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in_situ_record_schema.json
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{
"$schema": "http://json-schema.org/draft-07/schema#",
"title": "Cloud-based Data Match-Up Service In Situ Schema",
"description": "Description for each variable is copied from CF standard names table found at https://cfconventions.org/Data/cf-standard-names/77/build/cf-standard-name-table.html",
"type": "object",
"additionalProperties": false,
"properties": {
"time": {
"description": "Time of the observation",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0115/",
"type": "string",
"format": "date-time"
},
"latitude": {
"description": "Latitude position of the observation",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0600/",
"type": "number",
"minimum": -90,
"maximum": 90
},
"longitude": {
"description": "Longitude position of the observation",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0554/",
"type": "number",
"minimum": -180,
"maximum": 180
},
"depth": {
"description": "Depth value of the observation with below sea level being represented as positive values and -99999 as unknown",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0721/",
"type": "number"
},
"air_pressure": {
"description": "Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0015/",
"type": "number",
"units": "hPa"
},
"air_pressure_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"air_temperature": {
"description": "Air temperature is the bulk temperature of the air, not the surface (skin) temperature.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0023/",
"type": "number",
"units": "C"
},
"air_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"dew_point_temperature": {
"description": "Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0723/",
"type": "number",
"units": "C"
},
"dew_point_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"downwelling_longwave_flux_in_air": {
"description": "Downwelling radiation is radiation from above. It does not mean \"net downward\". The sign convention is that \"upwelling\" is positive upwards and \"downwelling\" is positive downwards. The term \"longwave\" means longwave radiation. When thought of as being incident on a surface, a radiative flux is sometimes called \"irradiance\". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called \"vector irradiance\". In accordance with common usage in geophysical disciplines, \"flux\" implies per unit area, called \"flux density\" in physics.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0699/",
"type": "number",
"units": "W m-2"
},
"downwelling_longwave_flux_in_air_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"downwelling_longwave_radiance_in_air": {
"description": "Downwelling radiation is radiation from above. It does not mean \"net downward\". The sign convention is that \"upwelling\" is positive upwards and \"downwelling\" is positive downwards. The term \"longwave\" means longwave radiation. Radiance is the radiative flux in a particular direction, per unit of solid angle. The direction from which it is coming must be specified, for instance with a coordinate of zenith_angle. If the radiation does not depend on direction, a standard name of isotropic radiance should be chosen instead.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0672/",
"type": "number",
"units": "W m-2 sr-1"
},
"downwelling_longwave_radiance_in_air_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"downwelling_shortwave_flux_in_air": {
"description": "Downwelling radiation is radiation from above. It does not mean \"net downward\". The sign convention is that \"upwelling\" is positive upwards and \"downwelling\" is positive downwards. The term \"shortwave\" means shortwave radiation. When thought of as being incident on a surface, a radiative flux is sometimes called \"irradiance\". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called \"vector irradiance\". In accordance with common usage in geophysical disciplines, \"flux\" implies per unit area, called \"flux density\" in physics.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0660/",
"type": "number",
"units": "W m-2"
},
"downwelling_shortwave_flux_in_air_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"mass_concentration_of_chlorophyll_in_sea_water": {
"description": "Mass concentration means mass per unit volume and is used in the construction mass_concentration_of_X_in_Y, where X is a material constituent of Y. A chemical species denoted by X may be described by a single term such as \"nitrogen\" or a phrase such as \"nox_expressed_as_nitrogen\". Chlorophylls are the green pigments found in most plants, algae and cyanobacteria; their presence is essential for photosynthesis to take place. There are several different forms of chlorophyll that occur naturally. All contain a chlorin ring (chemical formula C20H16N4) which gives the green pigment and a side chain whose structure varies. The naturally occurring forms of chlorophyll contain between 35 and 55 carbon atoms.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CF12S21/",
"type": "number",
"units": "kg m-3"
},
"mass_concentration_of_chlorophyll_in_sea_water_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"rainfall_rate": {
"description": "",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0410/",
"type": "number",
"units": "m s-1"
},
"rainfall_rate_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"relative_humidity": {
"description": "",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0413/",
"type": "number",
"units": "1"
},
"relative_humidity_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_surface_salinity": {
"description": "Sea surface salinity is the salt content of sea water close to the sea surface, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. Sea surface salinity is often abbreviated as \"SSS\". For the salinity of sea water at a particular depth or layer, a data variable of \"sea_water_salinity\" or one of the more precisely defined salinities should be used with a vertical coordinate axis. There are standard names for the precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s. Conversion of data between the observed scales follows: S_P = (S_K - 0.03) * (1.80655 / 1.805) and S_P = S_C, however the accuracy of the latter is dependent on whether chlorinity or conductivity was used to determine the S_C value, with this inconsistency driving the development of PSS-78. The more precise standard names should be used where appropriate for both modelled and observed salinities. In particular, the use of sea_water_salinity to describe salinity observations made from 1978 onwards is now deprecated in favor of the term sea_water_practical_salinity which is the salinity quantity stored by national data centers for post-1978 observations. The only exception to this is where the observed salinities are definitely known not to be recorded on the Practical Salinity Scale. The unit \"parts per thousand\" was used for sea_water_knudsen_salinity and sea_water_cox_salinity.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0376/",
"type": "number",
"units": "1e-3"
},
"sea_surface_salinity_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_surface_skin_temperature": {
"description": "The sea surface skin temperature is the temperature measured by an infrared radiometer typically operating at wavelengths in the range 3.7 - 12 micrometers. It represents the temperature within the conductive diffusion-dominated sub-layer at a depth of approximately 10 - 20 micrometers below the air-sea interface. Measurements of this quantity are subject to a large potential diurnal cycle including cool skin layer effects (especially at night under clear skies and low wind speed conditions) and warm layer effects in the daytime.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFV9N2/",
"type": "number",
"units": "C"
},
"sea_surface_skin_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_surface_subskin_temperature": {
"description": "The sea surface subskin temperature is the temperature at the base of the conductive laminar sub-layer of the ocean surface, that is, at a depth of approximately 1 - 1.5 millimeters below the air-sea interface. For practical purposes, this quantity can be well approximated to the measurement of surface temperature by a microwave radiometer operating in the 6 - 11 gigahertz frequency range, but the relationship is neither direct nor invariant to changing physical conditions or to the specific geometry of the microwave measurements. Measurements of this quantity are subject to a large potential diurnal cycle due to thermal stratification of the upper ocean layer in low wind speed high solar irradiance conditions.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFV9N3/",
"type": "number",
"units": "C"
},
"sea_surface_subskin_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_surface_temperature": {
"description": "Sea surface temperature is usually abbreviated as \"SST\". It is the temperature of sea water near the surface (including the part under sea-ice, if any). More specific terms, namely sea_surface_skin_temperature, sea_surface_subskin_temperature, and surface_temperature are available for the skin, subskin, and interface temperature. respectively. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0381/",
"type": "number",
"units": "C"
},
"sea_surface_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_water_density": {
"description": "Sea water density is the in-situ density (not the potential density). If 1000 kg m-3 is subtracted, the standard name sea_water_sigma_t should be chosen instead.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0393/",
"type": "number",
"units": "kg m-3"
},
"sea_water_density_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_water_electrical_conductivity": {
"description": "",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0394/",
"type": "number",
"units": "S m-1"
},
"sea_water_electrical_conductivity_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_water_practical_salinity": {
"description": "Practical Salinity, S_P, is a determination of the salinity of sea water, based on its electrical conductance. The measured conductance, corrected for temperature and pressure, is compared to the conductance of a standard potassium chloride solution, producing a value on the Practical Salinity Scale of 1978 (PSS-78). This name should not be used to describe salinity observations made before 1978, or ones not based on conductance measurements. Conversion of Practical Salinity to other precisely defined salinity measures should use the appropriate formulas specified by TEOS-10. Other standard names for precisely defined salinity quantities are sea_water_absolute_salinity (S_A); sea_water_preformed_salinity (S_*), sea_water_reference_salinity (S_R); sea_water_cox_salinity (S_C), used for salinity observations between 1967 and 1977; and sea_water_knudsen_salinity (S_K), used for salinity observations between 1901 and 1966. Salinity quantities that do not match any of the precise definitions should be given the more general standard name of sea_water_salinity. Reference: www.teos-10.org; Lewis, 1980 doi:10.1109/JOE.1980.1145448.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/IADIHDIJ/",
"type": "number",
"units": "1"
},
"sea_water_practical_salinity_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_water_salinity": {
"description": "Sea water salinity is the salt content of sea water, often on the Practical Salinity Scale of 1978. However, the unqualified term 'salinity' is generic and does not necessarily imply any particular method of calculation. The units of salinity are dimensionless and the units attribute should normally be given as 1e-3 or 0.001 i.e. parts per thousand. There are standard names for the more precisely defined salinity quantities: sea_water_knudsen_salinity, S_K (used for salinity observations between 1901 and 1966), sea_water_cox_salinity, S_C (used for salinity observations between 1967 and 1977), sea_water_practical_salinity, S_P (used for salinity observations from 1978 to the present day), sea_water_absolute_salinity, S_A, sea_water_preformed_salinity, S_*, and sea_water_reference_salinity. Practical Salinity is reported on the Practical Salinity Scale of 1978 (PSS-78), and is usually based on the electrical conductivity of sea water in observations since the 1960s. Conversion of data between the observed scales follows: S_P = (S_K - 0.03) * (1.80655 / 1.805) and S_P = S_C, however the accuracy of the latter is dependent on whether chlorinity or conductivity was used to determine the S_C value, with this inconsistency driving the development of PSS-78. The more precise standard names should be used where appropriate for both modelled and observed salinities. In particular, the use of sea_water_salinity to describe salinity observations made from 1978 onwards is now deprecated in favor of the term sea_water_practical_salinity which is the salinity quantity stored by national data centers for post-1978 observations. The only exception to this is where the observed salinities are definitely known not to be recorded on the Practical Salinity Scale. The unit \"parts per thousand\" was used for sea_water_knudsen_salinity and sea_water_cox_salinity.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0331/",
"type": "number",
"units": "1e-3"
},
"sea_water_salinity_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"sea_water_temperature": {
"description": "Sea water temperature is the in situ temperature of the sea water. To specify the depth at which the temperature applies use a vertical coordinate variable or scalar coordinate variable. There are standard names for sea_surface_temperature, sea_surface_skin_temperature, sea_surface_subskin_temperature and sea_surface_foundation_temperature which can be used to describe data located at the specified surfaces. For observed data, depending on the period during which the observation was made, the measured in situ temperature was recorded against standard \"scales\". These historical scales include the International Practical Temperature Scale of 1948 (IPTS-48; 1948-1967), the International Practical Temperature Scale of 1968 (IPTS-68, Barber, 1969; 1968-1989) and the International Temperature Scale of 1990 (ITS-90, Saunders 1990; 1990 onwards). Conversion of data between these scales follows t68 = t48 - (4.4 x 10e-6) * t48(100 - t - 48); t90 = 0.99976 * t68. Observations made prior to 1948 (IPTS-48) have not been documented and therefore a conversion cannot be certain. Differences between t90 and t68 can be up to 0.01 at temperatures of 40 C and above; differences of 0.002-0.007 occur across the standard range of ocean temperatures (-10 - 30 C). The International Equation of State of Seawater 1980 (EOS-80, UNESCO, 1981) and the Practical Salinity Scale (PSS-78) were both based on IPTS-68, while the Thermodynamic Equation of Seawater 2010 (TEOS-10) is based on ITS-90. References: Barber, 1969, doi: 10.1088/0026-1394/5/2/001; UNESCO, 1981; Saunders, 1990, WOCE Newsletter, 10, September 1990.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0335/",
"type": "number",
"units": "C"
},
"sea_water_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"surface_downwelling_photosynthetic_photon_flux_in_air": {
"description": "The surface called \"surface\" means the lower boundary of the atmosphere. Downwelling radiation is radiation from above. It does not mean \"net downward\". The sign convention is that \"upwelling\" is positive upwards and \"downwelling\" is positive downwards. \"Photosynthetic\" radiation is the part of the spectrum which is used in photosynthesis e.g. 400-700 nm. The range of wavelengths could be specified precisely by the bounds of a coordinate of radiation_wavelength. A photon flux is specified in terms of numbers of photons expressed in moles. In accordance with common usage in geophysical disciplines, \"flux\" implies per unit area, called \"flux density\" in physics.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0284/",
"type": "number",
"units": "mol m-2 s-1"
},
"surface_downwelling_photosynthetic_photon_flux_in_air_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"wet_bulb_temperature": {
"description": "",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0035/",
"type": "number",
"units": "C"
},
"wet_bulb_temperature_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"wind_speed": {
"description": "Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0038/",
"type": "number",
"units": "m s-1"
},
"wind_speed_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"wind_from_direction": {
"description": "Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) In meteorological reports, the direction of the wind vector is usually (but not always) given as the direction from which it is blowing (wind_from_direction) (westerly, northerly, etc.). In other contexts, such as atmospheric modelling, it is often natural to give the direction in the usual manner of vectors as the heading or the direction to which it is blowing (wind_to_direction) (eastward, southward, etc.) \"from_direction\" is used in the construction X_from_direction and indicates the direction from which the velocity vector of X is coming.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0036/",
"type": "number",
"units": "degree"
},
"wind_to_direction": {
"description": "Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) In meteorological reports, the direction of the wind vector is usually (but not always) given as the direction from which it is blowing (wind_from_direction) (westerly, northerly, etc.). In other contexts, such as atmospheric modelling, it is often natural to give the direction in the usual manner of vectors as the heading or the direction to which it is blowing (wind_to_direction) (eastward, southward, etc.) \"to_direction\" is used in the construction X_to_direction and indicates the direction towards which the velocity vector of X is headed. The direction is a bearing in the usual geographical sense, measured positive clockwise from due north.",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0041/",
"type": "number",
"units": "degree"
},
"wind_from_direction_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"wind_to_direction_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"eastward_wind": {
"description": "\"Eastward\" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0653/",
"type": "number",
"units": "m s-1"
},
"northward_wind": {
"description": "\"Northward\" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)",
"uri": "http://vocab.nerc.ac.uk/collection/P07/current/CFSN0461/",
"type": "number",
"units": "m s-1"
},
"wind_component_quality": {
"description": "",
"$ref": "#/definitions/quality"
},
"platform": {
"description": "",
"$ref": "#/definitions/platform"
},
"device": {
"description": "Device identifier is provided by the Natural Environment Research Council (NERC) Vocabulary Server developed and maintained by the British Oceanographic Data Centre and can be found at http://vocab.nerc.ac.uk/collection/L05/current/",
"type": "string",
"oneOf": [
{
"const": "364",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/364/",
"title": "1000 Hz top-bandwidth multi-channel seismic reflection systems"
},
{
"const": "363",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/363/",
"title": "1000 Hz top-bandwidth single-channel seismic reflection systems"
},
{
"const": "365",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/365/",
"title": "2000 Hz top-bandwidth multi-channel seismic reflection systems"
},
{
"const": "372",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/372/",
"title": "2000 Hz top-bandwidth single-channel seismic reflection systems"
},
{
"const": "375",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/375/",
"title": "250 Hz top-bandwidth multi-channel seismic reflection systems"
},
{
"const": "362",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/362/",
"title": "250 Hz top-bandwidth single-channel seismic reflection systems"
},
{
"const": "374",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/374/",
"title": "60 Hz top-bandwidth multi-channel seismic reflection systems"
},
{
"const": "371",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/371/",
"title": "60 Hz top-bandwidth single-channel seismic reflection systems"
},
{
"const": "366",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/366/",
"title": ">2000 Hz top-bandwidth multi-channel seismic reflection systems"
},
{
"const": "373",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/373/",
"title": ">2000 Hz top-bandwidth single-channel seismic reflection systems"
},
{
"const": "367",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/367/",
"title": ">2000 Hz top-bandwidth sub-bottom penetrator and mud profiler systems"
},
{
"const": "384",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/384/",
"title": "ADVs and turbulence probes"
},
{
"const": "386",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/386/",
"title": "Aerosol physical characterisers"
},
{
"const": "387",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/387/",
"title": "Aethalometers"
},
{
"const": "AQPL",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/AQPL/",
"title": "Aquapulse"
},
{
"const": "POS16",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS16/",
"title": "Argos GPS-localised transmitters"
},
{
"const": "POS17",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS17/",
"title": "Argos doppler-localised transmitters"
},
{
"const": "MOD03",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD03/",
"title": "Atmosphere models"
},
{
"const": "314",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/314/",
"title": "Atmospheric chemistry remote sensors"
},
{
"const": "LAB49",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB49/",
"title": "Atomic fluorescence spectrometers"
},
{
"const": "POS10",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS10/",
"title": "Automatic Ranging Grid Overlay DM 54 receivers"
},
{
"const": "MOD08",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD08/",
"title": "Biological and biogeochemical models"
},
{
"const": "BOMR",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/BOMR/",
"title": "Boomer"
},
{
"const": "130",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/130/",
"title": "CTD"
},
{
"const": "131",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/131/",
"title": "CTD undulators"
},
{
"const": "CHRP",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/CHRP/",
"title": "Chirp"
},
{
"const": "COLCMP",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/COLCMP/",
"title": "Colour comparators"
},
{
"const": "MOD05",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD05/",
"title": "Coupled models"
},
{
"const": "POS08",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS08/",
"title": "Decca Navigator System HiFix receivers"
},
{
"const": "POS01",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS01/",
"title": "Decca Navigator System main chain receivers"
},
{
"const": "POS04",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS04/",
"title": "Differential Global Positioning System receivers"
},
{
"const": "389",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/389/",
"title": "Expendable bathythermographs"
},
{
"const": "FFES",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/FFES/",
"title": "Fish-finder echosounders"
},
{
"const": "FLXS",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/FLXS/",
"title": "Flexichoc"
},
{
"const": "FLXT",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/FLXT/",
"title": "Flexotir"
},
{
"const": "GIAG",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/GIAG/",
"title": "GI-gun"
},
{
"const": "LAB39",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB39/",
"title": "Geiger counters"
},
{
"const": "POS02",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS02/",
"title": "Global Navigation Satellite System receivers"
},
{
"const": "MOD01",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD01/",
"title": "Global models"
},
{
"const": "POS21",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS21/",
"title": "Hyperfix receivers"
},
{
"const": "POS25",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS25/",
"title": "Kinematic Global Positioning System receivers"
},
{
"const": "LVLST",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LVLST/",
"title": "Levels and staffs"
},
{
"const": "POS05",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS05/",
"title": "Long Range Navigation version C receivers"
},
{
"const": "POS06",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS06/",
"title": "Marine chronometers"
},
{
"const": "390",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/390/",
"title": "Mechanical bathythermographs"
},
{
"const": "MOD06",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD06/",
"title": "Meteorological models"
},
{
"const": "POS20",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS20/",
"title": "Motorola Mini-Ranger receivers"
},
{
"const": "POS03",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS03/",
"title": "NAVSTAR Global Positioning System receivers"
},
{
"const": "POS18",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS18/",
"title": "Navy Navigation Satellite System receivers"
},
{
"const": "MOD04",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD04/",
"title": "Ocean models"
},
{
"const": "POS15",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS15/",
"title": "Omega receivers"
},
{
"const": "PERMON",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/PERMON/",
"title": "Performance monitors"
},
{
"const": "MOD07",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD07/",
"title": "Physical oceanographic models"
},
{
"const": "394",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/394/",
"title": "Pinger sub-bottom profilers"
},
{
"const": "POS14",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS14/",
"title": "Pulse8 receivers"
},
{
"const": "POS13",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS13/",
"title": "Rana receivers"
},
{
"const": "MOD02",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/MOD02/",
"title": "Regional models"
},
{
"const": "POS07",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS07/",
"title": "Sextants"
},
{
"const": "SPRK",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/SPRK/",
"title": "Sparker"
},
{
"const": "POS12",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS12/",
"title": "Syst\ufffdme leger de measure de distance receivers"
},
{
"const": "POS09",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS09/",
"title": "Toran receivers"
},
{
"const": "POS11",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS11/",
"title": "Trident receivers"
},
{
"const": "POS22",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS22/",
"title": "Trisponder navigation systems"
},
{
"const": "POS26",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS26/",
"title": "Ultra Short Baseline Positioning Systems"
},
{
"const": "VSHC",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/VSHC/",
"title": "Vaporchoc"
},
{
"const": "LAB40",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB40/",
"title": "Volume measures"
},
{
"const": "WDRG",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/WDRG/",
"title": "Wire drags"
},
{
"const": "LAB26",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB26/",
"title": "X-ray diffractometers"
},
{
"const": "LAB25",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB25/",
"title": "X-ray fluorescence analysers"
},
{
"const": "LAB17",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB17/",
"title": "accelerator mass spectrometers"
},
{
"const": "307",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/307/",
"title": "accelerometers"
},
{
"const": "183",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/183/",
"title": "acoustic backscatter sensors"
},
{
"const": "357",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/357/",
"title": "acoustic tracking systems"
},
{
"const": "LAB32",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB32/",
"title": "acoustic velocity systems"
},
{
"const": "64",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/64/",
"title": "active fishing gear"
},
{
"const": "353",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/353/",
"title": "active fluorometers"
},
{
"const": "13",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/13/",
"title": "aerosol samplers"
},
{
"const": "SNAG",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/SNAG/",
"title": "airgun"
},
{
"const": "ARAG",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/ARAG/",
"title": "airgun array"
},
{
"const": "379",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/379/",
"title": "altimeters"
},
{
"const": "101",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/101/",
"title": "anemometers"
},
{
"const": "382",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/382/",
"title": "atmospheric gas analysers"
},
{
"const": "308",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/308/",
"title": "atmospheric radiometers"
},
{
"const": "ATRANS",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/ATRANS/",
"title": "atmospheric transparency quantifiers"
},
{
"const": "LAB10",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB10/",
"title": "atomic absorption spectrometers"
},
{
"const": "LAB04",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB04/",
"title": "autoanalysers"
},
{
"const": "LAB13",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB13/",
"title": "balances and scales"
},
{
"const": "312",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/312/",
"title": "bathymetric LiDARs"
},
{
"const": "132",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/132/",
"title": "bathythermographs"
},
{
"const": "62",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/62/",
"title": "beam trawls"
},
{
"const": "LAB23",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB23/",
"title": "bench fluorometers"
},
{
"const": "LAB27",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB27/",
"title": "bench particle sizers"
},
{
"const": "151",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/151/",
"title": "benthic incubation chambers"
},
{
"const": "24",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/24/",
"title": "benthos samplers"
},
{
"const": "393",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/393/",
"title": "binoculars and terrestrial scopes"
},
{
"const": "BLUMS",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/BLUMS/",
"title": "bioluminescence sensors"
},
{
"const": "85",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/85/",
"title": "biorectors and chemostats"
},
{
"const": "313",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/313/",
"title": "bird detection radars"
},
{
"const": "358",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/358/",
"title": "bubble detectors"
},
{
"const": "311",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/311/",
"title": "cameras"
},
{
"const": "LAB38",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB38/",
"title": "cavity enhanced absorption spectrometers"
},
{
"const": "83",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/83/",
"title": "centrifuges"
},
{
"const": "LAB34",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB34/",
"title": "chemiluminescence analysers"
},
{
"const": "CCOV",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/CCOV/",
"title": "cloud cover quantifiers"
},
{
"const": "392",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/392/",
"title": "colonisation substrata"
},
{
"const": "LAB03",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB03/",
"title": "colorimeters"
},
{
"const": "58",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/58/",
"title": "continuous air samplers"
},
{
"const": "31",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/31/",
"title": "continuous water samplers"
},
{
"const": "CSEM",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/CSEM/",
"title": "controlled-source electromagnetic systems"
},
{
"const": "114",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/114/",
"title": "current meters"
},
{
"const": "115",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/115/",
"title": "current profilers"
},
{
"const": "DLOG",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/DLOG/",
"title": "data loggers"
},
{
"const": "POS24",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/POS24/",
"title": "dead reckoning"
},
{
"const": "61",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/61/",
"title": "demersal trawl nets"
},
{
"const": "11",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/11/",
"title": "discrete air samplers"
},
{
"const": "30",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/30/",
"title": "discrete water samplers"
},
{
"const": "351",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/351/",
"title": "dissolved gas sensors"
},
{
"const": "ERTQ",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/ERTQ/",
"title": "earthquake"
},
{
"const": "EMSR",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/EMSR/",
"title": "electromagnetic sensors"
},
{
"const": "LAB08",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB08/",
"title": "electron microprobes"
},
{
"const": "LAB07",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB07/",
"title": "electron microscopes"
},
{
"const": "LAB01",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB01/",
"title": "elemental analysers"
},
{
"const": "EQUIL",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/EQUIL/",
"title": "equilibrators"
},
{
"const": "354",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/354/",
"title": "expendable CTDs"
},
{
"const": "70",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/70/",
"title": "fish aggregating devices"
},
{
"const": "LAB37",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB37/",
"title": "flow cytometers"
},
{
"const": "LAB36",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB36/",
"title": "flow injection analysers"
},
{
"const": "388",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/388/",
"title": "flow meters"
},
{
"const": "LAB06",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB06/",
"title": "fluorescence microscopes"
},
{
"const": "113",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/113/",
"title": "fluorometers"
},
{
"const": "66",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/66/",
"title": "flushing drills"
},
{
"const": "12",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/12/",
"title": "fog samplers"
},
{
"const": "LAB22",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB22/",
"title": "gamma-ray spectrometers"
},
{
"const": "LAB19",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB19/",
"title": "gas chromatograph mass spectrometers"
},
{
"const": "LAB02",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB02/",
"title": "gas chromatographs"
},
{
"const": "LAB24",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB24/",
"title": "gel permeation chromatographs"
},
{
"const": "370",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/370/",
"title": "geothermometers"
},
{
"const": "65",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/65/",
"title": "gill nets"
},
{
"const": "158",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/158/",
"title": "gravimeters"
},
{
"const": "EXLH",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/EXLH/",
"title": "high penetration low resolution explosives"
},
{
"const": "LAB11",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/LAB11/",
"title": "high performance liquid chromatographs"
},
{
"const": "EXHL",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/EXHL/",
"title": "high resolution low penetration explosives"
},
{
"const": "67",
"uri": "http://vocab.nerc.ac.uk/collection/L05/current/67/",
"title": "high-speed plankton samplers"