bird 911plus CTD (+/- 0.001 °C). Therefore, there was no adjustment to the CTD temperature resulting from the application of manufacturer's coefficients during initial processing.
There were no casts where the CTD pressure was logging in air. No adjustments were made to the values resulting from application of manufacturer's coefficients during the intial processing.
Coefficients M and B were calculated, allowing calibration of the transmissometer with air readings taken during the cruise. M and B are calculated according to SBE Application Note No. 7:
M = (Tw/W0)*(A0-Y0)/(A1-Y1) B= -M*Y1
Where Tw is the percent transmission for pure water for the instrument (92.98%); W0 is the voltage output in pure water (4.649 volts); A0 is the manufacturer's air voltage (4.661 volts); Y0 is the manufacturer's blocked path voltage (0.000 volts); A1 is the cruise maximum air voltage (4.5006 volts); Y1 is the current blocked path voltage (0.00 volts). For this cruise, M and B were calculated to be 20.7127 and 0, respectively.
M and B are then inserted into the following equations (from SBE Application Note No. 7) to obtain calibrated beam attenuation:
Light transmission [%] = (M * voltage output) + B Beam attenuation coefficient c = - (1/z) * ln (light transmission [decimal])
M and B are the calibration coefficients, z is the transmissometer path length (0.2 m), light transmission[decimal] is light transmission [%] divided by 100, c = beam attenuation (m-1)
The data are currently un-calibrated.
LISST transmission and scattering
The data are currently supplied as voltages due to concerns about the observed variability in the clean water readings over time. With reliable clean water readings, the voltages can be calibrated to give optical transmission, beam attenuation, total volume concentration and Sauter mean diameter according to the following manufacturer's constants and calculations:
Optical Transmission = b = (VT-VToff)/(VTO-VToff)
Beam attenuation = -ln(b)/0.025 - units are metres-1, assumes 25mm path
Total volume concentration = TV = cal*[((VS-VSoff)/b)-(VSO-VSoff)] - units are µl l-1
Sauter mean diameter = SMD = a*[TV/(-ln(b)] - units are µm
Where, the coefficients supplied here are from clear water readings taken during the most recent manufacturer calibration (October 2006) as follows:
- VT = measured transmission output V
- VToff = transmission output offset = 0.007 V
- VTO = clear water transmission output = 2.828 V
- cal = total volume concentration calibration constant = 630
- VS = measured scattering output V
- VSoff = scattering output offset = 0.004 V
- VSO = clear water scattering output = 0.155 V
- a = Sauter mean diameter calibration constant = 0.075
Ideally the manufacturer's clear water values should be substituted by values determined by the LISST calibration cast, during which the instrument is placed in a tank of clean water. However, there is suspicion that these values may not be accurate.
The clean water transmission and scattering voltages can be seen to both increase and decrease with time, showing inconsistency in either the instrument performance or the calibration dip method. Therefore, manufacturer's values have been quoted along with values measured by the instrument during previous cruises since the last manufacturer's calibration. Users are advised to use their own discretion in deciding which coefficients to apply.
Date (UT) Cruise VT VS 2006-12-12 PD37_06 2.723 0.156 2007-02-12 PD02_07 2.74 0.154 2007-03-12 PD04_07 2.672 0.17 2007-04-15 PD06_07 2.72207 0.16728 2007-05-14 PD09_07 2.70208 0.16606 2007-06-20 PD13_07 2.47863 0.20879 2007-07-25 PD16_07 2.42979 0.21123 2007-08-28 PD20_07 2.45543 0.20757 2007-10-02 PD23_07 Not recorded Not recorded 2007-11-20 PD27_07 2.70696 0.15751 2008-01-08 PD01_08 2.68742 0.15873 2008-02-12 PD01_08 Not recorded Not recorded 2008-03-10 PD07_08 2.66545 0.15873 2008-04-15 PD09_08 2.69353 0.15873
During instrument deployment, no effort was made to avoid data collection possibly being affected by ship shadowing. The LI-COR LI-192SB sensor number 26 was calibrated from raw voltages using the CEFAS supplied equation:
PAR = 0.135278*exp(volts*3.4544)
Oceans 2025 Theme 10
Oceans 2025 is a strategic marine science programme, bringing marine researchers together to increase people's knowledge of the marine environment so that they are better able to protect it for future generations.
Theme 10: Integration of Sustained Observations in the Marine Environment spans all marine domains from the sea-shore to the global ocean, providing data and knowledge on a wide range of ecosystem properties and processes (from ocean circulation to biodiversity) that are critical to understanding Earth system behaviour and identifying change. They have been developed not merely to provide long-term data sets, but to capture extreme or episodic events, and play a key role in the initialisation and validation of models. Many of these SOs will be integrated into the newly developing UK Marine Monitoring Strategy - evolving from the Defra reports Safeguarding our Seas (2002) and Charting Progress (2005), thus contributing to the underpinning knowledge for national marine stewardship. They will also contribute to the UK GOOS Strategic Plan (IACMST, 2006) and the Global Marine Assessment.
Oceans 2025 - The NERC Marine Centres' Strategic Research Programme 2007-2012
Who funds the programme?
The Natural Environment Research Council (NERC) funds the Oceans 2025 programme, which was originally planned in the context of NERC's 2002-2007 strategy and later realigned to NERC's subsequent strategy (Next Generation Science for Planet Earth; NERC 2007).
Who is involved in the programme?
The Oceans 2025 programme was designed by and is to be implemented through seven leading UK marine centres. The marine centres work together in coordination and are also supported by cooperation and input from government bodies, universities and other partners. The seven marine centres are:
- National Oceanography Centre, Southampton (NOCS)
- Plymouth Marine Laboratory (PML)
- Marine Biological Association (MBA)
- Sir Alister Hardy Foundation for Marine Science (SAHFOS)
- Proudman Oceanographic Laboratory (POL)
- Scottish Association for Marine Science (SAMS)
- Sea Mammal Research Unit (SMRU)
Oceans2025 provides funding to three national marine facilities, which provide services to the wider UK marine community, in addition to the Oceans 2025 community. These facilities are:
- British Oceanographic Data Centre (BODC), hosted at POL
- Permanent Service for Mean Sea Level (PSMSL), hosted at POL
- Culture Collection of Algae and Protozoa (CCAP), hosted at SAMS
The NERC-run Strategic Ocean Funding Initiative (SOFI) provides additional support to the programme by funding additional research projects and studentships that closely complement the Oceans 2025 programme, primarily through universities.
What is the programme about?
Oceans 2025 sets out to address some key challenges that face the UK as a result of a changing marine environment. The research funded through the programme sets out to increase understanding of the size, nature and impacts of these changes, with the aim to:
- improve knowledge of how the seas behave, not just now but in the future;
- help assess what that might mean for the Earth system and for society;
- assist in developing sustainable solutions for the management of marine resources for future generations;
- enhance the research capabilities and facilities available for UK marine science.
In order to address these aims there are nine science themes supported by the Oceans 2025 programme:
- Climate, circulation and sea level (Theme 1)
- Marine biogeochemical cycles (Theme 2)
- Shelf and coastal processes (Theme 3)
- Biodiversity and ecosystem functioning (Theme 4)
- Continental margins and deep ocean (Theme 5)
- Sustainable marine resources (Theme 6)
- Technology development (Theme 8)
- Next generation ocean prediction (Theme 9)
- Integration of sustained observations in the marine environment (Theme 10)
In the original programme proposal there was a theme on health and human impacts (Theme 7). The elements of this Theme have subsequently been included in Themes 3 and 9.
When is the programme active?
The programme started in April 2007 with funding for 5 years.
Brief summary of the programme fieldwork/data
Programme fieldwork and data collection are to be achieved through:
- physical, biological and chemical parameters sampling throughout the North and South Atlantic during collaborative research cruises aboard NERC's research vessels RRS Discovery, RRS James Cook and RRS James Clark Ross;
- the Continuous Plankton Recorder being deployed by SAHFOS in the North Atlantic and North Pacific on 'ships of opportunity';
- physical parameters measured and relayed in near real-time by fixed moorings and ARGO floats;
- coastal and shelf sea observatory data (Liverpool Bay Coastal Observatory (LBCO) and Western Channel Observatory (WCO)) using the RV Prince Madog and RV Quest.
The data is to be fed into models for validation and future projections. Greater detail can be found in the Theme documents.
Oceans 2025 Theme 10, Sustained Observation Activity 11: Liverpool Bay and Irish Sea Coastal Observatory
Sustained, systematic observations of the ocean and continental shelf seas at appropriate time and space scales allied to numerical models are key to understanding and prediction. In shelf seas these observations address issues as fundamental as 'what is the capacity of shelf seas to absorb change?' encompassing the impacts of climate change, biological productivity and diversity, sustainable management, pollution and public health, safety at sea and extreme events. Advancing understanding of coastal processes to use and manage these resources better is challenging; important controlling processes occur over a broad range of spatial and temporal scales which cannot be simultaneously studied solely with satellite or ship-based platforms.
Considerable effort has been spent by the Proudman Oceangraphic Laboratory (POL) in the years 2001 - 2006 in setting up an integrated observational and now-cast modelling system in Liverpool Bay (see Figure), with the recent POL review stating the observatory was seen as a leader in its field and a unique 'selling' point of the laboratory. Cost benefit analysis (IACMST, 2004) shows that benefits really start to accrue after 10 years. In 2007 - 2012 exploitation of (i) the time series being acquired, (ii) the model-data synthesis and (iii) the increasingly available quantities of real-time data (e.g. river flows) can be carried out through Sustained Observation Activity (SO) 11, to provide an integrated assessment and short term forecasts of the coastal ocean state.
Overall Aims and Purpose of SO 11
- To continue and enlarge the scope of the existing coastal observatory in Liverpool Bay to routinely monitor the northern Irish Sea
- To develop the synthesis of measurements and models in the coastal ocean to optimize measurement arrays and forecast products. Driving forward shelf seas' operational oceanography with the direct objective of improving the national forecasting capability, expressed through links to the National Centre for Ocean Forecasting (NCOF)
- To exploit the long time-series of observations and model outputs to: a) identify the roles of climate and anthropogenic inputs on the coastal ocean's physical and biological functioning (including impacts of nutrient discharges, offshore renewable energy installations and fishing activity) taking into consideration the importance of events versus mean storms / waves, river discharge / variable salinity stratification / horizontal gradients; b) predict the impacts of climate change scenarios; and c) provide new insights to Irish Sea dynamics for variables either with seasonal cycles and interannual variability, or which show weak or no seasonal cycles
- To provide and maintain a 'laboratory' within which a variety of observational and model experiments can be undertaken (Oceans 2025 Themes 3, 6, 8, 9), including capture of extreme events
- Demonstrate the value of an integrated approach in assessment and forecasting
- Demonstrate the coastal observatory as a tool for marine management strategies through collaboration with the Environment Agency (EA), Department for Environment, Food and Rural Affairs (DEFRA), Joint Nature Conservation Commmittee (JNCC), English Nature (EN), Department of Agriculture and Rural Development (DARD), and Local Authorities, providing management information pertinent to policy (e.g. Water Framework Directive)
Measurement and Modelling Activities
- East Mooring Site: Bottom frame with full suite of physical measurements (high frequency Acoustic Doppler Current Profiler (ADCP), conductivity, temperature, turbidity and fluorescence), a Centre for Environment, Fisheries and Aquaculture Science (CEFAS) directional wavebuoy, and a CEFAS Smartbuoy collecting surface properties including salinity, temperature, turbidity, nutrients, irradiance and chlorophyll. All transmit data in real-time via Orbcomm. The Smartbuoy also collects daily water samples.
- West Mooring Site: Bottom frame with full suite of physical measurements (high frequency ADCP, conductivity, temperature, turbidity and fluorescence), CEFAS Smartbuoy.
- Spatial Survey: Four - six week intervals (determined by biofouling of optical sensors). Spatial surveys comprise of vertical profiles of CTD, suspended particulate material (SPM), some bed sediment sampling and surface and bed nutrients, phytoplankton, zooplankton.
- Ferry: The Birkenhead - Belfast ferry samples near surface (5 m depth) temperature, salinity, turbidity, chlorophyll, with data transmitted by Orbcomm. The route is scientifically varied passing through six completely different hydrodynamic regions, which significantly impact on their ecological function.
- Tide gauges: Real-time data are obtained from tide gauges operated by Mersey Docks and Harbour Company (MDHC) and the UK tide gauge network.
- Satellite imagery: Weekly composite satellite data, Advanced Very High Resolution Radiometer (AVHRR) sea surface temperature (SST) and ocean colour (chlorophyll and suspended sediment), are provided by the Remote Sensing Data Analysis Service (RSDAS) based at Plymouth Marine Laboratory (PML).
- HF radar: A phased array HF radar system (a 12-16MHz WERA HF radar) measuring surface currents and waves with maximum range 75km at a resolution of 4km for sea surface currents and for 2-D wave spectra.
- Meteorology station: With web camera, located on Hilbre Island at the mouth of the Dee Estuary
- Operational models: The Coastal Observatory uses Proudman Oceanographic Laboratory Coastal Ocean Modelling System (POLCOMS), which is part of Oceans 2025 Theme 9.
More detailed information on this Work Package is available at pages 32 - 35 of the official Oceans 2025 Theme 10 document: Oceans 2025 Theme 10
IACMST., 2004. The Economics of Sustained Marine Measurements. IACMST Information Document, N0.11, Southampton: IACMST, 96 pp
Proudman Oceanographic Laboratory Coastal Observatory
The Coastal Observatory was established by Proudman Oceanographic Laboratory as a coastal zone real time observing and monitoring system. The main objective is to understand a coastal sea's response both to natural forcing and to the consequences of human activity. Near real-time measurements will be integrated with coupled models into a pre-operational coastal prediction system whose results will be displayed on the World Wide Web.
The Observatory is expected to grow and evolve as resources and technology allow, all the while building up long time series. A site selection pilot study was carried out in September 2001 and the Observatory became operational in August 2002.
The site is located in Liverpool Bay and is subject to typical coastal sea processes, with strong tides, occasional large storm surges and waves, freshwater input, stable and unstable stratification, high suspended sediment concentration and biogeochemical interaction. Measurements and monitoring will focus on the impacts of storms, variations in river discharge (especially the Mersey), seasonality and blooms in Liverpool Bay.
A variety of methods will be used to obtain measurements, including:
- Moored instruments for in situ time series of currents, temperature and salinity profiles, and surface waves and meteorology. It is hoped that turbidity and chlorophyll measurements will be made at another site as the Observatory progresses;
- The Cefas Smartbuoy for surface properties such as nutrients and chlorophyll, starting late 2002;
- R.V. Prince Madog to carry out spatial surveys and service moorings;
- Instrumented ferries for near surface temperature, salinity, turbidity, chlorophyll and nutrients. The first route will be Liverpool to Douglas, Isle of Man, starting late 2002;
- Drifters for surface currents and properties such as temperature and salinity, starting in 2004;
- Tide gauges, with sensors for meteorology, waves, temperature and salinity, where appropriate;
- Meteorological data from Bidston Observatory and Hilbre Island, HF radar and tide gauge sites;
- Shore-based HF radar measuring waves and surface currents out to a range of 50 km, starting in 2003;
- Satellite data, with infrared for sea surface temperature and visible for chlorophyll and suspended sediment.
The partners currently involved with the project are listed below:
- Proudman Oceanographic Laboratory
- British Oceanographic Data Centre
- UK Meteorological Office
- Centre for Environment, Fisheries and Aquaculture Science
- Environment Agency
- Liverpool University and Port Erin Marine Laboratory
- Bangor University School of Ocean Sciences
- National Oceanography Centre Southampton
- Department of Agriculture and Rural Development in Northern Ireland
A summary of Coastal Observatory cruises to date on R.V. Prince Madog is given in the table below:
|Year||No. of cruises||Work summary|
|2001||1||Site selection and pilot study. 95 CTD casts.|
|2002||4||POL moorings deployed and serviced |
Cefas Waverider and SmartBuoy deployed and serviced
103 CTD casts
|2003||10||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
341 CTD/LISST casts
|2004||9||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
347 CTD/LISST casts
|2005||9||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
268 CTD/LISST casts
|2006||11||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
508 CTD/LISST casts
|2007||9||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
471 CTD/LISST casts
|2008||9||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
260 CTD/LISST casts
|2009||7||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
213 CTD/LISST casts
|2010||8||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
268 CTD/LISST casts
|2011||6||POL moorings serviced |
Cefas Waverider and SmartBuoy serviced
307 CTD/LISST casts to date, ongoing
|Principal Scientist(s)||Phil J Knight (Proudman Oceanographic Laboratory)|
|Ship||RV Prince Madog|
Complete Cruise Metadata Report is available here
Fixed Station Information
|Station Name||Coastal Observatory Site 20|
|Latitude||53° 32.13' N|
|Longitude||3° 38.39' W|
|Water depth below MSL||32.5 m|
Liverpool Bay Coastal Observatory Site 20
This station is one of 34 stations regularly visited by the Proudman Oceanographic Laboratory (POL) as part of the Liverpool Bay Coastal Observatory. During each site visit CTD profiles are collected and since March 2010 (when this became the secondary mooring site for the Coastal Observatory (also known as Site B)) moorings are deployed. The station lies within a box of mean water depth 32.5 m with the following co-ordinates:
The position of this station relative to the other POL Coastal Observatory sites can be seen from the figure below.
CTD Sampling History
|Year||Number of Visits||Total Casts per year|
The CTD instrument package for these cruises was a Sea-Bird 911plus, with beam transmissometer, fluorometer, LICOR PAR sensor, LISST-25, and oxygen sensor.
Related Fixed Station activities are detailed in Appendix 1
The following single character qualifying flags may be associated with one or more individual parameters with a data cycle:
|<||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.)|
|E||End of CTD Down/Up Cast|
|G||Non-taxonomic biological characteristic uncertainty|
|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|
|O||Improbable value - user quality control|
|0||no quality control|
|2||probably good value|
|3||probably bad value|
|6||value below detection|
|7||value in excess|
|A||value phenomenon uncertain|
|Q||value below limit of quantification|
Appendix 1: Coastal Observatory Site 20
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 Identifier||Data Category||Start date/time||Start position||Cruise|
|1013118||CTD or STD cast||2006-11-02 06:18:00||53.53267 N, 3.64367 W||RV Prince Madog PD35/06|
|979271||CTD or STD cast||2007-02-15 17:26:00||53.53317 N, 3.63867 W||RV Prince Madog PD02/07|
|937772||CTD or STD cast||2007-04-20 02:36:00||53.53767 N, 3.64383 W||RV Prince Madog PD06/07|
|942239||CTD or STD cast||2007-05-17 06:12:00||53.53283 N, 3.63633 W||RV Prince Madog PD09/07|
|942995||CTD or STD cast||2007-06-21 06:23:00||53.5365 N, 3.64517 W||RV Prince Madog PD13/07|
|943396||CTD or STD cast||2007-07-27 06:37:00||53.53367 N, 3.62917 W||RV Prince Madog PD16/07|
|943808||CTD or STD cast||2007-08-30 05:46:00||53.53267 N, 3.6425 W||RV Prince Madog PD20/07|
|945759||CTD or STD cast||2007-10-04 06:47:00||53.5315 N, 3.63883 W||RV Prince Madog PD23/07|
|946818||CTD or STD cast||2008-01-11 02:24:00||53.53517 N, 3.6435 W||RV Prince Madog PD01/08|
|947084||CTD or STD cast||2008-03-14 05:52:00||53.533 N, 3.64533 W||RV Prince Madog PD07/08|
|948235||CTD or STD cast||2008-05-15 13:00:00||53.53367 N, 3.64517 W||RV Prince Madog PD14/08|
|948585||CTD or STD cast||2008-06-25 20:03:00||53.53367 N, 3.641 W||RV Prince Madog PD19/08|
|949472||CTD or STD cast||2008-07-31 07:10:00||53.53367 N, 3.6365 W||RV Prince Madog PD23/08|
|950079||CTD or STD cast||2008-12-11 06:25:00||53.53117 N, 3.6365 W||RV Prince Madog PD37/08|
|950485||CTD or STD cast||2009-02-06 09:50:00||53.53367 N, 3.64533 W||RV Prince Madog PD02/09B|
|951464||CTD or STD cast||2009-04-02 03:57:00||53.53183 N, 3.64217 W||RV Prince Madog PD12/09|
|953803||CTD or STD cast||2009-05-13 11:24:00||53.53433 N, 3.64083 W||RV Prince Madog PD18/09|
|1023149||CTD or STD cast||2009-06-17 21:35:00||53.53167 N, 3.64483 W||RV Prince Madog PD24/09|
|1023487||CTD or STD cast||2009-08-03 14:35:00||53.53283 N, 3.6415 W||RV Prince Madog PD33/09|
|1024349||CTD or STD cast||2009-09-16 04:31:00||53.53383 N, 3.643 W||RV Prince Madog PD38/09|
|1641347||Hydrography time series at depth||2010-01-26 11:40:03||53.53783 N, 3.64033 W||RV Prince Madog PD02/10|
|1624135||Currents -subsurface Eulerian||2010-01-26 11:45:00||53.53783 N, 3.64033 W||RV Prince Madog PD02/10|
|1030380||CTD or STD cast||2010-01-26 13:08:00||53.539 N, 3.64017 W||RV Prince Madog PD02/10|
|1641384||Hydrography time series at depth||2010-01-26 13:10:00||53.53833 N, 3.64033 W||RV Prince Madog PD02/10|
|1641396||Hydrography time series at depth||2010-01-26 13:10:00||53.53833 N, 3.64033 W||RV Prince Madog PD02/10|
|1641323||Hydrography time series at depth||2010-01-26 13:10:01||53.53833 N, 3.64033 W||RV Prince Madog PD02/10|
|1641335||Hydrography time series at depth||2010-01-26 13:10:02||53.53833 N, 3.64033 W||RV Prince Madog PD02/10|
|1075687||Fluorescence or pigments||2010-01-26 14:00:00||53.5383 N, 3.6403 W||RV Prince Madog PD02/10|
|1075558||Hydrography time series at depth||2010-01-26 14:00:00||53.5383 N, 3.6403 W||RV Prince Madog PD02/10|
|1076629||Transmittance/attenuance, turbidity, or SPM conc.||2010-01-26 14:00:00||53.5383 N, 3.6403 W||RV Prince Madog PD02/10|
|1030564||CTD or STD cast||2010-01-27 06:05:00||53.54083 N, 3.63667 W||RV Prince Madog PD02/10|
|1038333||CTD or STD cast||2010-03-17 15:37:00||53.5395 N, 3.64383 W||RV Prince Madog PD05/10|
|1641440||Hydrography time series at depth||2010-03-17 16:40:03||53.53783 N, 3.64217 W||RV Prince Madog PD05/10|
|1624080||Currents -subsurface Eulerian||2010-03-17 16:45:00||53.53783 N, 3.64217 W||RV Prince Madog PD05/10|
|1641488||Hydrography time series at depth||2010-03-17 16:50:00||53.539 N, 3.64017 W||RV Prince Madog PD05/10|
|1641507||Hydrography time series at depth||2010-03-17 16:50:00||53.539 N, 3.64017 W||RV Prince Madog PD05/10|
|1641415||Hydrography time series at depth||2010-03-17 16:50:01||53.539 N, 3.64017 W||RV Prince Madog PD05/10|
|1641439||Hydrography time series at depth||2010-03-17 16:50:01||53.539 N, 3.64017 W||RV Prince Madog PD05/10|
|1075699||Fluorescence or pigments||2010-03-17 17:00:00||53.539 N, 3.6402 W||RV Prince Madog PD05/10|
|1075571||Hydrography time series at depth||2010-03-17 17:00:00||53.539 N, 3.6402 W||RV Prince Madog PD05/10|
|1076120||Transmittance/attenuance, turbidity, or SPM conc.||2010-03-17 17:00:00||53.539 N, 3.6402 W||RV Prince Madog PD05/10|
|1038345||CTD or STD cast||2010-03-17 17:03:00||53.54 N, 3.6435 W||RV Prince Madog PD05/10|
|1641556||Hydrography time series at depth||2010-04-28 17:40:03||53.5395 N, 3.64017 W||RV Prince Madog PD10/10|
|1624031||Currents -subsurface Eulerian||2010-04-28 17:45:00||53.5395 N, 3.64017 W||RV Prince Madog PD10/10|
|1075706||Fluorescence or pigments||2010-04-28 18:00:00||53.5408 N, 3.6392 W||RV Prince Madog PD10/10|
|1075583||Hydrography time series at depth||2010-04-28 18:00:00||53.5408 N, 3.6392 W||RV Prince Madog PD10/10|
|1641600||Hydrography time series at depth||2010-04-28 18:00:00||53.54083 N, 3.63917 W||RV Prince Madog PD10/10|
|1641612||Hydrography time series at depth||2010-04-28 18:00:00||53.54083 N, 3.63917 W||RV Prince Madog PD10/10|
|1076630||Transmittance/attenuance, turbidity, or SPM conc.||2010-04-28 18:00:00||53.5408 N, 3.6392 W||RV Prince Madog PD10/10|
|1641519||Hydrography time series at depth||2010-04-28 18:00:01||53.54083 N, 3.63917 W||RV Prince Madog PD10/10|
|1641532||Hydrography time series at depth||2010-04-28 18:00:01||53.54083 N, 3.63917 W||RV Prince Madog PD10/10|
|1090696||CTD or STD cast||2010-06-10 16:48:00||53.53833 N, 3.638 W||RV Prince Madog PD17/10|
|1641685||Hydrography time series at depth||2010-06-10 18:00:03||53.53917 N, 3.641 W||RV Prince Madog PD17/10|
|1624079||Currents -subsurface Eulerian||2010-06-10 18:05:00||53.53917 N, 3.641 W||RV Prince Madog PD17/10|
|1075718||Fluorescence or pigments||2010-06-10 18:30:00||53.5405 N, 3.6386 W||RV Prince Madog PD17/10|
|1075595||Hydrography time series at depth||2010-06-10 18:30:00||53.5405 N, 3.6386 W||RV Prince Madog PD17/10|
|1090703||CTD or STD cast||2010-06-10 19:05:00||53.54333 N, 3.63433 W||RV Prince Madog PD17/10|
|1090893||CTD or STD cast||2010-07-07 21:40:00||53.543 N, 3.63967 W||RV Prince Madog PD21/10|
|1090997||CTD or STD cast||2010-07-08 06:04:00||53.53617 N, 3.635 W||RV Prince Madog PD21/10|
|1641790||Hydrography time series at depth||2010-07-08 07:40:03||53.5395 N, 3.64083 W||RV Prince Madog PD21/10|
|1624043||Currents -subsurface Eulerian||2010-07-08 07:45:00||53.5395 N, 3.64083 W||RV Prince Madog PD21/10|
|1075731||Fluorescence or pigments||2010-07-08 08:00:00||53.5378 N, 3.6367 W||RV Prince Madog PD21/10|
|1075602||Hydrography time series at depth||2010-07-08 08:00:00||53.5378 N, 3.6367 W||RV Prince Madog PD21/10|
|1641833||Hydrography time series at depth||2010-07-08 08:10:00||53.53783 N, 3.63667 W||RV Prince Madog PD21/10|
|1641845||Hydrography time series at depth||2010-07-08 08:10:00||53.53783 N, 3.63667 W||RV Prince Madog PD21/10|
|1641741||Hydrography time series at depth||2010-07-08 08:10:01||53.53783 N, 3.63667 W||RV Prince Madog PD21/10|
|1641777||Hydrography time series at depth||2010-07-08 08:10:01||53.53783 N, 3.63667 W||RV Prince Madog PD21/10|
|1091000||CTD or STD cast||2010-07-08 08:25:00||53.54233 N, 3.63367 W||RV Prince Madog PD21/10|
|1112294||CTD or STD cast||2010-08-12 06:06:00||53.53467 N, 3.64383 W||RV Prince Madog PD29/10|
|1112405||CTD or STD cast||2010-08-12 18:07:00||53.539 N, 3.643 W||RV Prince Madog PD29/10|
|1641870||Hydrography time series at depth||2010-08-12 19:10:03||53.5395 N, 3.64117 W||RV Prince Madog PD29/10|
|1112417||CTD or STD cast||2010-08-12 19:11:00||53.53667 N, 3.6385 W||RV Prince Madog PD29/10|
|1623967||Currents -subsurface Eulerian||2010-08-12 19:15:00||53.5395 N, 3.64117 W||RV Prince Madog PD29/10|
|1114160||CTD or STD cast||2010-09-29 04:05:00||53.5315 N, 3.64317 W||RV Prince Madog PD36/10|
|1114196||CTD or STD cast||2010-09-29 07:03:00||53.541 N, 3.64433 W||RV Prince Madog PD36/10|
|1641962||Hydrography time series at depth||2010-09-29 07:50:03||53.54017 N, 3.64167 W||RV Prince Madog PD36/10|
|1623851||Currents -subsurface Eulerian||2010-09-29 07:55:00||53.54017 N, 3.64167 W||RV Prince Madog PD36/10|
|1075743||Fluorescence or pigments||2010-09-29 08:30:00||53.5405 N, 3.6363 W||RV Prince Madog PD36/10|
|1075614||Hydrography time series at depth||2010-09-29 08:30:00||53.5405 N, 3.6363 W||RV Prince Madog PD36/10|
|1641998||Hydrography time series at depth||2010-09-29 08:30:00||53.5405 N, 3.63633 W||RV Prince Madog PD36/10|
|1642001||Hydrography time series at depth||2010-09-29 08:30:00||53.5405 N, 3.63633 W||RV Prince Madog PD36/10|
|1076132||Transmittance/attenuance, turbidity, or SPM conc.||2010-09-29 08:30:00||53.5405 N, 3.6363 W||RV Prince Madog PD36/10|
|1641913||Hydrography time series at depth||2010-09-29 08:30:01||53.5405 N, 3.63633 W||RV Prince Madog PD36/10|
|1641937||Hydrography time series at depth||2010-09-29 08:30:01||53.5405 N, 3.63633 W||RV Prince Madog PD36/10|
|1114203||CTD or STD cast||2010-09-29 08:51:00||53.54033 N, 3.63717 W||RV Prince Madog PD36/10|
|1642062||Hydrography time series at depth||2010-12-07 15:20:03||53.5405 N, 3.64283 W||RV Prince Madog PD49/10|
|1623666||Currents -subsurface Eulerian||2010-12-07 15:25:00||53.5405 N, 3.64283 W||RV Prince Madog PD49/10|
|1642098||Hydrography time series at depth||2010-12-07 16:10:00||53.537 N, 3.638 W||RV Prince Madog PD49/10|
|1642105||Hydrography time series at depth||2010-12-07 16:10:00||53.537 N, 3.638 W||RV Prince Madog PD49/10|
|1642117||Hydrography time series at depth||2010-12-07 16:10:00||53.537 N, 3.638 W||RV Prince Madog PD49/10|
|1642013||Hydrography time series at depth||2010-12-07 16:10:01||53.537 N, 3.638 W||RV Prince Madog PD49/10|
|1642025||Hydrography time series at depth||2010-12-07 16:10:01||53.537 N, 3.638 W||RV Prince Madog PD49/10|
|1075755||Fluorescence or pigments||2010-12-07 16:30:00||53.5405 N, 3.6428 W||RV Prince Madog PD49/10|
|1075626||Hydrography time series at depth||2010-12-07 16:30:00||53.5405 N, 3.6428 W||RV Prince Madog PD49/10|
|1140953||CTD or STD cast||2010-12-07 16:46:00||53.53667 N, 3.646 W||RV Prince Madog PD49/10|
|1141016||CTD or STD cast||2010-12-07 21:10:00||53.534 N, 3.63433 W||RV Prince Madog PD49/10|
|1149067||CTD or STD cast||2011-01-13 08:03:00||53.54033 N, 3.64283 W||RV Prince Madog PD01/11|
|1149079||CTD or STD cast||2011-01-13 09:10:00||53.543 N, 3.6415 W||RV Prince Madog PD01/11|
|1642178||Hydrography time series at depth||2011-01-13 09:10:03||53.54033 N, 3.64383 W||RV Prince Madog PD01/11|
|1623771||Currents -subsurface Eulerian||2011-01-13 09:14:59||53.54033 N, 3.64383 W||RV Prince Madog PD01/11|
|1642209||Hydrography time series at depth||2011-01-13 15:10:00||53.54017 N, 3.63983 W||RV Prince Madog PD01/11|
|1642210||Hydrography time series at depth||2011-01-13 15:10:00||53.54017 N, 3.63983 W||RV Prince Madog PD01/11|
|1642222||Hydrography time series at depth||2011-01-13 15:10:00||53.54017 N, 3.63983 W||RV Prince Madog PD01/11|
|1642130||Hydrography time series at depth||2011-01-13 15:10:01||53.54017 N, 3.63983 W||RV Prince Madog PD01/11|
|1642142||Hydrography time series at depth||2011-01-13 15:10:01||53.54017 N, 3.63983 W||RV Prince Madog PD01/11|
|1149159||CTD or STD cast||2011-01-13 15:32:00||53.53833 N, 3.637 W||RV Prince Madog PD01/11|
|1149946||CTD or STD cast||2011-03-17 08:59:00||53.53833 N, 3.63967 W||RV Prince Madog PD07/11|
|1150112||CTD or STD cast||2011-03-18 10:34:00||53.542 N, 3.64017 W||RV Prince Madog PD07/11|
|1642295||Hydrography time series at depth||2011-03-18 11:20:03||53.53983 N, 3.64233 W||RV Prince Madog PD07/11|
|1624111||Currents -subsurface Eulerian||2011-03-18 11:25:00||53.53983 N, 3.64233 W||RV Prince Madog PD07/11|
|1642326||Hydrography time series at depth||2011-03-18 11:40:00||53.5385 N, 3.64017 W||RV Prince Madog PD07/11|
|1642338||Hydrography time series at depth||2011-03-18 11:40:00||53.5385 N, 3.64017 W||RV Prince Madog PD07/11|
|1642351||Hydrography time series at depth||2011-03-18 11:40:00||53.5385 N, 3.64017 W||RV Prince Madog PD07/11|
|1642246||Hydrography time series at depth||2011-03-18 11:40:01||53.5385 N, 3.64017 W||RV Prince Madog PD07/11|
|1642271||Hydrography time series at depth||2011-03-18 11:40:01||53.5385 N, 3.64017 W||RV Prince Madog PD07/11|
|1150124||CTD or STD cast||2011-03-18 11:55:00||53.54067 N, 3.64167 W||RV Prince Madog PD07/11|
|1117735||CTD or STD cast||2011-04-20 11:12:00||53.5395 N, 3.63167 W||RV Prince Madog PD11/11|
|1117747||CTD or STD cast||2011-04-20 12:05:00||53.53883 N, 3.63783 W||RV Prince Madog PD11/11|
|1118683||CTD or STD cast||2011-06-07 00:35:00||53.53917 N, 3.63383 W||RV Prince Madog PD43/11|