Get a list of ProcedureComputation objects. ProcedureComputations have a 1:1 mapping with Observations where used.
These may have a number of 2 or more components made up of combinations of Computation and Acquisition records.
The details of the underlying records have been serialised.

### Available end points:

- `/ProcedureComputations/` - Will list all ProcedureComputations in the database
- `/ProcedureComputations.json` - Will return all ProcedureComputations in json format
- `/ProcedureComputations/<object_id>/` - Returns ProcedureComputations object with that id

### Available Methods:

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### How to use filters:

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GET /api/v2/composites/?format=api&offset=500
HTTP 200 OK
Allow: GET, HEAD, OPTIONS
Content-Type: application/json
Vary: Accept

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            "ob_id": 38837,
            "computationComponent": [
                {
                    "ob_id": 38838,
                    "uuid": "83b75e6d88a2425cbb13909b5afd7a57",
                    "title": "Level 2 Formaldehyde (HCHO) total column processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "The general method used for the derivation of HCHO VCDs from UV spectral measurements is the Differential Optical Absorption Spectroscopy method (DOAS; Platt and Stutz, 2008) which involves two main steps. First, the effective slant column amount (corresponding to the integrated HCHO concentration along the mean atmospheric optical path: Ns) is derived through a least-squares fit of the measured Earth reflectance spectrum by laboratory absorption cross-sections and a low order polynomial. Subsequently, a correction is applied to the slant column values to correct for appearing biases that may be of known or unknown origin. Finally, slant columns are converted into vertical columns by means of air mass factors (AMF) obtained from suitable radiative transfer calculations, accounting for the presence of clouds, surface properties, and best-guess HCHO vertical profiles.\r\n\r\nIn the UV, the sensitivity to HCHO concentrations in the boundary layer is intrinsically limited from space due to the combined effect of Rayleigh and Mie scattering that limits the radiation fraction scattered back toward the satellite. In addition, ozone absorption reduces the number of photons that reaches the lowest atmospheric layers. Furthermore, the absorption signatures of HCHO are weaker than those of other UV Vis absorbers, such as e.g. NO2. As a result, the retrieval of formaldehyde from space is noise sensitive and error prone. While the precision (or random error uncertainty) is driven by the signal to noise ratio of the recorded spectra and by the width of the retrieval interval, the trueness (or systematic error uncertainty) is limited by the current knowledge of the external parameters needed in the different retrieval steps.\r\n\r\nThe selection of the optimal retrieval interval must maximize the sensitivity of the inversion to the HCHO absorption signatures while minimizing errors from geophysical and instrument related spectral features. The retrieval interval should be chosen as wide as possible to maximize the number of sampling points while avoiding overlap with strong atmospheric spectral features from interfering species (mainly O3, BrO, and O4). The DOAS algorithm intrinsically assumes that the atmosphere is optically thin so that the optical light path is independent of wavelength within the fitting window. Hence the method is accurate only for modest ozone absorption (i.e., for small to medium solar zenith angles). Generally, the effect of ozone misfit on the retrieval can be handled by introducing wavelength dependent-AMF in the fit, and by applying appropriate background corrections on the columns. The correlation with BrO absorption can be reduced by using two different wavelength intervals to fit BrO and HCHO (see section 5.3: Formaldehyde slant column retrieval).\r\n\r\nThe Sentinel-5P sensor TROPOMI samples the Earth’s surface with a revisit time of one day and with an unprecedented spatial resolution of 7x3.5 km2 (5.5x3.5 km2 from 6 August 2019). Furthermore, the signal to noise ratio of TROPOMI is required to be equivalent to OMI in the UV-Visible range. This allows the resolution of fine details and S5P will arguably be a valuable tool to better study NMVOC emissions. Nevertheless, it poses additional constraints on the retrieval code for several reasons:\r\n1. Computational speed: the Level 1b data flow delivers spectral measurements for band 3 with a size of 4 gigabytes per orbit (15 orbits daily).\r\n2. Precision: given the required signal to noise ratio of measured spectra, the air quality requirements for HCHO [RD04] will not be met for individual ground pixels. Spatial and temporal averages of the HCHO columns will have to be considered in order to provide useful constraints on human and natural NMVOC emissions.\r\n3. Trueness: currently, the spatial resolution of global-scale external parameters needed in the AMF calculation (e.g. albedo or a priori HCHO profiles) is much coarser than the resolution of TROPOMI. This introduces errors in the final vertical columns, mostly for coastal regions and localized sources (Heckel et al., 2011) \r\n\r\nTo fully exploit the potential of satellite data, applications relying on tropospheric HCHO observations require high quality long-term time series, provided with well characterized errors and averaging kernels, and consistently retrieved from the different sensors. Furthermore, as the HCHO observations are aimed to be used synergistically with other species observations (e.g. for air quality applications), it is essential to homogenize as far as possible the retrieval methods as well as the external databases, in order to minimize systematic biases between the observations.",
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                            "ob_id": 11891,
                            "platform": "https://api.catalogue.ceda.ac.uk/api/v2/platforms/26439/?format=api",
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            "computationComponent": [
                {
                    "ob_id": 38859,
                    "uuid": "87fe4f2cf868471d87a3a843cde2f667",
                    "title": "Level 2 processing algorithm applied to Sentinel 3 Ocean and Land Colour Instrument (OLCI) raw data",
                    "abstract": "In addition, a common pre-processing and product formatting process aims to read, check the input, and define and write the outputs.\r\n\r\nIt is important to note that, for each geophysical parameter included in the OLCI Level-2 product, a switch has been defined in the OLCI Level-2 configuration file. Each parameter and its associated flags are produced only if the associated switch is set to '1'. As a consequence, the module generating each parameter is triggered only if the appropriate switch is set to '1'.\r\n\r\nThe pre-processing module, starting from the Level-1B TOA radiances, derives reflectances corrected for gaseous absorption. The consolidation of pixel classifications from Level-1B and the definition of water vapour retrieval are included in this module.\r\n\r\nThe algorithm is divided into five successive steps:\r\n\r\n1. The conversion from radiances to reflectances step-checks the Level-1B products and converts radiances into reflectances (also known as first instrumental correction).\r\n2. To be correctly taken into account or to be rejected from the algorithm, pixels have to be differentiated according to four criteria: cloud, land, water and invalid pixels. The first pixel classification focuses on identification of cloudy pixels. This Cloud masking will be improved in the frame of coming evolutions, including the improvement tested and validated during the MERIS 4th reprocessing.\r\n3. Gaseous correction: correcting reflectances for gaseous absorption (i.e. O2, H2O and O3). Five OLCI bands are dedicated to this correction and are not used after this step: Oa13 to Oa15, Oa19 and Oa20.\r\n4. The second-pixel classification estimates glint reflectance and completes pixel classification starting at the second step by consolidating the classification of land and water pixels.\r\n5. The water vapour process retrieves atmospheric water vapour content from clear sky pixels.\r\n\r\nThe land processing module consists of two independent sections (one for each product):\r\n\r\n1. The Green Instantaneous Fraction of Absorbed Photosynthetically Active Radiation (GI-FAPAR) section combines the information contained in the blue band with that contained in the bands at 681 and 865 nm to generate \"rectified channels\" at these latter two wavelengths.\r\n2. The OLCI Terrestrial Chlorophyll Index (OTCI) section uses Rayleigh correction to produce the necessary index. This step accounts for the spectral smile i.e. the in-FOV variation of the central wavelengths of OLCI channels.\r\n\r\nFor more information please see the OLCI user guide in the docs tab.",
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                            "ob_id": 10049,
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                "https://api.catalogue.ceda.ac.uk/api/v2/rpis/186910/?format=api"
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                {
                    "ob_id": 38861,
                    "uuid": "7f3ded66e9234b08969ce6b799357d87",
                    "title": "LiCSAR processing",
                    "abstract": "COMET LiCSAR processing using Gamma SAR and Interferometry software on Sentinel 1 IW SLC products.\r\n\r\nFor the details of the LiCSAR methodology [LiCSAR: An Automatic InSAR Tool for Monitoring Tectonic and Volcanic Activities paper in the docs tab]. In summary, once a new acquisition arrives, it is logically decomposed into pre-defined burst units and registered in the LiCSInfo database that handles burst and frame definitions. Images including bursts that form a given frame are extracted and merged into frame images. These are coregistered towards a primary frame image (a master image) that was set during the initialization of a frame, beforehand. The coregistration process includes spectral diversity and other necessary corrections. Once coregistered, the interferograms are formed by combining the new image with three chronologically previous ones. This way is suitable for interpretation and for further use of the interferograms in multitemporal InSAR processing methods based on small baselines strategy (e.g. NSBAS approach currently implemented into custom LiCSBAS chain [ LiCSBAS: An Open-Source InSAR Time Series Analysis Package Integrated with the LiCSAR Automated Sentinel-1 InSAR Processor paper in the docs tab]). The interferogram unwrapping is performed using optimised SNAPHU approach. All the LiCSAR products are multilooked by factors of 5 in the range and 20 in the azimuth directions to achieve a resolution of around 100×100 m per pixel.\r\n\r\nLiCSAR processing chain consists of:\r\n1. Preparation of Frame Epoch SLC\r\n2. Resampling to RSLC\r\n3. Formation of Differential Interferograms\r\n4. Unwrapping Interferograms\r\n5. LiCSInfo Metadata Database\r\n6. LiCSAR FrameBatch Processing\r\n7. FrameBatch Processing Chain\r\n8. FrameBatch Post-Processing\r\n\r\nFor more information please see the  LiCSAR: An Automatic InSAR Tool for Monitoring Tectonic and Volcanic Activities paper in the docs tab.",
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                    "ob_id": 39207,
                    "uuid": "a3aa8304674943f788a95d442155520e",
                    "title": "Derivation of the CH4_S5P_WFMD v1.5 product from the WFM-DOAS Retrieval algorithm",
                    "abstract": "The Weighting Function Modified Differential Optical Absorption Spectroscopy (WFM-DOAS) algorithm is a least-squares retrieval method based on scaling (or shifting) pre-selected atmospheric vertical profiles.   The column-averaged dry air mole fractions of  methane (denoted XCH4) are derived from the vertical column amounts of methane by normalising with the dry air column, which is obtained from the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis v5 (ERA5). The corresponding vertical columns of CH4 are retrieved from the measured sun-normalised radiance using spectral fitting windows in the SWIR spectral region (2311-2315.5 nm and 2320-2338 nm).\r\n\r\nFor further details see the documentation section.",
                    "keywords": "",
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                            "ob_id": 11891,
                            "platform": "https://api.catalogue.ceda.ac.uk/api/v2/platforms/26439/?format=api",
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            "computationComponent": [
                {
                    "ob_id": 707,
                    "uuid": "fea5a699972c4649a95d53d0cb611044",
                    "title": "Met Office operational unified model (UM) deployed on Keflavik, Iceland",
                    "abstract": "This computation involved: Met Office operational unified model (UM) deployed on Keflavik, Iceland.  Base for the GFDex measurement campaign",
                    "keywords": "",
                    "inputDescription": null,
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                    "identifier_set": [
                        "https://api.catalogue.ceda.ac.uk/api/v2/identifiers/458/?format=api",
                        "https://api.catalogue.ceda.ac.uk/api/v2/identifiers/459/?format=api"
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                {
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                        2010
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                    "uuid": "a0dd77615c424b50b314d6c30e17a0bf",
                    "title": "BRDF/Albedo Inversion Model.",
                    "abstract": "Computation for the Globalbedo BRDF products.\r\nFor more information, please see the ATBD document in the related docs tab.",
                    "keywords": "",
                    "inputDescription": null,
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                            "platform": "https://api.catalogue.ceda.ac.uk/api/v2/platforms/846/?format=api",
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                                "uuid": "85a81af3fa474c7bb11d45843c1eeb9f",
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                    "uuid": "a08cc459df1945b29f1bd5a67eaee9ca",
                    "title": "DTU Space ESMR NIMBUS-5 algorithm",
                    "abstract": "Sea ice concentration is obtained from ESMR passive microwave satellite data over the polar regions. The processing chain features: 1) dynamic tuning of tie-points and algorithms,  2) correction of atmospheric noise using a Radiative Transfer Model,  3) computation of per-pixel uncertainties, and 4) one channel sea ice concentration algorithm.",
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                    "uuid": "28a24e2f4a1e4b50962b3378afabc980",
                    "title": "Computation Component: Level 2 Land processing algorithm applied to Sentinel 3 SRAL raw data.",
                    "abstract": "There are three main steps in the Level-2 processing chain:\r\n\r\n1. Compute time-derived geophysical/environmental parameters.\r\n2. Perform re-tracking and compute physical parameters.\r\n3. Compute Level-2 altimeter/radiometer geophysical processing. \r\n\r\nComputing time-derived geophysical parameters involves:\r\n\r\n* re-computing altitude, orbital altitude rate, location and Doppler correction, accounting for updated orbit data\r\n* computing ionospheric corrections\r\n*computing non-equilibrium and equilibrium ocean tide heights, tidal loading, solid earth tide height, equilibrium long period ocean tide height and pole tide height (using pole locations)\r\n*computing the height of the mean sea surface above the reference ellipsoid\r\n*computing the mean dynamic topography, the height of the geoid and the ocean depth/land elevation.\r\n\r\nPerforming retracking and computing physical parameters (both SAR and LRM modes) involves:\r\n\r\n*discriminating echoes (ocean/lead, sea-ice, ice sheet margin or ocean/coastal)\r\n*performing retracking (ocean/lead, sea-ice, ice sheet margin or ocean/coastal)\r\n*computing physical parameters\r\n*merging snow depth (ocean/lead and sea-ice only)\r\n*performing a short-arc, along track ocean interpolation (ocean/lead and sea-ice only)\r\n*estimating freeboards (ocean/lead and sea-ice only)\r\n*performing a latitude limit check (ocean/lead and sea-ice only)\r\n\r\n(For SAR mode) performing modified slope correction (ice sheet margin and ocean/coastal only).\r\nLevel-2 altimeter/radiometer geophysical processing involves:\r\n\r\n*inputting and checking Level-1 MWR products\r\n*computing and correcting physical parameters according to platform data\r\n*interpolating MWR data and computing MWR geophysical parameters\r\n*computing altimeter wind speed and rain/ice flags\r\n*computing wind, tropospheric corrections and inverted barometer according to meteorological data\r\n*computing HF fluctuations of the atmospheric effect on the surface (dynamic atmosphere correction)\r\n*computing sea state bias\r\n*computing dual frequency ionospheric corrections\r\n*building and checking Level-2 SRAL/MWR products.",
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                    "uuid": "aaa20cc705654b399a314bf2fa15c294",
                    "title": "BRDF/Albedo Inversion Model computation for QA4ECV broadband albedo.",
                    "abstract": "More information needed",
                    "keywords": "QA4ECV",
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                    "abstract": "Data for each of the four Gabon FBRMS plots is found within plot directories: OKO-01; OKO-02; OKO-03 and LPG-01. Plot directories contain a main project directory (named using the starting date of data collection and the plot ID, e.g. 2022-06-24_LPG-01_PROJ) with nine data sub-directories, a tile_index.dat file and a 2022-06-24_LPG-01.kmz file as shown in the archived ForestScan_example_data_directory_structure.pdf document.\r\n\r\nThe raw project sub-directory contains all registered scans for each FBRMS 1ha plot. The matrix project sub-directory contains each scan’s Sensor's Orientation and Position (SOP) matrix with the GNSS coordinates (geographical coordinate system: WGS84 Cartesian) for all scans saved separately and made available via a .kmz file under the project main directory, e.g. 2022-06-24_LPG-01.kmz.\r\n\r\nIn order to estimate woody volume and above ground biomass (AGB) for each plot, the TLS2trees processing pipeline was used. 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