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No Problem Report Found in the Database
You must always use the following attribution statement to acknowledge the source of the information: "Contains data supplied by Natural Environment Research Council."
The SBE 43 is a dissolved oxygen sensor designed for marine applications. It incorporates a high-performance Clark polarographic membrane with a pump that continuously plumbs water through it, preventing algal growth and the development of anoxic conditions when the sensor is taking measurements.
Two configurations are available: SBE 43 produces a voltage output and can be incorporated with any Sea-Bird CTD that accepts input from a 0-5 volt auxiliary sensor, while the SBE 43F produces a frequency output and can be integrated with an SBE 52-MP (Moored Profiler CTD) or used for OEM applications. The specifications below are common to both.
Housing | Plastic or titanium |
Membrane | 0.5 mil- fast response, typical for profile applications 1 mil- slower response, typical for moored applications |
Depth rating | 600 m (plastic) or 7000 m (titanium) 10500 m titanium housing available on request |
Measurement range | 120% of surface saturation |
Initial accuracy | 2% of saturation |
Typical stability | 0.5% per 1000 h |
Further details can be found in the manufacturer's specification sheet.
A Sea-Bird 9plus CTD system (serial number 09P-31240-0720) used on cruise D351 for the following casts: 001, 003-006, 008-010, 018-022, 024-032, 034-038, 040-101. This was mounted on a stainless steel rosette frame, equipped with 24 20-litre Niskin bottles. The CTD was fitted with the following scientific sensors:
Sensor | Serial Number | Last calibration date | Comments |
---|---|---|---|
Digiquartz Pressure | 90573 | 20th October 2008 | - |
Primary Temperature SBE-3P | 3P-4151 | 27th February 2010 | - |
Secondary Temperature SBE-3P | 3P-4872 | 31st March 2010 | - |
Primary Conductivity SBE-4C | 4C-2841 | 10th March 2010 | developed an offset therefore was replaced after cast 095 |
Primary Conductivity SBE-4C | 4C-3272 | 25th February 2010 | used from cast 096 onwards |
Secondary Conductivity SBE-4C | 4C-3258 | 31st March 2010 | - |
Sea-Bird SBE 43 dissolved oxygen sensor | 43-1624 | 9th April 2010 | - |
CTG MkIII Aquatracka fluorimeter | 88-2050-095 | 19th January 2009 | - |
CTG MkII Alphatracka Transmissometer (10cm path) | 161049 | 24th September 2005 | Failed after cast 003 |
CTG MkII Alphatracka Transmissometer (10cm path) | 161050 | 7th November 2005 | From cast 004 |
Tritech PA200 Altimeter | 6196.118171 | - | - |
TRDI WHM300kHz LADCP | 13329 | Serviced 21st September 2009 | - |
CTG 2pi-PAR light | PAR06 | 26th October 2007 | UWIRR |
CTG 2pi-PAR light | PAR07 | 11th October 2007 | UWIRR |
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.
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.
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.
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.
The Chelsea Technologies Group ALPHAtracka (the Mark I) and its successor, the ALPHAtracka II (the Mark II), are both accurate (< 0.3 % fullscale) transmissometers that measure the beam attenuation coefficient at 660 nm. Green (565 nm), yellow (590 nm) and blue (470 nm) wavelength variants are available on special order.
The instrument consists of a Transmitter/Reference Assembly and a Detector Assembly aligned and spaced apart by an open support frame. The housing and frame are both manufactured in titanium and are pressure rated to 6000 m depth.
The Transmitter/Reference housing is sealed by an end cap. Inside the housing an LED light source emits a collimated beam through a sealed window. The Detector housing is also sealed by an end cap. A signal photodiode is placed behind a sealed window to receive the collimated beam from the Transmitter.
The primary difference between the ALPHAtracka and ALPHAtracka II is that the Alphatracka II is implemented with surface-mount technology; this has enabled a much smaller diameter pressure housing to be used while retaining exactly the same optical train as in the Mark I. Data from the Mark II version are thus fully compatible with that already obtained with the Mark I. The performance of the Mark II is further enhanced by two electronic developments from Chelsea Technologies Group - firstly, all items are locked in a signal nulling loop of near infinite gain and, secondly, the signal output linearity is inherently defined by digital circuitry only.
Among other advantages noted above, these features ensure that the optical intensity of the Mark II, indicated by the output voltage, is accurately represented by a straight line interpolation between a reading near full-scale under known conditions and a zero reading when blanked off.
For optimum measurements in a wide range of environmental conditions, the Mark I and Mark II are available in 5 cm, 10 cm and 25 cm path length versions. Output is default factory set to 2.5 volts but can be adjusted to 5 volts on request.
Further details about the Mark II instrument are available from the Chelsea Technologies Group ALPHAtrackaII specification sheet.
This altimeter is a sonar ranging device that gives the height above the sea bed when mounted vertically. When mounted in any other attitude the sensor provides a subsea distance. It can be configured to operate on its own or under control from an external unit and can be supplied with simultaneous analogue and digital outputs, allowing them to interface to PC devices, data loggers, telemetry systems and multiplexers.
These instruments can be supplied with different housings, stainless steel, plastic and aluminum, which will limit the depth rating. There are three models available: the PA200-20S, PA200-10L and the PA500-6S, whose transducer options differ slightly.
Transducer options | PA200-20S | P200-10L | PA500-6S |
Frequency (kHz) | 200 | 200 | 500 |
Beamwidth (°) | 20 Conical | 10 included conical beam | 6 Conical |
Operating range | 1 to 100 m 0.7 to 50 m | - | 0.3 to 50 m 0.1 to 10 m |
Common specifications are presented below
Digital resolution | 1 mm |
Analogue resolution | 0.25% of range |
Depth rating | 700 , 2000, 4000 and 6800 m |
Operating temperature | -10 to 40°C |
Further details can be found in the manufacturer's specification sheet.
The CTD data from the Stainless Steel Frame were supplied to BODC in 89 PStar files and converted to the BODC internal format (QXF).
During transfer the originator's variables were mapped to unique BODC parameter codes. The following table shows the parameter mapping.
Originator's variable | Units | Description | BODC Code | Units | Comments |
---|---|---|---|---|---|
time | - | Time | - | - | Not transferred - will be superseded in BODC processing |
press | decibars | Pressure (spatial co-ordinate) exerted by the water body by profiling pressure sensor and corrected to read zero at sea level. | PRESPR01 | decibars | - |
temp | degC (ITS-90) | Temperature of the water body by CTD and NO verification against independent measurements | TEMPCU01 | degC (ITS-90) | - |
temp2 | degC (ITS-90) | Temperature of the water body by CTD and NO verification against independent measurements | TEMPCU02 | degC (ITS-90) | - |
cond | mS/cm | Electrical conductivity of the water body by CTD | CNDCST01 | Siemens per metre | cond divided by 10 |
cond2 | mS/cm | Electrical conductivity of the water body by CTD | CNDCST02 | Siemens per metre | cond2 divided by 10 |
oxyV | volts | Raw output from the oxygen sensor | - | - | Raw output, not transferred - superseded by processed oxygen |
oxygen | umol/l | Concentration of oxygen {O2} per unit volume of the water body [dissolved phase] by Sea-Bird SBE 43 sensor and calibration against sample data | DOXYSC01 | Micromoles per litre | - |
salin | pss-78 | Practical salinity of the water body by CTD and computation using UNESCO 1983 algorithm and calibration against independent measurements | PSALCC01 | pss-78 | - |
salin2 | pss-78 | Practical salinity of the water body by CTD and computation using UNESCO 1983 algorithm and calibration against independent measurements | PSALCC02 | pss-78 | - |
potemp | degC | Potential Temperature | - | - | Not transferred - can be calculated from pressure, salinity and temperature |
potemp2 | degC | Potential Temperature | - | - | Not transferred - can be calculated from pressure, salinity and temperature |
sigma0 | kg/m3 | Sigma-theta of the water body | - | - | Not transferred - recalculated by the BODC transfer |
sigma2 | kg/m3 | Sigma-theta of the water body | - | - | Not transferred - recalculated by the BODC transfer |
fluor | ug/l | Concentration of chlorophyll-a {chl-a} per unit volume of the water body [particulate phase] by in-situ chlorophyll fluorometer and manufacturer's calibration applied | CPHLPM01 | mg/m3 | ug/l=mg/m3 |
trans | % | Transmittance per unspecified length of the water column by transmissometer | POPTPZ01 | % | - |
atten | /m | Attenuance (red light wavelength) per unit length of the water body by 5 or 10cm path length transmissometer | ATTNSR01 | /m | - |
The PAR data was not supplied by the Data Originator.
Following transfer the data were screened using BODC in-house visualisation software. Suspect data values were assigned the appropriate BODC data quality flag. Missing data values were changed to the missing data value and assigned a BODC data quality flag
Two Conductivity-Temperature-Depth (CTD) units was used on D351 to produce vertical profiles of the temperature and salinity of the water column. In total 101 CTD profiles were conducted during D351 using a combination of Stainless Steel and Titanium framed rosette systems.
62 CTD casts were conducted to obtain the 2010 Ellett Line hydrographic section. A further 39 CTD profiles were conducted, after completion of the Ellett Line section, as part of a 24 hour station occupation above the Anton Dohrn seamount, during which time the CTD was repeatedly 'yo-yoed' from the surface to a depth of ~800m, and as part of a short survey away from the seamount itself.
The data were processed using PEXEC routines, using different scripts for the stainless steel frame and the titanium frame. Further details on the processing can be found in the cruise report. The data were calibrated post-cruise and further details can be found in the post cruise calibration report.
The processed data, together with the raw Sea-Bird, configuration and bottle files, were supplied to BODC for banking.
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:
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:
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:
In order to address these aims there are nine science themes supported by the Oceans 2025 programme:
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:
The data is to be fed into models for validation and future projections. Greater detail can be found in the Theme documents.
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.
Weblink: http://www.oceans2025.org/
The Ellett Line (begun in 1975 and since 1996 the Extended Ellett Line from Scotland to Iceland) crosses important north Atlantic Meridional Overturning Circulation (MOC) components and thus provides an additional contribution to understanding the north Atlantic response to climate change. Sustained Observation Activity (SO) 4 will repeat this section annually collecting a wide variety of physical and biogeochemical measurements, and will, to enhance the time variable component, make use of Argo floats and gliders. SO 4 will be implemented by physical, biological and chemical scientists at the National Oceanography Centre, Southampton (NOCS) and the Scottish Association for Marine Science (SAMS).
SO 4 formally contributes to the Department for Environment, Food and Rural Affairs (DEFRA)-funded Marine Environmental Change Network (MECN). Established in 2002 to coordinate and promote the collection and utilisation of marine time-series and long-term data sets, the goal of the network is to use long-term marine environmental data from around the British Isles and Ireland to separate natural fluctuations from global, regional and local anthropogenic impacts.
The specific deliverables for SO 4 are:
More detailed information on this Work Package is available at pages 15 - 16 of the official Oceans 2025 Theme 10 document: Oceans 2025 Theme 10
Weblink: http://www.oceans2025.org/
Cruise Name | D351 |
Departure Date | 2010-05-11 |
Arrival Date | 2010-05-28 |
Principal Scientist(s) | Jane F Read (National Oceanography Centre, Southampton) |
Ship | RRS Discovery |
Complete Cruise Metadata Report is available here
Station Name | Ellett Line/Extended Ellett Line Station 11G |
Category | Offshore location |
Latitude | 56° 43.98' N |
Longitude | 7° 40.02' W |
Water depth below MSL | 55.0 m |
Station 11G is one of the fixed CTD stations, which together form The Extended Ellett Line. The line lies between Iceland and the Sound of Mull (Scotland) crossing the Iceland Basin and Rockall Trough via the outcrop of Rockall. As part of this initiative, CTD dips, together with associated discrete sampling of the water column, have typically been carried out annually at this station since September 1996.
Prior to September 1996, Station 11G was part of a shorter repeated survey section, consisting of 35 fixed stations, known as The Ellett Line (originally termed the Anton Dohrn Seamount Section). This line incorporated those stations across the Rockall Trough and Scottish shelf between Rockall and the Sound of Mull and was visited at regular intervals (usually at least once a year) between 1975 and January 1996. During this period Station 11G was also referred to as Station C7.
Other Cruises linked to this Fixed Station (with the number of series) - 0508S (1) CD176 (1) CD44 (1) CD92B (2) CH1/85 (1) CH10/81 (1) CH10/84 (1) CH101B (1) CH103 (1) CH105 (2) CH11/77 (1) CH11/83 (1) CH110 (1) CH112 (2) CH114 (1) CH116 (1) CH11B/78 (1) CH120 (1) CH124 (1) CH13/77 (1) CH13/79 (1) CH14 (1) CH14B/78 (1) CH15/80 (1) CH16/79 (1) CH2/78 (1) CH2/84 (1) CH22 (1) CH25 (1) CH30 (2) CH4/77 (1) CH4/80 (1) CH4/85 (1) CH5A/76 (1) CH6/78 (1) CH67A (1) CH6A/81 (1) CH6B/77 (1) CH7/79 (1) CH71A (1) CH74A_1 (1) CH75B (1) CH7A/82 (1) CH7B/83 (1) CH8/76 (1) CH8/85 (1) CH81 (1) CH86B (1) CH89B (1) CH9 (1) CH97 (1) CH9B/80 (1) D180 (1) D245 (1) D312 (2) D340A (1) D379 (1) DSK1/86 (1) DY031 (1) FR13/85 (1) FR18/87 (1) FR8/86 (1) JR20140531 (JR302) (1) LF1/89 (1) LF2/89 (1) PO300_2 (2) PO314 (1)
Station Name | Ellett Line |
Category | Offshore route/traverse |
The Ellett Line is a hydrographic transect consisting of 35 individual fixed stations which were occupied, usually at least once a year, between 1975 and 1996. The time series is named after the scientist David Ellett, who coordinated the survey work at Dunstaffnage Marine Laboratory (DML), near Oban. The transect ran between the north west coast of Scotland to the small outcrop of Rockall, via the Anton Dohrn Seamount - a prominent bathymetric feature in the Rockall Trough (see map). STD/CTD dips and associated water sampling for the analysis of nutrients were routinely performed during each station occupation.
In 1996 the transect was lengthened to incorporate new additional fixed stations crossing the Iceland Basin from Rockall to Iceland. This transect, which is still routinely occupied annually, is now known as the Extended Ellett Line and is a collaborative effort between scientists at Dunstaffnage Marine Laboratory and the Southampton site of the National Oceanography Centre (NOC).
Map produced using the GEBCO Digital Atlas
The white triangles indicate the nominal positions of the Ellett Line stations (1975- 1996). Measurements made along the Ellett Line lie within a box bounded by co-ordinates 56° 40.02' N, 13° 42.0' W at the south west corner and 57° 37.2' N, 6° 7.98' W at the north east corner.
Listed below are nominal details of the standard hydrographic stations that formed the Ellett Line between 1975 and January 1996.
Station | Latitude | Longitude | Depth | Range |
---|---|---|---|---|
A | 57.583 N | 13.633 W | 130 m | 10.0 nm |
B | 57.567 N | 13.333 W | 210 m | 9.7 nm |
C | 57.550 N | 13.000 W | 330 m | 10.8 nm |
D | 57.542 N | 12.867 W | 1000 m | 4.3 nm |
E | 57.533 N | 12.633 W | 1658 m | 7.6 nm |
F | 57.508 N | 12.250 W | 1817 m | 12.5 nm |
G | 57.492 N | 11.850 W | 1812 m | 13.0 nm |
H | 57.483 N | 11.533 W | 2020 m | 10.3 nm |
I | 57.467 N | 11.317 W | 750 m | 7.0 nm |
J | 57.450 N | 11.083 W | 550 m | 7.6 nm |
K | 57.400 N | 10.867 W | 850 m | 7.6 nm |
L | 57.367 N | 10.667 W | 2076 m | 6.8 nm |
M | 57.300 N | 10.383 W | 2340 m | 10.1 nm |
N | 57.233 N | 10.050 W | 2100 m | 11.5 nm |
O | 57.150 N | 9.700 W | 1900 m | 12.4 nm |
P | 57.100 N | 9.417 W | 1050 m | 9.7 nm |
Q | 57.050 N | 9.217 W | 350 m | 7.2 nm |
R | 57.000 N | 9.000 W | 135 m | 7.7 nm |
S | 56.950 N | 8.783 W | 125 m | 7.7 nm |
15G | 56.883 N | 8.500 W | 125 m | 10.1 nm |
T | 56.837 N | 8.333 W | 120 m | 6.1 nm |
14G | 56.808 N | 8.167 W | 115 m | 5.7 nm |
13G | 56.783 N | 8.000 W | 110 m | 5.7 nm |
12G | 56.758 N | 7.833 W | 80 m | 5.7 nm |
11G | 56.733 N | 7.667 W | 55 m | 5.7 nm |
10G | 56.733 N | 7.500 W | 220 m | 5.5 nm |
9G | 56.733 N | 7.333 W | 160 m | 5.5 nm |
8G | 56.733 N | 7.167 W | 175 m | 5.5 nm |
7G | 56.733 N | 7.000 W | 145 m | 5.5 nm |
6G | 56.733 N | 6.750 W | 35 m | 8.2 nm |
5G | 56.733 N | 6.600 W | 75 m | 4.9 nm |
4G | 56.733 N | 6.450 W | 115 m | 4.9 nm |
3G | 56.708 N | 6.367 W | 75 m | 3.1 nm |
2G | 56.683 N | 6.283 W | 40 m | 3.2 nm |
1G | 56.667 N | 6.133 W | 190 m | 5.0 nm |
BODC Cruise Identifier | Cruise Dates | Ship |
---|---|---|
CH3/75 | 4-13 March 1975 | RRS Challenger |
CH7A/75 | 1-6 May 1975 | RRS Challenger |
CH10A/75 | 4-10 July 1975 | RRS Challenger |
CH12A/75 | 26 August-2 September 1975 | RRS Challenger |
CH14A/75 | 7-12 November 1975 | RRS Challenger |
CH5A/76 | 29 March-5 April 1976 | RRS Challenger |
CH8/76 | 19 May-1 June 1976 | RRS Challenger |
CH12/76 | 4-15 August 1976 | RRS Challenger |
CH15/76 | 7-16 October 1976 | RRS Challenger |
CH17/76 | 7-20 December 1976 | RRS Challenger |
CH4/77 | 25 February-11 March 1977 | RRS Challenger |
CH6B/77 | 14-19 April 1977 | RRS Challenger |
CH10/77 | 29 June-10 July 1977 | RRS Challenger |
CH11/77 | 12-26 July 1977 | RRS Challenger |
CH13/77 | 20 August-3 September 1977 | RRS Challenger |
CH2/78 | 30 January-13 February 1978 | RRS Challenger |
CH6/78 | 11-21 April 1978 | RRS Challenger |
CH9/78 | 31 May-10 June 1978 | RRS Challenger |
CH11B/78 | 29 July-12 August 1978 | RRS Challenger |
CH11D/78 | 3-17 September 1978 | RRS Challenger |
CH14B/78 | 4-11 November 1978 | RRS Challenger |
CH7/79 | 10-23 May 1979 | RRS Challenger |
S5/79 | 19 June-2 July 1979 | RRS Shackleton |
CH13/79 | 11-16 September 1979 | RRS Challenger |
CH16/79 | 28 October-11 November 1979 | RRS Challenger |
CH4/80 | 26 February-7 March 1980 | RRS Challenger |
CH7/80 | 21 April-6 May 1980 | RRS Challenger |
CH2/81 | 26 January-4 February 1981 | RRS Challenger |
CH6A/81 CH6B/81 | 6-25 April 1981 | RRS Challenger |
CH10/81 | 4-14 July 1981 | RRS Challenger |
CH15/81 | 6-20 October 1981 | RRS Challenger |
CH7A/82 CH7B/82 | 26 April-16 May 1982 | RRS Challenger |
CH15/82 | 16-30 October 1982 | RRS Challenger |
CH7B/83 | 23 May-2 June 1983 | RRS Challenger |
CH11/83 | 10-24 August 1983 | RRS Challenger |
CH2/84 | 23 June-8 July 1984 | RRS Challenger |
CH10/84 | 16 November-6 December 1984 | RRS Challenger |
CH1/85 | 20 January-5 February 1985 | RRS Challenger |
CH4/85 | 2-16 May 1985 | RRS Challenger |
CH8/85 | 14-28 August 1985 | RRS Challenger |
CH9 | 8-22 January 1987 | RRS Challenger |
CH14 | 24 April-7 May 1987 | RRS Challenger |
CH22 | 23 November-5 December 1987 | RRS Challenger |
CH25 | 24 February-7 March 1988 | RRS Challenger |
CH30 | 6-23 June 1988 | RRS Challenger |
D180 | 20 January-4 February 1989 | RRS Discovery |
LF1/89 | 5-11 May 1989 | RV Lough Foyle |
LF2/89 | 4-10 August 1989 | RV Lough Foyle |
CD44 | 24 November-2 December 1989 | RRS Charles Darwin |
CH67A | 21-29 June 1990 | RRS Challenger |
CH71A | 29 August-5 September 1990 | RRS Challenger |
CH75B | 23 February-3 March 1991 | RRS Challenger |
CH81 | 1-8 July 1991 | RRS Challenger |
CH97 | 25 September-6 October 1992 | RRS Challenger |
CH101B | 13-20 March 1993 | RRS Challenger |
CH103 | 12-24 May 1993 | RRS Challenger |
CH105 | 3-16 September 1993 | RRS Challenger |
CH110 | 10-20 March 1994 | RRS Challenger |
CH112 | 28 April-13 May 1994 | RRS Challenger |
CH114 | 15-29 August 1994 | RRS Challenger |
CH116 | 17-29 November 1994 | RRS Challenger |
CD92B | 13 April-2 May 1995 | RRS Charles Darwin |
CH120 | 18 July-6 August 1995 | RRS Challenger |
CH124 | 8-27 January 1996 | RRS Challenger |
Other Series linked to this Fixed Station for this cruise - 1052652 1052664 1052676 1052688 1052707 1052719 1052720 1052732 1052744 1052756 1052768 1052781 1052793 1052800 1052812 1052824 1052836 1052848 1052861 1052873 1052885 1052904 1052916 1052928 1052941 1052953 1052965 1052977 1052989 1052990 1053004 1053551 1053563
Other Cruises linked to this Fixed Station (with the number of series) - 0508S (29) 0700S (20) 0703S (20) CD176 (32) CD44 (34) CD92B (47) CH1/85 (19) CH10/77 (3) CH10/81 (21) CH10/84 (22) CH101B (13) CH103 (37) CH105 (34) CH10A/75 (15) CH11/77 (28) CH11/83 (35) CH110 (19) CH112 (35) CH114 (31) CH116 (25) CH11B/78 (26) CH11D/78 (14) CH120 (28) CH124 (32) CH12A/75 (3) CH13/77 (19) CH13/79 (17) CH14 (29) CH14A/75 (21) CH14B/78 (17) CH15/80 (8) CH15/81 (16) CH16/79 (13) CH2/78 (32) CH2/81 (13) CH2/82 (4) CH2/84 (29) CH22 (14) CH25 (18) CH3/83 (1) CH30 (23) CH4/77 (19) CH4/80 (29) CH4/85 (30) CH5A/76 (18) CH6/78 (25) CH63_2 (5) CH67A (27) CH6A/81 (14) CH6B/77 (24) CH6B/81 (20) CH7/79 (18) CH7/80 (16) CH71A (32) CH74A_1 (13) CH75B (31) CH7A/75 (24) CH7A/82 (24) CH7B/82 (13) CH7B/83 (29) CH8/76 (27) CH8/85 (30) CH81 (30) CH86B (8) CH89B (9) CH9 (25) CH9/78 (22) CH97 (30) CH9B/80 (10) D180 (30) D223A (22) D230 (11) D233 (10) D242 (23) D245 (25) D253 (22) D312 (34) D321B (35) D340A (34) D351 (33) D365 (55) D379 (36) DSK1/86 (10) FR13/85 (12) FR13/87 (2) FR14B/87 (2) FR18/87 (11) FR7B/86 (6) FR8/86 (13) JC086 (35) JR20140531 (JR302) (37) LF1/89 (29) LF2/89 (30) PO300_2 (31) PO314 (30) S5/79 (8)
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 |
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 |