Metadata Report for BODC Series Reference Number 1748986
Metadata Summary
Problem Reports
Data Access Policy
Narrative Documents
Project Information
Data Activity or Cruise Information
Fixed Station Information
BODC Quality Flags
SeaDataNet Quality Flags
Metadata Summary
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Problem Reports
No Problem Report Found in the Database
RRS Discovery DY029 surface hydrography quality control report
General comments
The non-toxic, pumped seawater supply was not switched on until 14:35 on 01/04/2015, therefore around two hours after the ship had departed at the beginning of the cruise. All sea surface hydrography sensors did not stabilise until 16:10 that same day; data were therefore flagged as suspect prior to this time (BODC assessment). In addition, suspicious data in all sea surface hydrography sensors were spotted between 16:10 on 01/04/2015 and 08:22 on 02/04/2015; the technical cruise report submitted to BODC noted that air bubbles had been identified in the underway pumped system during this period. These data were therefore flagged (BODC assessment).
All underway water sampling systems were shut off on 13/04/2015 between 05:30 and 07:20 during a mid-cruise boat transfer near Falmouth; all corresponding surface hydrography data were flagged by BODC. The underway system was stopped again shortly afterwards, to clean the fluorometer and transmissometer sensors, and the data do not regain stability until 10:44 that day. All data were therefore flagged by BODC over this subsequent period too.
On 16/04/2015 between 14:56 and 15:32, large spikes in all channels were noticed. The technical cruise report notes that the non-toxic supply was shut off, and the SBE38 swapped with the spare sensor. All surface hydrography data over this period were flagged (BODC assessment).
Several small spikes and high levels of noise were recorded in conductivity and both temperature channels between 24/04/2015 and 25/04/2015. This was noted by the technicians, whom attempted to fix the problem by switching Surfmet off and on between 15:41 and 15:45 on 25/04/2015. BODC only flagged the most obvious spikes within the time frame Surfmet was being re-booted.
Housing temperature, conductivity and salinity
The SBE 45 parameters were particularly noisy and spiky throughout the length of the cruise. These problems were acknowledged by the technicians; however the cause could not be immediately identified and resolved. A quality report was issued following cruise DY040, where the same instrument was used and the causes to the problems were finally identified to be:
- Air bubbles in the TSG system. Despite the presence of a de-bubbler, bubbles collected upstream the TSG system, resulting in noisy readings, particularly in salinity.
- Engineers carried out regular switching of the pump every about 12 hours. This routine was found to cause stagnant water to flow through the underway instrumentation, and cause temperature and conductivity spikes at this frequency.
Spikes and particularly noisy data associated with these known issues were identified and flagged accordingly, as well as drifts in data matching times of decreasing flow rate noted in the technical cruise report (BODC assessment).
Transmittance was very noisy throughout the whole series. Extensive flagging had to be carried out to clean the record (BODC assessment).
Large spikes were recorded in fluorescence data for most of the duration of the cruise. Several cycles were flagged (BODC assessment).
Salinity appeared very noisy throughout the whole length of the cruise, with several small spikes. All spikes greater than 0.04 were flagged by BODC, together with the corresponding conductivity data cycles.
Temperature, salinity, transmittance and fluorescence data were flagged throughout most of 20/04/2015, due to spikes and higher levels of noise (BODC assessment). The SBE 45 was removed and re-installed following these malfunctions; the technical cruise report notes that following this procedure however, the noise in temperature increased by an order of magnitude and remained such until the end of the cruise. This decrease in data quality affected the calculated salinity measurements, which also became noisier and at a higher frequency than the temperature data itself. Some tests were run by the technicians, whom concluded that the best way to remove the noisy data was to apply a discrete time low-pass filter to temperature data, and re-calculate salinity from the filtered values.
Sea surface temperature
Occasional noisy data, spikes and drifts in raw inlet temperature data were flagged accordingly (BODC assessment).
Data Access Policy
Open Data supplied by Natural Environment Research Council (NERC)
You must always use the following attribution statement to acknowledge the source of the information: "Contains data supplied by Natural Environment Research Council."
Narrative Documents
SeaBird Digital Oceanographic Thermometer SBE38
The SBE38 is an ultra-stable thermistor that can be integrated as a remote temperature sensor with an SBE21 Thermosalinograph or an SBE 45 Micro TSG, or as a secondary temperature sensor with an SBE 16 plus, 16plus-IM, 16plus V2, 16plus-IM V2 or 19plus V2 SEACAT CTD.
Temperature is determined by applying an AC excitation to reference resistances and an ultra-stable aged thermistor. The reference resistor is a hermetically sealed VISHAY. AC excitation and ratiometric comparison using a common processing channel removes measurement errors due to parasitic thermocouples, offset voltages, leakage currents and gain errors.
The SBE38 can operate in polled sampling, where it takes one sample and transmits the data, or in continuous sampling.
Specifications
Depth rating | up to 10500 m |
Temperature range | -5 to 35°C |
Initial accuracy | ± 0.001°C |
Resolution | 0.00025°C |
Stability | 0.001°C in 6 months |
Response time | 500 ms |
Self-heating error | < 200 µK |
Further details can be found in the manufacturer's specification sheet.
WET Labs WETStar Fluorometers
WET Labs WETStar fluorometers are miniature flow-through fluorometers, designed to measure relative concentrations of chlorophyll, CDOM, uranine, rhodamineWT dye, or phycoerythrin pigment in a sample of water. The sample is pumped through a quartz tube, and excited by a light source tuned to the fluorescence characteristics of the object substance. A photodiode detector measures the portion of the excitation energy that is emitted as fluorescence.
Specifications
By model:
Chlorophyll WETStar | CDOM WETStar | Uranine WETStar | Rhodamine WETStar | Phycoerythrin WETStar | |
---|---|---|---|---|---|
Excitation wavelength | 460 nm | 370 nm | 485 nm | 470 nm | 525 nm |
Emission wavelength | 695 nm | 460 nm | 530 nm | 590 nm | 575 nm |
Sensitivity | 0.03 µg l-1 | 0.100 ppb QSD | 1 µg l-1 | - | - |
Range | 0.03-75 µg l-1 | 0-100 ppb; 0-250 ppb | 0-4000 µg l-1 | - | - |
All models:
Temperature range | 0-30°C |
---|---|
Depth rating | 600 m |
Response time | 0.17 s analogue; 0.125 s digital |
Output | 0-5 VDC analogue; 0-4095 counts digital |
Further details can be found in the manufacturer's specification sheet, and in the instrument manual.
WETLabs C-Star transmissometer
This instrument is designed to measure beam transmittance by submersion or with an optional flow tube for pumped applications. It can be used in profiles, moorings or as part of an underway system.
Two models are available, a 25 cm pathlength, which can be built in aluminum or co-polymer, and a 10 cm pathlength with a plastic housing. Both have an analog output, but a digital model is also available.
This instrument has been updated to provide a high resolution RS232 data output, while maintaining the same design and characteristics.
Specifications
Pathlength | 10 or 25 cm |
Wavelength | 370, 470, 530 or 660 nm |
Bandwidth | ~ 20 nm for wavelengths of 470, 530 and 660 nm ~ 10 to 12 nm for a wavelength of 370 nm |
Temperature error | 0.02 % full scale °C-1 |
Temperature range | 0 to 30°C |
Rated depth | 600 m (plastic housing) 6000 m (aluminum housing) |
Further details are available in the manufacturer's specification sheet or user guide.
RRS Discovery DY029 surface hydrographic instrumentation
The sea surface hydrographical suite of sensors was fed by the pumped-seawater, non-toxic supply. The seawater intake was located approximately 6 m below the sea surface.
The following surface hydrology sensors were fitted:
Manufacturer | Model | Serial number | Last manufacturer's calibration date | Comments |
WETLabs | WETStar | WS3S-247 | 29/07/2014 | |
WETLabs | C-Star | CST-112R | 26/06/2014 | |
Sea-Bird | SBE38 | 3853440-0475 | 22/07/2014 | Used from start of cruise until 15:20 16/04/2015. Calibration applied by sensor firmware |
Sea-Bird | SBE38 | 3853440-0416 | 22/07/2014 | Used from 15:20 16/04/2015 until end of cruise. Calibration applied by sensor firmware |
Sea-Bird | SBE45 | 4548881-0229 | 14/01/2014 | Calibration applied by sensor firmware |
SeaBird MicroTSG Thermosalinograph SBE 45
The SBE45 MicroTSG is an externally powered instrument designed for shipboard measurement of temperature and conductivity of pumped near-surface water samples. The instrument can also compute salinity and sound velocity internally.
The MicroTSG comprises a platinum-electrode glass conductivity cell and a stable, pressure-protected thermistor temperature sensor. It also contains an RS-232 port for appending the output of a remote temperature sensor, allowing for direct measurement of sea surface temperature.
The instrument can operate in Polled, Autonomous and Serial Line Sync sampling modes:
- Polled sampling: the instrument takes one sample on command
- Autonomous sampling: the instrument samples at preprogrammed intervals and does not enter quiescence (sleep) state between samples
- Serial Line Sync: a pulse on the serial line causes the instrument to wake up, sample and re-enter quiescent state automatically
Specifications
Conductivity | Temperature | Salinity | |
---|---|---|---|
Range | 0 to 7 Sm-1 | -5 to 35°C | |
Initial accuracy | 0.0003 Sm-1 | 0.002°C | 0.005 (typical) |
Resolution | 0.00001 Sm-1 | 0.0001°C | 0.0002 (typical) |
Typical stability (per month) | 0.0003 Sm-1 | 0.0002°C | 0.003 (typical) |
Further details can be found in the manufacturer's specification sheet.
RRS Discovery DY029 surface hydrography data processing procedures
Originator's Data Processing
The data were logged directly by the TECHSAS (TECHnical and Scientific sensors Acquisition System) system into NetCDF files and UKORS RVS Level-C format. The data in the UKORS RVS format were submitted to BODC for post-cruise processing and data banking.
Files delivered to BODC
Filename | Content description | Format | Interval | Start date/time (UTC) | End date/time (UTC) | Comments |
sbe45 | SBE45 and SBE38 data only | UKORS | <1 - 1 sec approx. | 31/3/2015 14:37:19 | 29/4/2015 14:47:29 | SBE45 and SBE38 data which is not delayed in time |
surfmet | All raw surfmet data | UKORS | <1 - 1 sec approx. | 31/3/2015 14:37:20 | 29/4/2015 14:47:29 | All sea surface hydrography data but the SBE45 and SBE38 may be delayed in time. |
BODC Data Processing
Reformatting
sbe45 and surfmet files contained sea surface hydrography data, and were thus selected for transfer into BODC format. The TSG (housing temperature, housing conductivity and salinity) and sea surface temperature data from the raw water inlet were sourced from the sbe45 data stream since the same variables in surfmet may be delayed in time. Underway data files were merged into a single file using time as the primary linking key, and reformatted to NetCDF using BODC standard data banking procedures. The time span of the file is 01/04/2015 11:00:19 to 29/04/2015 14:47:19, with a sampling interval of 30 seconds.
The following table shows how the variables within the files were mapped to appropriate BODC parameter codes:
sbe45
Originator's variable | Originator's units | Description | BODC Code | BODC Units | Unit conversion | Comments |
temp_h | °C | TSG housing temperature | TMESSG01 | °C | ||
cond | S m-1 | TSG housing conductivity | CNDCSG01 | S m-1 | ||
salin | PSU | Practical salinity | PSALSU01 | dimensionless | Calculated in real time by UNESCO 1983 algorithm | |
sndspeed | m s-1 | Speed of sound | Not transferred. Derived by BODC | |||
temp_r | °C | Sea surface temperature | TEMPHU01 | °C |
surfmet
Originator's variable | Originator's units | Description | BODC Code | BODC Units | Unit conversion | Comments |
press | hPa | Air pressure | ||||
speed | m s-1 | Relative wind speed | ||||
direct | Degrees | Relative wind direction | ||||
airtemp | °C | Air temperature | ||||
humidity | % | Relative humidity of the air | ||||
ppar | volt x 105 | Port-side PAR sensor | ||||
spar | volt x 105 | Starboard-side PAR sensor | ||||
ptir | volt x 105 | Port-side TIR sensor | ||||
stir | volt x 105 | Starboard-side TIR sensor | ||||
temp_h | °C | SBE45 housing water temperature | ||||
temp_r | °C | SBE38 remote temperature at raw inlet | ||||
cond | S m-1 | SBE45 housing water conductivity | ||||
fluo | volt | Instrument output from fluorometer | FVLTWS01 | volt | ||
trans | volt | Instrument output from transmissometer | TVLTDR01 | volt |
Screening
All reformatted data were inspected on a graphics workstation, and any spikes or dubious data were flagged. The workstation software also allowed comparative screening checks between channels, carried out by overlaying data channels.
Data processing, correction and calibration
Chlorophyll-a
The following manufacturer's calibration was applied to the fluorometer to derive chlorophyll-a concentration:
Chl. a (mg m-3) = (raw - a) x b |
Which includes the raw chlorophyll fluorescence data (raw), the clean water output coefficient (a) = 0.047 V, the scale factor (b) = 6.1 µg V-1. Note: 1 µg L-1= 1 mg m-3.
Transmittance and beam attenuation
No air and dark calibration values were measured on the ship, therefore the manufacturer's calibration equation including the factory's readings only was used to derive light transmission (%) from raw transmittance voltage outputs:
light transmission (%) = 100 x (raw - Vdark) / (Vref - Vdark) |
Which includes the raw transmittance data (raw), the manufacturer's dark voltage reading (Vdark) = 0.058 V, and the manufacturer's voltage output in pure water (Vref) = 4.623 V.
The following manufacturer's equation was applied to derive beam attenuation from raw transmittance voltage output:
Attenuance (m-1) = (-1/a) x ln(Tr) |
Which includes the path length (a) = 0.25 m, and the decimal transmittance (Tr) = light transmission (%) / 100.
Salinity
Salinity was calibrated against independent bottle samples. Bottle salinities and corresponding underway data values were extracted using standard BODC procedures. Only 49 out of the 65 discrete underway salinity samples collected during the cruise were included in the calculation of the calibration equation. The remaining 16 bottle salinity samples were excluded because either their corresponding thermosalinograph data cycle had been flagged as suspect, or the bottle salinity value was deemed suspiciously high after BODC assessment and subsequently flagged as such, or they resulted to be outliers in regression analysis. No trends with time or bottle salinity were found, therefore underway salinity was calibrated with a mean offset as follows:
new_salinity (PSU) = old_salinity (PSU) + 0.0205 (±0.0035 S.D., n = 49, P < 0.05) |
Where 'new_salinity' is the calibrated salinity, 'old_salinity' is the thermosalinograph salinity.
Sea surface temperature (SST)
SST was calibrated against the primary CTD temperature sensor. CTD temperature (interpolated to 6 m depth) and corresponding SST data values were extracted using standard BODC procedures (n=108). Twenty sample points were removed as they resulted to be outliers from regression analysis. There is a significant but weak trend with time, therefore underway raw inlet temperature was calibrated with a mean offset instead, as follows:
new_temperature (°C) = old_temperature (°C) - 0.1753 (±0.0604 S.D., n = 108, P < 0.05) |
Where 'new_temperature' is the calibrated underway raw inlet temperature, 'old_temperature' is the raw inlet underway temperature.
Project Information
Shelf Sea Biogeochemistry (SSB) Programme
Shelf Sea Biogeochemistry (SSB) is a £10.5 million, six-year (2011-2017) research programme, jointly funded by the Natural Environment Research Council (NERC) and the Department for Environment, Food and Rural Affairs (DEFRA). The aim of the research is to reduce the uncertainty in our understanding of nutrient and carbon cycling within the shelf seas, and of their role in global biogeochemical cycles. SSB will also provide effective policy advice and make a significant contribution to the Living with Environmental Change programme.
Background
The Shelf Sea Biogeochemistry research programme directly relates to the delivery of the NERC Earth system science theme and aims to provide evidence that supports a number of marine policy areas and statutory requirements, such as the Marine Strategy Framework Directive and Marine and Climate Acts.
The shelf seas are highly productive compared to the open ocean, a productivity that underpins more than 90 per cent of global fisheries. Their importance to society extends beyond food production to include issues of biodiversity, carbon cycling and storage, waste disposal, nutrient cycling, recreation and renewable energy resources.
The shelf seas have been estimated to be the most valuable biome on Earth, but they are under considerable stress, as a result of anthropogenic nutrient loading, overfishing, habitat disturbance, climate change and other impacts.
However, even within the relatively well-studied European shelf seas, fundamental biogeochemical processes are poorly understood. For example: the role of shelf seas in carbon storage; in the global cycles of key nutrients (nitrogen, phosphorus, silicon and iron); and in determining primary and secondary production, and thereby underpinning the future delivery of many other ecosystem services.
Improved knowledge of such factors is not only required by marine policymakers; it also has the potential to increase the quality and cost-effectiveness of management decisions at the local, national and international levels under conditions of climate change.
The Shelf Sea Biogeochemistry research programme will take a holistic approach to the cycling of nutrients and carbon and the controls on primary and secondary production in UK and European shelf seas, to increase understanding of these processes and their role in wider biogeochemical cycles. It will thereby significantly improve predictive marine biogeochemical and ecosystem models over a range of scales.
The scope of the programme includes exchanges with the open ocean (transport on and off the shelf to a depth of around 500m), together with cycling, storage and release processes on the shelf slope, and air-sea exchange of greenhouse gases (carbon dioxide and nitrous oxide).
Further details are available on the SSB website.
Participants
15 different organisations are directly involved in research for SSB. These institutions are
- Centre for Environment, Fisheries and Aquaculture Science (Cefas)
- Meteorological Office
- National Oceanography Centre (NOC)
- Plymouth Marine Laboratory (PML)
- Scottish Association for Marine Science (SAMS) / Scottish Marine Institute (SMI)
- University of Aberdeen
- University of Bangor
- University of East Anglia (UEA)
- University of Edinburgh
- University of Essex
- University of Liverpool
- University of Oxford
- Plymouth University
- University of Portsmouth
- University of Southampton
In addition, there are third party institutions carrying out sampling work for SSB, but who are not involved in the programme itself. These are:
- The Agri-Food and Biosciences Institute (AFBI)
- Irish Marine Institute (MI)
- Marine Science Scotland (MSS)
Research details
Overall, five Work Packages have been funded by the SSB programme. These are described in brief below:
-
Work Package 1: Carbon and Nutrient Dynamics and Fluxes over Shelf Systems (CaNDyFloSS).
This work package aims to perform a comprehensive study of the cycling of nutrients and carbon throughout the water column over the whole north-west European shelf. This will allow the fluxes of nutrients and carbon between the shelf and the deep ocean and atmosphere to be quantified, establishing the role of the north-west European continental shelf in the global carbon cycle. -
Work Package 2: Biogeochemistry, macronutrient and carbon cycling in the benthic layer.
This work package aims are to map the sensitivity and status of seabed habitats, based on physical conditions, ecological community structure and the size and dynamics of the nitrogen and carbon pools found there. This information will be used, in conjunction with some laboratory-based work, to generate an understanding of the potential impacts on the benthic community as a result of changing environmental conditions, such as rising CO2 levels. -
Work Package 3: The supply of iron from shelf sediments to the ocean.
The research for this work package addresses the question of how currents, tides, weather and marine chemistry allow new iron to be transported away from the shallow shelf waters around the United Kingdom (UK), to the nearby open ocean. This will ultimately allow an improved understanding of how the transport of iron in shelf waters and shelf sediments influences phytoplankton growth in open oceans. This in turn improves the understanding of carbon dioxide uptake by phytoplankton. -
Work Package 4: Integrative modelling for Shelf Seas Biogeochemistry.
The aim of this work package is the development of a new shelf seas biogeochemical model system, coupled to a state of the art physical model, that is capable of predicting regional impacts of environmental change of timescales from days to decades. It is envisaged that the combination of predictive tools and new knowledge developed in this work package will underpin development and implementation of marine policy and marine forecasting systems. - Work Package 5: Data synthesis and management of marine and coastal carbon (DSMMAC).
This work package is funded by Defra and is also known by the name 'Blue Carbon'. The aim is to provide a process-based, quantitative assessment of the role of UK coastal waters and shelf seas in carbon storage and release, using existing data and understanding, and also emerging results from SSB fieldwork, experiments and modelling. Particular emphasis will be given to processes that may be influenced by human activities, and hence the opportunity for management interventions to enhance carbon sequestration.
Fieldwork and data collection
The campaign consists of the core cruises in the table below, to the marine shelf (and shelf-edge) of the Celtic Sea on board the NERC research vessels RRS Discovery and RRS James Cook. These cruises will focus on the physics and biogeochemistry of the benthic and pelagic zones of the water column, primarily around four main sampling sites in this area.
Cruise identifier | Research ship | Cruise dates | Work packages |
---|---|---|---|
DY008 | RRS Discovery | March 2014 | WP 2 and WP 3 |
JC105 | RRS James Cook | June 2014 | WP 1, WP 2 and WP 3 |
DY026 | RRS Discovery | August 2014 | WP1, WP 2 and WP 3 |
DY018 | RRS Discovery | November - December 2014 | WP 1 and WP 3 |
DY021 (also known as DY008b) | RRS Discovery | March 2015 | WP 2 and WP 3 |
DY029 | RRS Discovery | April 2015 | WP 1 and WP 3 |
DY030 | RRS Discovery | May 2015 | WP 2 and WP 3 |
DY033 | RRS Discovery | July 2015 | WP 1 and WP 3 |
DY034 | RRS Discovery | August 2015 | WP 2 and WP 3 |
Core cruises will be supplemented by partner cruises led by Cefas, MI, MSS, Bangor University and AFBI, spanning the shelf seas and shelf-edges around United Kingdom and Republic of Ireland.
Activities will include coring, Conductivity Temperature and Depth (CTD) deployments, Acoustic Doppler Current Profilers (ADCP) surveys, moorings and wire-walker deployments, benthic lander observatories, autonomous gliders and submersible surveys, Marine Snow Catcher particulate matter analysis, plankton net hauls, in-situ sediment flume investigations and laboratory incubations with core and sea water samples.
Shelf Sea Biogeochemistry (SSB) Programme Work Package 1: CaNDyFloSS
Carbon and Nutrient Dynamics and Fluxes over Shelf Systems (CaNDyFloSS) is a £2.76 million component of the Natural Environment Research Council (NERC) Shelf Sea Biogeochemistry (SSB) research programme, running from 2013 to 2017. It is jointly funded by NERC and the Department for Environment, Food and Rural Affairs (DEFRA). The aim of the research is to perform a comprehensive study of the cycling of nutrients and carbon throughout the water column over the whole north-west European shelf. This will allow the fluxes of nutrients and carbon between the shelf and the deep ocean and atmosphere to be quantified, establishing the role of the north-west European continental shelf in the global carbon cycle.
Background
Shelf seas are the primary regions of human marine resource exploitation, including both renewable and fossil fuel energy sources, recreation, trade and food production. They provide 90% of global fish catches which form an important source of food to much of the global population. They also play an important role in the ecosystem services provided by the oceans as a whole, in particular in storing carbon away from the atmosphere.
Physical and biochemical processes in shelf seas influence the removal of CO2 from the atmosphere and the subsequent storage of carbon in the deep ocean. Biological growth draws carbon out of the water, which is then replaced by carbon in CO2 from the atmosphere. In the shelf seas this growth is supported by terrestrial and open ocean sources of nutrients, implying intimate roles for both the terrestrial biosphere and the open ocean environment in regulating shelf sea climate services. The oceans can also be a major source or sink for other greenhouse gases, including nitrous oxide (N2O), with the shallow shelf sea thought to play a key role.
The spatial extent of the submerged continental shelves varies greatly. The NW European shelf sea is one of the largest and hence is likely to play a significant role in marine biogeochemical cycling, alongside providing a useful model for other systems. However, even in this relatively well studied region, there is a lack of detailed understanding of the principal controls on the cycling of carbon and the major nutrient elements, nitrogen, phosphorus and silicon. Consequently it is also difficult to predict how the cycling of these elements and hence the carbon removal they support may be altered by ongoing and potential future global change. This work package aims to address these uncertainties through a comprehensive study of the cycling of the major nutrients and carbon throughout the water column over the NW European shelf sea system.
Further details are available on the SSB website.
Participants
9 different organisations are directly involved in research for SSB Work Package 1. These institutions are
- Centre for Environment, Fisheries and Aquaculture Science (Cefas)
- National Oceanography Centre (NOC)
- Plymouth Marine Laboratory (PML)
- Scottish Association for Marine Science (SAMS) / Scottish Marine Institute (SMI)
- University of Aberdeen
- University of Bangor
- University of East Anglia (UEA)
- University of Liverpool
- University of Southampton
In addition, there are third party institutions carrying out sampling work for SSB Work Package 1, but who are not involved in the programme itself. These are:
- The Agri-Food and Biosciences Institute (AFBI)
- Irish Marine Institute (MI)
- Marine Science Scotland (MSS)
Objectives
Two overarching objectives are defined for this Work Package.
-
Objective 1: Estimate the size of the continental shelf carbon pump over the whole north-west European shelf.
This will consist of two principal activities. (1) Over a 12 month period, observations of air-sea CO2 fluxes will be made to provide a synoptic estimate of the magnitude of carbon update by the whole shelf system. (2) Concentrations of carbon (C), nitrogen (N), phosphate (P) and silicate (Si) will be estimated in water flowing on and off the shelf. These estimates will be coupled to estimates of flow and dispersion along the shelf edge, through collaboration with the NERC Fluxes across Sloping Topography of the North East Atlantic (FASTNEt) programme to allow an observational estimate of the net off-shelf transport of C, N, P and Si. -
Objective 2: Determine the relative importance of external nutrient sources and internal biogeochemical cycling in maintaining the continental shelf pump.
Estimates of the flux of nutrients and carbon generated in Objective 1 will be used to determine the estimation of any excess of on-shelf nutrient supply, relative to that of carbon. Work Package 1 will then quantify the processes which govern internal biogeochemical cycling by measuring the uptake ratios of N, P, Si and C into phytoplankton and the element and energy balance of organic matter production by autotrophs. Potential modifications to the relative concentrations and uptake of C, N, P and Si in the thermocline and sediment food webs will also be assessed, as will the relative importance of microbial and zooplankton turnover in controlling C, N, P and Si.
Fieldwork and data collection
Data for Objective 1 will be provided using pCO2 systems aboard third party vessels and ferry boxes, along with measurements made through the FASTNEt programme and through the Work Package 1 process cruises detailed below. The third party cruises will be undertaken by Cefas, MI, MSS, University of Bangor and AFBI, spanning the shelf seas and shelf-edges around the United Kingdom and the Republic of Ireland.
The Work Package 1 process cruises will provide data for Objective 1 and Objective 2 and are listed in the table below. The study area is the marine shelf (and shelf-edge) of the Celtic Sea. Work will be carried out on board the NERC research vessels RRS Discovery and RRS James Cook. These cruises will focus on the physics and biogeochemistry of the benthic and pelagic zones of the water column, primarily around four main sampling sites in this area.
Cruise identifier | Research ship | Cruise dates | Work packages |
---|---|---|---|
JC105 | RRS James Cook | June 2014 | WP 1, WP 2 and WP 3 |
DY026 | RRS Discovery | August 2014 | WP1, WP 2 and WP 3 |
DY018 | RRS Discovery | November - December 2014 | WP 1 and WP 3 |
DY029 | RRS Discovery | April 2015 | WP 1 and WP 3 |
DY033 | RRS Discovery | July 2015 | WP 1 and WP 3 |
Activities will include Conductivity Temperature and Depth (CTD) deployments, Acoustic Doppler Current Profilers (ADCP) surveys, moorings and wire-walker deployments, autonomous gliders and submersible surveys, Marine Snow Catcher particulate matter analysis, plankton net hauls and laboratory incubations with sea water samples.
Data Activity or Cruise Information
Cruise
Cruise Name | DY029 (GApr04) |
Departure Date | 2015-04-01 |
Arrival Date | 2015-04-29 |
Principal Scientist(s) | Alex Poulton (National Oceanography Centre, Southampton) |
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 |