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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."
A networked gas chromatograph that separates and analyses gas mixtures in water or air. The instrument includes a dual channel design supporting two inlets and two detectors. An automatic liquid sampling system is fully integrated into the mainframe control and atmospheric pressure and temperature compensation is standard. The instrument also supports 6 column oven ramps with 7 plateaus.
The 6890N is completely customisable depending on the application, with choices of inlets, columns, detectors and sampling systems. Available detectors include; flame ionization, thermal conductivity, micro-electron capture, nitrogen-phosphorus, single- or dual-wavelength flame photometric. Specialised detectors include: atomic emission, Helium ionization, sulphur chemiluminescence and pulsed discharge ionization. All detectors include electronic pneumatics control and electronic on/off for all detector gases. Carrier and makeup gas settings are selectable for He, H2, N2, and argon/methane. There is a choice of inlets including; packed purged injection port, split/splitless capillary inlet, temperature-programmable cool on-column, programmable temperature vaporizer and volatiles inlet. A full array of gas sampling and column switching valves are also available. The instrument has a 7683 ALS interface and incorporates local area network technology as standard.
The Agilent 6890N uses many of the same components as the Agilent 6850N GC producing virtually identical results, but the Agilent 6850N is only half as wide. The Agilent 6890N replaces the HP Agilent 5890 and is no longer in production.
Please see the Agilent 6890N brochure and data sheet for further details.
Instrument | Serial Number | Calibration date | Comments |
---|---|---|---|
Rockland Scientific International Vertical Microstructure Profiler 5500 | 016 | - | - |
Sea-bird 3F fast temperature sensor | 4634 | - | Standard with the VMP 5500 |
Sea-bird 4C conductivity sensor | 3240 | - | Standard with the VMP 5500 |
Sea-bird SPM-38-5 velocity shear probe (x2) | - | - | Standard with the VMP 5500 |
Sea-bird FP07-38-5 fast thermistor (x2) | - | - | Standard with the VMP 5500 |
Sea-bird microstructure conductivity probe (SBE7) | - | - | Optional with the VMP 5500 |
Please see the cruise report for further details of the instrumentation performance and recommendations.
A fast-response temperature sensor measuring microstructure temperature fluctuations for oceanographic applications. The sensing tip is a microbead thermistor (manufactured by GE Thermometics), mounted on a 9.525 mm diameter stainless steel sting which can be attached to ocean microstructure instruments. The instrument consists of small diameter glass-coated thermistor bead, thermetically sealed onto the tip of a shock-resistant glass rod.
Specifications
Range | -2 to 32 °C |
---|---|
Resolution | 0.0001 °C |
Response | 0.007 s (nominal) |
Nominal resistance | 2 kOhm (at 25 °C) |
Glass bead maximum | 2.2 mm |
Thermistor tip | Approximately 0.2 mm |
Length (overall) | 127 mm |
Weight (in air) | Approximately 100 g |
Diameter at base | 9.53 mm |
Housing | SS316 stainless steel |
Connector | Brass |
Bead | Glass |
A velocity shear probe measuring microstructure velocity fluctuations in oceans and lakes. The instrument measures a single spatial component of turbulent velocity fluctuations, in a direction perpendicular to the probes main axis. The sensing head is based upon the design by Osborn (1974) and the sensing element consists of a parabolic, flexible rubber tip. The oncoming flow produces a hydrodynamic lift force proportional to the fluctuating cross-stream velocity component u. A piezo-ceramic beam embedded in the rubber tip translates the lift force into an electric signal that is proportional to u. The length of the sensing tip (10 mm) determines the maximum wavenumber resolution of the sensor which is approximately 48 cycles per meter. The measurements can be corrected to include wavenumbers up to 150 cpm.
Specifications
Range | 0 to 10 s-1 |
---|---|
Resolution | Approximately 10 to 4 s-1 |
Response | 0.007 s (nominal) |
Sensitivity | 0.04 to 0.09 V m s -2 |
Pressure Rating | 1000 dbar (6000 dbar optional) |
Temperature range | -2 to 35 °C |
Length | 127 mm |
Diameter (maximum) | 9.5 mm |
Materials | Stainless/Teflon/Silicone |
Osborn, T.R., 1974. Vertical profiling of velocity microstructure. Journal of Physical Oceanography, 4, 109-115.
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.
Water temperature sensor primarily designed for use on the SBE 25 and 25plus Sealogger CTD systems but can be used as a component in custom oceanographic profiling systems or high-accuracy temperature-monitoring applications. The sensor operates over the range -5 to +35 °C and has an initial accuracy of +/-0.001°C. The sensor has a depth rating of 6800 m (aluminum housing) or 10500 m (titanium housing). The SBE 3F is an enhanced version of the SBE 3 temperature sensor.
Please see the SBE 3F specification sheet for further details.
Microstructure conductivity sensor designed for use on marine profiling applications to characterise small scale ocean conductivity features. The sensor is primarily used for the determination of conductivity gradients but it is configured to respond to absolute conductivity as well. The SBE 7 has an accuracy typically within 0.005 S m-1 over periods of several hours and has a high speed micro-scale resolution of 3 dbar at 100 cycles m -1 (-3 dbar at 1000 Hz). The sensor has aluminium housing and a depth rating of 6800 m.
Please see the SBE 7 specification sheet for further details.
VMP profiles provided by the originator in a structured Matlab format were converted into BODC internal format using standard BODC processing procedures. The following table shows how the variables within the Matlab file were mapped to appropriate BODC parameter codes:
Originator's Parameter Name | Units | Description | BODC Parameter Code | Units | Comments |
---|---|---|---|---|---|
jr276vmp.press | dbar | Pressure (spatial co-ordinate) exerted by the water body by profiling pressure sensor and corrected to read zero at sea level | PRESPR01 | dbar | - |
jr276vmp.temp | °C | Temperature of the water body from the CTD sensor | TEMPPR01 | °C | - |
jr276vmp.salin | Dimensionless | Practical salinity of the water body by conductivity cell and computation using UNESCO 1983 algorithm, from the CTD sensors | PSALPR01 | Dimensionless | - |
jr276vmp.chi | °C2 s -1 | Log10 temperature dissipation rate in the water body by turbulence profiler fast temperature sensor | TDSSFT01 | °C2 s -1 | The data have been transformed using Log10 |
jr276vmp.eps | W kg-1 | Log10 turbulent kinetic energy dissipation {epsilon} per unit volume of the water body by turbulence profiler shear sensor | EPSIPM01 | W kg-1 | The data have been transformed using Log10 |
The reformatted data were visualised using the in-house EDSERPLO software. The data were screened and quality control flags were applied to data as necessary.
Thirteen Vertical Microstructure Profiler (VMP) deployments were carried out successfully from 55 CTD stations. The general mode of microstructure operations consisted of a VMP deployment every four to eight CTD stations along section S3 and at alternate CTD stations on section SR1.
Instrument calibrations for the VMP were applied and corrections for the fact the unit was not pumped, but no external calibration either to the ship CTD or water samples were made.
A matlab routine (finestructure_processing_routine.m) was used to process the seabird finestructure. The temperature and salinity data from the CTD sensors were processed as follows:
Another matlab routine (process_micro_jr276_v2.m) was then used to convert the data to real units and to calibrate the seabird data. The epsilon and chi values are estimated by integrating the power spectra of the shear and the microtemperature gradient, respectively. The data were averaged into regular 0.5 dbar bins. The pressure value used to start the extracted downcast was modified from that used on JC054, such that the pressure value at which to start the extracted downcast was increased from 5.25 dB to 6.25 dB. The change was required to account for the different deployment procedures. On this cruise the VMP was released when deeper in the water than on JC054, such that the profiler did not reach the previous criteria of a drop speed of 0.4 m s-1 at 5.25 dB
Lastly the data were averaged into 1 dbar bins and saved as a matlab structure file using a Matlab program (make_cruise_data_set.m). The average results from the two shear or microtemperature probes were used, unless a probe was noisy, in which case the noisy probe data was discarded.
A full ocean-depth untethered vertical microstructure turbulence profiler for the measurement of dissipation-scale turbulence along with temperature and conductivity for up to 5500 m depth. The instrument is fitted with pressure, temperature (SBE-3F) and conductivity (SBE-4C) sensors, three acceleration sensors, a PC104 computer data acquisition and communication system, anti-aliasing filters and a standard suite of microstructure sensors which includes two SPM-38-5 velocity shear probes, two FP07-38-5 fast thermistors and an optional microstructure conductivity probe (SBE7).
All microstructure sensors are held in the nose cone and can be exchanged or replaced in the field, without the need of disassemble the main pressure case of the VMP which can hold up to 6 microstructure probes in any combination. The main pressure case contains the pressure transducer as well as the accelerometers, electronics for signal conditioning A/D conversion and data logging, and is separated from the nose cone by a 38 mm thick bulkhead which prevents water penetration into the main pressure case.
The instrument has an aluminium frame with syntactic foam attached for floatation. Data are collected on the downcast and after reaching a pre-defined depth the profiler releases ballast weights so that the instrument becomes positively buoyant. The instrument rises to the surface with a nominal speed of 1.0 ms-1. As a backup, there is a triple-redundancy emergency ballast release consisting of a corrosion trigger, time-out trigger and pressure rate-of-change trigger. The VMP 5500 has a strobe light and a radio beacon and can also be fitted with an Argos transmitter for locating the instrument after it has returned to the surface. The VMP 5500 was replaced by the VMP 6000 in 2010.
Please see the VMP 5500 specification sheet for further details.
DIMES is a US/UK field program aimed at measuring diapycnal and isopycnal mixing in the Southern Ocean, along the tilting isopycnals of the Antarctic Circumpolar Current.
The Meridional Overturning Circulation (MOC) of the ocean is a critical regulator of the Earth's climate processes. Climate models are highly sensitive to the representation of mixing processes in the southern limb of the MOC, within the Southern Ocean, although the lack of extensive in situ observations of Southern Ocean mixing processes has made evaluation of mixing somewhat difficult. Theories and models of the Southern Ocean circulation have been built on the premise of adiabatic flow in the ocean interior, with diabatic processes confined to the upper-ocean mixed layer. Interior diapycnal mixing has often been assumed to be small, but a few recent studies have suggested that diapycnal mixing might be large in some locations, particularly over rough bathymetry. Depending on its extent, this interior diapycnal mixing could significantly affect the overall energetics and property balances for the Southern Ocean and in turn for the global ocean. The goals of DIMES are to obtain measurements that will help us quantify both along-isopycnal eddy-driven mixing and cross-isopycnal interior mixing.
DIMES includes tracer release, isopycnal following RAFOS floats, microstructure measurements, shearmeter floats, EM-APEX floats, a mooring array in Drake Passage, hydrographic observations, inverse modeling, and analysis of altimetry and numerical model output.
DIMES is sponsored by the National Science Foundation (U.S.), Natural Environment Research Council (U.K) and British Antarctic Survey (U.K.)
For more information please see the official project website at DIMES
Cruise Name | JR20110409 (JR276, UKD-2.5) |
Departure Date | 2011-04-09 |
Arrival Date | 2011-04-26 |
Principal Scientist(s) | Andrew J Watson (University of East Anglia School of Environmental Sciences) |
Ship | RRS James Clark Ross |
Complete Cruise Metadata Report is available here
Station Name | Drake Passage - WOCE SR1b |
Category | Offshore route/traverse |
WOCE Southern Repeat Section 1B is a section across Drake Passage in the South Atlantic Ocean. The nominal end points of the section (to date) are at 52° 55.74' S, 58° 00.00' W (at the south of the Falkland Islands) and 61° 03.05' S, 54° 33.10' W (off Elephant Island at the north end of the Antarctic Peninsula).
The section was first occupied by the R/V Polarstern in 1992 (Gersonde, 1993). The first UK occupation of SR1b followed on RRS Discovery later the same year. The National Oceanography Centre, Southampton (formerly known as Southampton Oceanography Centre), in collaboration with the British Antarctic Survey, have occupied the section most years since 1993 on the RRS James Clark Ross. Additionally, there were three Spanish occupations on R/V Hespérides in February 1995, 1996 and 1998 (Garcia et al., 2002). A Drake Passage summary report for RRS James Clark Ross cruises between 1993 - 2000 has been produced.
A table of cruises which occupied SR1b is presented below with links to the relevant cruise reports (were available).
Cruise | Country | Start Date | End Date |
---|---|---|---|
R/V Polarstern ANT 10-5 | Germany | 08-08-1992 | 26-09-1992 |
RRS Discovery D198 | United Kingdom | 11-11-1992 | 17-12-1992 |
RRS James Clark Ross JR0a | United Kingdom | 20-11-1993 | 18-12-1993 |
RRS James Clark Ross JR0b | United Kingdom | 13-11-1994 | 30-11-1994 |
R/V Hespérides 29HE19951203 | Spain | 03-12-1995 | 06-01-1996 |
R/V Hespérides 29HE19960117 | Spain | 17-01-1996 | 05-02-1996 |
RRS James Clark Ross JR16 | United Kingdom | 13-11-1996 | 07-12-1996 |
RRS James Clark Ross JR27 | United Kingdom | 17-12-1997 | 08-01-1998 |
R/V Hespérides 29HE19980730 | Spain | 27-07-1998 | 27-08-1998 |
RRS James Clark Ross JR47 | United Kingdom | 13-01-2000 | 17-02-2000 |
RRS James Clark Ross JR55 | United Kingdom | 21-11-2000 | 14-12-2000 |
RRS James Clark Ross JR67 | United Kingdom | 19-11-2001 | 17-12-2001 |
RRS James Clark Ross JR81 | United Kingdom | 18-12-2002 | 02-01-2003 |
RRS James Clark Ross JR94 | United Kingdom | 28-11-2003 | 16-12-2003 |
RRS James Clark Ross JR115 | United Kingdom | 01-12-2004 | 19-12-2004 |
RRS James Clark Ross JR139 | United Kingdom | 05-12-2005 | 12-12-2005 |
RRS James Clark Ross JR163 | United Kingdom | 06-12-2006 | 15-12-2006 |
RRS James Clark Ross JR193 | United Kingdom | 29-11-2007 | 08-12-2007 |
RRS James Clark Ross JR194 | United Kingdom | 12-12-2008 | 20-12-2008 |
RRS James Cook JC031 | United Kingdom | 03-02-2009 | 03-03-2009 |
RRS James Clark Ross JR195 | United Kingdom | 19-11-2009 | 26-11-2009 |
RRS James Clark Ross JR242 | United Kingdom | 06-12-2010 | 18-12-2000 |
RRS James Clark Ross JR276 | United Kingdom | 09-04-2011 | 26-04-2011 |
RRS James Clark Ross JR265 and JR254D | United Kingdom | 27-11-2011 | 24-12-2011 |
RRS James Cook JC069 | United Kingdom | 31-01-2012 | 21-03-2012 |
RRS James Clark Ross JR281 | United Kingdom | 17-03-2013 | 27-04-2013 |
RRS James Clark Ross JR299 | United Kingdom | 08-03-2014 | 29-03-2014 |
RRS James Clark Ross JR306 | United Kingdom | 10-01-2015 | 20-01-2015 |
RRS James Clark Ross JR15003 | United Kingdom | 17-12-2015 | 13-01-2016 |
RRS James Clark Ross JR16002 | United Kingdom | 10-11-2016 | 03-12-2016 |
García, M. A., I. Bladé, A. Cruzado, Z. Velásquez, H. García, J. Puigdefàbregas and J. Sospedra, 2002: Observed variability of water properties and transports on the World Ocean Circulation Experiment SR1b section across the Antarctic Circumpolar Current. J. Geophys. Res. 107 (C10) 3162, 10.1029/2000JC000277.
Gersonde, R., 1993: The Expedition Antarktis X/5 of RV Polarstern in 1992. Berichte zur Polarforschung, 131, 167 pp.
Other Series linked to this Fixed Station for this cruise - 1089197 1089204 1089216 1089228 1089241 1089253 1089265 1089277 1089289 1089308 1089321 1089333 1089345 1089357 1089369 1716401 1716413 1716425 1716437 1716449 1716450 1716462 1716474 1716486 1716498 1716505 1716517 1718075 1718087 1718099 1718106 1718118 1718131 1718143 1718155 1718167 1718179 1718180 1718192 1718211 1718223 1718235
Other Cruises linked to this Fixed Station (with the number of series) - JC031 (105) JC069 (UKD-3) (18) JR16002 (61) JR19931120 (JR00a) (30) JR19941113 (JR0B) (29) JR19961128 (JR16) (29) JR19971217 (JR27) (54) JR20000113 (JR47) (29) JR20001121 (JR55) (31) JR20021224 (JR81) (32) JR20031211 (JR94) (30) JR20041201 (JR111, JR115) (35) JR20071129 (JR171, JR193, JR196 Leg1, JR212) (32) JR20081212 (JR194, JR197) (30) JR20091118 (JR195, JR198) (33) JR20101205 (JR242) (9) JR20110409 (JR276, UKD-2.5) (42) JR20111127 (JR254D, JR264, JR265) (31) JR20130317 (JR252B, JR272B, JR273A, JR281, UKD-4) (64) JR20140309 (JR293 Leg1, JR299 Leg1, UKD-5) (21) JR20150110 (JR305, JR306) (31)
Station Name | Drake Passage - WOCE SR1 |
Category | Offshore route/traverse |
WOCE established a repeat hydrographic section across Drake Passage and designated it SR1 (also known as A21). The section is located between the Southern tip of South America and the West Antarctic Peninsula within a bounding box of 55° 19.40' S, 68° 15.80' W (North-Western corner) and 64° 8.52' S, 63° 4.80' W (South-Eastern corner).
A table of cruises which occupied SR1 is presented below with links to the relevant cruise reports (where available).
Cruise | Country | Start Date | End Date |
---|---|---|---|
R/V Meteor 11/5 | Germany | 23-01-1990 | 08-03-1990 |
Polarstern ANT 10-5 | Germany | 08-08-1992 | 26-09-1992 |
R/V Vidal Gormaz 20VDSR0193_1 | Chile | 02-11-1993 | 25-12-1993 |
R/V Vidal Gormaz 20VDSR0194_1 | Chile | 08-11-1994 | 08-12-1994 |
R/V Vidal Gormaz 20VDSR0195_1 | Chile | 04-12-1995 | 15-12-1995 |
R/V Vidal Gormaz 20VDSR0196_1 | Chile | 28-11-1996 | 13-12-1996 |
R/V Vidal Gormaz 20VDSR0198_1 | Chile | 26-11-1998 | 15-12-1998 |
RRS James Clark Ross JR40 | United Kingdom | 15-03-1999 | 22-04-1999 |
RRS James Cook JC031 | United Kingdom | 03-02-2009 | 03-03-2009 |
RRS James Cook JC054 | United Kingdom | 28-11-2010 | 08-01-2011 |
RRS James Cook JC069 | United Kingdom | 31-01-2012 | 22-03-2012 |
Other Series linked to this Fixed Station for this cruise - 1716401 1716413 1716425 1716437 1716449 1716450 1716462 1716474 1716486 1716498 1716505 1716517
Other Cruises linked to this Fixed Station (with the number of series) - JC031 (142) JC054 (UKD-2) (45) JC069 (UKD-3) (8) JR19950320 (JR10) (128) JR20110409 (JR276, UKD-2.5) (12)
Station Name | Drake Passage |
Category | Offshore area |
Latitude | 59° 0.00' S |
Longitude | 62° 0.00' W |
Water depth below MSL |
The World Ocean Circulation Experiment (WOCE, 1990-1998) was a major international experiment which made measurements and undertook modelling studies of the deep oceans in order to provide a much improved understanding of the role of ocean circulation in changing and ameliorating the Earth's climate.
The Drake Passage is the narrowest constriction of the Antarctic Circumpolar Current (ACC) - the largest current in the world and connects all three major oceanic basins both horizontally and vertically, thus being a key control in the global overturning circulation.Within the Drake Passage, two repeat hydrographic sections (SR1 and SR1b) were established by WOCE. These were designed to extend measurements collected earlier by the International Southern Ocean Studies (ISOS) programme and have continued beyond the WOCE time-frame.
The original section was SR1 (which also covers part of the A21 one time survey track). Subsequently, the section was shifted to the east (and designated SR1b) in order for it to lie on a satellite ground track as illustrated in the image below.
In addition to the hydrographic measurements, UK research in Drake Passage also includes a network of coastal and deep tide gauges, analysis of satellite altimeter data, and state-of-the-art global numerical modeling.
Other Series linked to this Fixed Station for this cruise - 1089197 1089204 1089216 1089228 1089241 1089253 1089265 1089277 1089289 1089308 1089321 1089333 1089345 1089357 1089369 1716401 1716413 1716425 1716437 1716449 1716450 1716462 1716474 1716486 1716498 1716505 1716517 1717662 1717674 1717686 1717698 1717705 1717717 1717729 1717730 1717742 1717754 1717766 1717778 1717791 1717809 1717810 1717822 1717834 1717846 1717858 1717871 1717883 1717895 1717902 1717914 1717926 1717938 1717951 1717963 1717975 1717987 1717999 1718002 1718014 1718026 1718038 1718051 1718063
Other Cruises linked to this Fixed Station (with the number of series) - JC031 (247) JC041 (UKD-1) (66) JC054 (UKD-2) (146) JC069 (UKD-3) (24) JR16002 (61) JR19931120 (JR00a) (30) JR19941113 (JR0B) (29) JR19961128 (JR16) (29) JR20000113 (JR47) (29) JR20001121 (JR55) (32) JR20021224 (JR81) (32) JR20031211 (JR94) (30) JR20041201 (JR111, JR115) (35) JR20050124 (JR112, JR113) (5) JR20060216 (JR136, JR137) (1) JR20061206 (JR155, JR163, JR164) (1) JR20071129 (JR171, JR193, JR196 Leg1, JR212) (32) JR20091118 (JR195, JR198) (33) JR20101205 (JR242) (9) JR20110409 (JR276, UKD-2.5) (64) JR20130317 (JR252B, JR272B, JR273A, JR281, UKD-4) (175) JR20140309 (JR293 Leg1, JR299 Leg1, UKD-5) (21) JR20150110 (JR305, JR306) (1) RATS/CTD100 (1) RATS/CTD103 (1) RATS/CTD106 (1) RATS/CTD108 (1) RATS/CTD111 (1) RATS/CTD113 (1) RATS/CTD115 (1) RATS/CTD120 (1) RATS/CTD122 (1) RATS/CTD124 (1) RATS/CTD126 (1) RATS/CTD129 (1) RATS/CTD131 (1) RATS/CTD133 (1) RATS/CTD136 (1) RATS/CTD138 (1) RATS/CTD140 (1) RATS/CTD142 (1) RATS/CTD145 (1) RATS/CTD147 (1) RATS/CTD150 (1) RATS/CTD151 (1) RATS/CTD153 (1) RATS/CTD154 (1) RATS/CTD156 (1) RATS/CTD157 (1) RATS/CTD160 (1) RATS/CTD163 (1) RATS/CTD164 (1) RATS/CTD166 (1) RATS/CTD167 (1) RATS/CTD169 (1) RATS/CTD170 (1) RATS/CTD173 (1) RATS/CTD175 (1) RATS/CTD177 (1) RATS/CTD180 (1) RATS/CTD182 (1) RATS/CTD184 (1) RATS/CTD186 (1) RATS/CTD189 (1) RATS/CTD191 (1) RATS/CTD193 (1) RATS/CTD195 (1) RATS/CTD198 (1) RATS/CTD200 (1) RATS/CTD202 (1) RATS/CTD204 (1) RATS/CTD206 (1) RATS/CTD208 (1) RATS/CTD210 (1) RATS/CTD214 (1) RATS/CTD217 (1) RATS/CTD219 (1) RATS/CTD221 (1) RATS/CTD223 (1) RATS/CTD225 (1) RATS/CTD227 (1) RATS/CTD230 (1) RATS/CTD232 (1) RATS/CTD234 (1) RATS/CTD237 (1) RATS/CTD239 (1) RATS/CTD241 (1) RATS/CTD243 (1) RATS/CTD245 (1) RATS/CTD247 (1) RATS/CTD249 (1) RATS/CTD251 (1) RATS/CTD254 (1) RATS/CTD256 (1) RATS/CTD258 (1) RATS/CTD260 (1) RATS/CTD262 (1) RATS/CTD265 (1) RATS/CTD267 (1) RATS/CTD269 (1) RATS/CTD271 (1) RATS/CTD273 (1) RATS/CTD275 (1) RATS/CTD277 (1) RATS/CTD281 (1) RATS/CTD283 (1) RATS/CTD285 (1) RATS/CTD287 (1) RATS/CTD289 (1) RATS/CTD291 (1) RATS/CTD293 (1) RATS/CTD295 (1) RATS/CTD297 (1) RATS/CTD301 (1) RATS/CTD305 (1) RATS/CTD307 (1) RATS/CTD309 (1) RATS/CTD311 (1) RATS/CTD313 (1) RATS/CTD315 (1) RATS/CTD317 (1) RATS/CTD319 (1) RATS/CTD321 (1) RATS/CTD323 (1) RATS/CTD325 (1) RATS/CTD327 (1) RATS/CTD329 (1) RATS/CTD331 (1) RATS/CTD335 (1) RATS/CTD337 (1) RATS/CTD341 (1) RATS/CTD343 (1) RATS/CTD345 (1) RATS/CTD347 (1) RATS/CTD351 (1) RATS/CTD353 (1) RATS/CTD355 (1) RATS/CTD357 (1) RATS/CTD361 (1) RATS/CTD363 (1) RATS/CTD365 (1) RATS/CTD373 (1) RATS/CTD375 (1) RATS/CTD377 (1) RATS/CTD379 (1) RATS/CTD381 (1) RATS/CTD383 (1) RATS/CTD385 (1) RATS/CTD387 (1) RATS/CTD389 (1) RATS/CTD395 (1) RATS/CTD397 (1) RATS/CTD399 (1) RATS/CTD401 (1) RATS/CTD403 (1) RATS/CTD405 (1) RATS/CTD407 (1) RATS/CTD409 (1) RATS/CTD411 (1) RATS/CTD415 (1) RATS/CTD417 (1) RATS/CTD419 (1) RATS/CTD423 (1) RATS/CTD425 (1) RATS/CTD427 (1) RATS/CTD429 (1) RATS/CTD43 (1) RATS/CTD431 (1) RATS/CTD433 (1) RATS/CTD437 (1) RATS/CTD439 (1) RATS/CTD443 (1) RATS/CTD445 (1) RATS/CTD461 (1) RATS/CTD463 (1) RATS/CTD465 (1) RATS/CTD467 (1) RATS/CTD469 (1) RATS/CTD471 (1) RATS/CTD473 (1) RATS/CTD475 (1) RATS/CTD477 (1) RATS/CTD479 (1) RATS/CTD481 (1) RATS/CTD483 (1) RATS/CTD485 (1) RATS/CTD487 (1) RATS/CTD489 (1) RATS/CTD49 (1) RATS/CTD491 (1) RATS/CTD493 (1) RATS/CTD495 (1) RATS/CTD497 (1) RATS/CTD499 (1) RATS/CTD501 (1) RATS/CTD503 (1) RATS/CTD505 (1) RATS/CTD507 (1) RATS/CTD509 (1) RATS/CTD51 (1) RATS/CTD511 (1) RATS/CTD513 (1) RATS/CTD515 (1) RATS/CTD517 (1) RATS/CTD519 (1) RATS/CTD521 (1) RATS/CTD523 (1) RATS/CTD525 (1) RATS/CTD527 (1) RATS/CTD529 (1) RATS/CTD53 (1) RATS/CTD531 (1) RATS/CTD534 (1) RATS/CTD536 (1) RATS/CTD538 (1) RATS/CTD540 (1) RATS/CTD542 (1) RATS/CTD545 (1) RATS/CTD547 (1) RATS/CTD549 (1) RATS/CTD55 (1) RATS/CTD551 (1) RATS/CTD553 (1) RATS/CTD555 (1) RATS/CTD557 (1) RATS/CTD559 (1) RATS/CTD561 (1) RATS/CTD563 (1) RATS/CTD565 (1) RATS/CTD567 (1) RATS/CTD569 (1) RATS/CTD571 (1) RATS/CTD573 (1) RATS/CTD575 (1) RATS/CTD577 (1) RATS/CTD579 (1) RATS/CTD58 (1) RATS/CTD581 (1) RATS/CTD583 (1) RATS/CTD585 (1) RATS/CTD587 (1) RATS/CTD589 (1) RATS/CTD591 (1) RATS/CTD593 (1) RATS/CTD595 (1) RATS/CTD597 (1) RATS/CTD599 (1) RATS/CTD60 (1) RATS/CTD601 (1) RATS/CTD603 (1) RATS/CTD605 (1) RATS/CTD607 (1) RATS/CTD609 (1) RATS/CTD611 (1) RATS/CTD613 (1) RATS/CTD615 (1) RATS/CTD617 (1) RATS/CTD619 (1) RATS/CTD62 (1) RATS/CTD621 (1) RATS/CTD623 (1) RATS/CTD625 (1) RATS/CTD627 (1) RATS/CTD629 (1) RATS/CTD631 (1) RATS/CTD633 (1) RATS/CTD635 (1) RATS/CTD637 (1) RATS/CTD639 (1) RATS/CTD64 (1) RATS/CTD654 (1) RATS/CTD66 (1) RATS/CTD669 (1) RATS/CTD678 (1) RATS/CTD68 (1) RATS/CTD687 (1) RATS/CTD695 (1) RATS/CTD70 (1) RATS/CTD705 (1) RATS/CTD72 (1) RATS/CTD722 (1) RATS/CTD724 (1) RATS/CTD727 (1) RATS/CTD729 (1) RATS/CTD731 (1) RATS/CTD733 (1) RATS/CTD735 (1) RATS/CTD737 (1) RATS/CTD739 (1) RATS/CTD74 (1) RATS/CTD741 (1) RATS/CTD743 (1) RATS/CTD745 (1) RATS/CTD747 (1) RATS/CTD749 (1) RATS/CTD751 (1) RATS/CTD753 (1) RATS/CTD755 (1) RATS/CTD757 (1) RATS/CTD759 (1) RATS/CTD761 (1) RATS/CTD763 (1) RATS/CTD765 (1) RATS/CTD767 (1) RATS/CTD77 (1) RATS/CTD771 (1) RATS/CTD773 (1) RATS/CTD775 (1) RATS/CTD777 (1) RATS/CTD779 (1) RATS/CTD781 (1) RATS/CTD783 (1) RATS/CTD785 (1) RATS/CTD787 (1) RATS/CTD789 (1) RATS/CTD795 (1) RATS/CTD797 (1) RATS/CTD799 (1) RATS/CTD80 (1) RATS/CTD801 (1) RATS/CTD803 (1) RATS/CTD805 (1) RATS/CTD807 (1) RATS/CTD809 (1) RATS/CTD811 (1) RATS/CTD813 (1) RATS/CTD817 (1) RATS/CTD819 (1) RATS/CTD82 (1) RATS/CTD821 (1) RATS/CTD823 (1) RATS/CTD825 (1) RATS/CTD827 (1) RATS/CTD829 (1) RATS/CTD831 (1) RATS/CTD833 (1) RATS/CTD837 (1) RATS/CTD839 (1) RATS/CTD84 (1) RATS/CTD841 (1) RATS/CTD843 (1) RATS/CTD845 (1) RATS/CTD847 (1) RATS/CTD849 (1) RATS/CTD851 (1) RATS/CTD853 (1) RATS/CTD855 (1) RATS/CTD857 (1) RATS/CTD859 (1) RATS/CTD861 (1) RATS/CTD863 (1) RATS/CTD865 (1) RATS/CTD867 (1) RATS/CTD869 (1) RATS/CTD87 (1) RATS/CTD871 (1) RATS/CTD873 (1) RATS/CTD879 (1) RATS/CTD881 (1) RATS/CTD883 (1) RATS/CTD885 (1) RATS/CTD887 (1) RATS/CTD889 (1) RATS/CTD89 (1) RATS/CTD891 (1) RATS/CTD893 (1) RATS/CTD895 (1) RATS/CTD897 (1) RATS/CTD899 (1) RATS/CTD901 (1) RATS/CTD903 (1) RATS/CTD905 (1) RATS/CTD907 (1) RATS/CTD909 (1) RATS/CTD91 (1) RATS/CTD913 (1) RATS/CTD915 (1) RATS/CTD917 (1) RATS/CTD919 (1) RATS/CTD921 (1) RATS/CTD923 (1) RATS/CTD925 (1) RATS/CTD927 (1) RATS/CTD929 (1) RATS/CTD93 (1) RATS/CTD931 (1) RATS/CTD933 (1) RATS/CTD935 (1) RATS/CTD937 (1) RATS/CTD939 (1) RATS/CTD941 (1) RATS/CTD943 (1) RATS/CTD945 (1) RATS/CTD947 (1) RATS/CTD949 (1) RATS/CTD951 (1) RATS/CTD953 (1) RATS/CTD955 (1) RATS/CTD957 (1) RATS/CTD959 (1) RATS/CTD96 (1) RATS/CTD961 (1) RATS/CTD963 (1) RATS/CTD965 (1) RATS/CTD967 (1) RATS/CTD969 (1) RATS/CTD971 (1) RATS/CTD973 (1) RATS/CTD975 (1) RATS/CTD977 (1) RATS/CTD979 (1) RATS/CTD98 (1) RATS/CTD981 (1) RATS/CTD983 (1) RATS/CTD985 (1) RATS/CTD987 (1) RATS/CTD989 (1) RATS/CTD991 (1)
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 |