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:

- `GET`
- `HEAD`

### Available filters:

None
### How to use filters:

None

GET /api/v2/composites/?format=api&offset=300
HTTP 200 OK
Allow: GET, HEAD, OPTIONS
Content-Type: application/json
Vary: Accept

{
    "count": 662,
    "next": "https://api.catalogue.ceda.ac.uk/api/v2/composites/?format=api&limit=100&offset=400",
    "previous": "https://api.catalogue.ceda.ac.uk/api/v2/composites/?format=api&limit=100&offset=200",
    "results": [
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                {
                    "ob_id": 14521,
                    "uuid": "70aa606ca0584f4594588fc6d7842595",
                    "title": "NAME dispersion model footprints",
                    "abstract": "Atmospheric dispersion model footprints computed at the University of Leicester for various projects using the the Met Office's Numerical Atmospheric-dispersion Modelling Environment (NAME)",
                    "keywords": "",
                    "inputDescription": null,
                    "outputDescription": null,
                    "softwareReference": null,
                    "identifier_set": []
                }
            ],
            "acquisitionComponent": [
                {
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                    "independentInstrument": [],
                    "instrumentplatformpair_set": [
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                            "relatedTo": {
                                "ob_id": 14528,
                                "uuid": "96ffb69542634508b8969ba111a733c6",
                                "short_code": "acq"
                            }
                        },
                        {
                            "ob_id": 5510,
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                            }
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                    ]
                }
            ],
            "identifier_set": [],
            "responsiblepartyinfo_set": []
        },
        {
            "ob_id": 14538,
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                {
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                    "uuid": "70aa606ca0584f4594588fc6d7842595",
                    "title": "NAME dispersion model footprints",
                    "abstract": "Atmospheric dispersion model footprints computed at the University of Leicester for various projects using the the Met Office's Numerical Atmospheric-dispersion Modelling Environment (NAME)",
                    "keywords": "",
                    "inputDescription": null,
                    "outputDescription": null,
                    "softwareReference": null,
                    "identifier_set": []
                }
            ],
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                        {
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                        {
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                            "relatedTo": {
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                            "relatedTo": {
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        },
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                    "keywords": "",
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                    "abstract": "This computation involved: MRI-CGCM2.3.2 Meteorological Research Institute Coupled Global Circulation Model deployed on Meteorological Research Institute (Japan) computer.",
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                    "abstract": "This computation involved: BCCR-BCM2.0 Bergen Climate Model Version 2 deployed on Bjerknes Centre for Climate Research (Norway) Computer.",
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                    "abstract": "This computation involved: GISS-AOM Atmosphere Ocean Model deployed on NASA Goddard Institute for Space Studies (GISS) (USA) computer.",
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                    "title": "GFDL-CM2.0 Global Coupled Climate Model deployed on Geophysical Fluid Dynamics Laboratory (USA) computing facility",
                    "abstract": "This computation involved: GFDL-CM2.0 Global Coupled Climate Model deployed on Geophysical Fluid Dynamics Laboratory (USA) computing facility.",
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                    "title": "CGCM3.1 Canadian Global Coupled Model Version 3.1 deployed on Canadian Centre for Climate Modelling and Analysis computing facility",
                    "abstract": "This computation involved: CGCM3.1 Canadian Global Coupled Model Version 3.1 deployed on Canadian Centre for Climate Modelling and Analysis computing facility.",
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                    "abstract": "This computation involved: GISS-ModelE/HYCOM Coupled Atmosphere Ocean Model deployed on NASA Goddard Institute for Space Studies (GISS) (USA) computer.",
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                    "abstract": "This computation involved: GISS-ModelE/Russell Coupled Atmosphere Ocean Model deployed on NASA Goddard Institute for Space Studies (GISS) (USA) computer.",
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                    "title": "CNRM-CM3  Centre National de Recherches Météorologiques Coupled Model Version 3 deployed on Météo-France/Centre National de Recherches Météorologiques (France) computer",
                    "abstract": "This computation involved: CNRM-CM3  Centre National de Recherches Météorologiques Coupled Model Version 3 deployed on Météo-France/Centre National de Recherches Météorologiques (France) computer.",
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                    "abstract": "This computation involved: INM-CM3.0 Institute for Numerical Mathematics Coupled Model Version 3.0 deployed on Institute for Numerical Mathematics (Russia) computer.",
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                    "abstract": "This computation involved: ECHAM4 ocean coupled general circulation model deployed on Max Planck Institute für Meteorologie computing facility.",
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                    "abstract": "The GlobTemperature Level-2 MODIS Land Surface Temperature (LST) algorithm derives LST data from L1B calibrated radiances from the MODIS instruments on the Aqua and Terra Satellites.   It uses a generalized split-window (SW) approach to estimate Land Surface Temperature as a linear function of clear-sky TOA (top of atmosphere) brightness temperatures from MODIS bands 31 and 32 centred on 11 and 12 microns respectively.\r\n\r\nThe GlobTemperature MODIS product also provides a full breakdown of the pixel level uncertainty budget.  The uncertainty analysis takes into account the expected performance of the retrieval algorithm under varying surface and atmospheric conditions, with these uncertainties categorised into a 3-component model: random, locally correlated and systematic.   The locally correlated component is further split into surface and atmospheric conditions.",
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                    "title": "Level 2 Carbon Monoxide (CO) total column processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 2 processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data. The retrieval algorithm requires several input fields:\r\n• The measured Earth radiance and solar irradiance spectra including noise estimate, solar and viewing\r\ngeometry, and information of geo-location.\r\n• ECMWF temperature, water vapor, and pressure profiles, and geo-potential height.\r\n• An estimate of the CH4 field using a chemistry transport model, e.g. Transport Model 5 (TM5, [RD33]).\r\n• An estimate of the CO column from a chemistry transport model (e.g. TM5).\r\nThe retrieval is performed in two steps: first, as part of the SWIR preprocessing module, the vertically integrated amount of methane is retrieved from a dedicated fit window of the SWIR band between 2315 and 2324 nm using a non-scattering radiative transfer model. The extent of lightpath shortening and enhancement due to atmospheric scattering by clouds and aerosols can be indicated by comparing the retrieved CH4 column with a priori knowledge. If the difference ∆CH4 exceeds a certain threshold, observations are strongly contaminated by clouds and are rejected. In a second step, the SICOR full physics retrieval approach is used to infer CO columns from the adjacent spectral window, 2324-2338 nm. Here, the methane absorption features are used to infer information on atmospheric scattering by clouds and aerosols, which passed the cloud filter, together with the atmospheric CO and H2O abundances, surface albedo, and spectral calibration of the reflectance spectrum. The scattering layer has a triangular height distribution of fixed geometrical thickness, and its optical depth and height are parameters to be retrieved. This step of the retrieval relies on accurate a priori knowledge of CH4 which will be provided within an accuracy of ±3 % by a dedicated methane forecast using the TM5 atmospheric transport model. The atmospheric scattering is described by a two-stream radiative transfer model. Finally, the retrieval product consists of a CO column estimate including a column averaging kernel and a random error estimate. For more information on the processing algorithm please look at the ATBD document on the TROPOMI CO webpage.",
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                    "title": "Level 2 Ozone (O3) total column processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 2 processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data. The one-step OFFL algorithm (S5P_TO3_GODFIT) comprises a non-linear least-squares inversion based on the direct comparison of simulated and measured backscattered\r\nradiances. Simulated radiances are computed (again for a multiple scattering atmosphere) at all nominal wavelengths in the UV fitting window, along with corresponding analytically derived weighting functions for total ozone, albedo and effective temperature. The algorithm also contains closure fitting coefficients and a semi-empirical correction for Ring interference. Although more accurate, the S5P_TO3_GODFIT algorithm involves many more RT simulations than S5P_TO3_DOAS, and is, therefore, slower by an order of magnitude approximately. This is currently the main driver for the selection of S5P_TO3_DOAS for the\r\nNRTI product. For more information on the processing of the O3 product please refer to the ATBD document.",
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                    "title": "Level 2 Nitrogen Dioxide (NO2) total column processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 2 processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data. The TROPOMI NO2 processing system is based on the DOMINO and QA4ECV processing systems, with improvements related to specific TROPOMI aspects and new scientific insights. The basis for the processing at KNMI is a retrieval-assimilation-modeling system that uses the 3-dimensional global TM5 chemistry transport model as an essential element. The retrieval consists of a three-step procedure, performed on each measured Level-1b spectrum:\r\n1. the retrieval of a total NO2 slant column density (Ns) from the Level-1b radiance and irradiance spectra\r\nmeasured by TROPOMI using a DOAS (Differential Optical Absorption Spectroscopy) method,\r\n2. the separation of the Ns into a stratospheric and a tropospheric part on the basis of\r\ninformation coming from a data assimilation system, and\r\n3. the conversion of the tropospheric slant column density into a tropospheric vertical column density and of the stratospheric slant column density into a stratospheric vertical column density, by applying an appropriate AMF based on a look-up table of altitude-dependent AMFs and actual, daily information on the vertical distribution of NO2 from the TM5-MP model on a 1-degree by 1-degree grid. The altitude-dependent AMF depends on the satellite geometry, terrain height, cloud fraction and height and surface albedo.\r\nThese steps are described in detail in the ATBD document.",
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                    "title": "Level 2 Cloud processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 2 processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data.\r\nOptical Cloud Recognition Algorithm (OCRA) is the S5P_CLOUD_OCRA heritage. In OCRA, optical sensor measurements are divided into two components: a cloud-free background and a remainder expressing the influence of clouds. OCRA was first developed for GOME in the late 1990s, when enough data from the three sub-pixel broad-band PMDs (Polarization Measurement Devices) had accumulated to allow for the construction of the global cloud-free composite which is the key element in the algorithm. Over the course of the 16-year GOME record, the\r\nalgorithm was refined and the cloud-free composite adjusted as more data became available. OCRA has also been applied to SCIAMACHY and GOME-2. Initial cloud-free composites for these sensors were based on GOME data before dedicated measurements became available from SCIAMACHY and GOME-2. For S5P_CLOUD_OCRA, the initial cloud-free composite will be based on GOME-2 and OMI (see section 5.2). Retrieval of Cloud Information using Neural Networks (ROCINN) is the S5P_CLOUD_ROCINN heritage. ROCINN is based on the comparison of measured and simulated satellite sun-normalized radiances in and near the O2 A-band, and it uses a neural network algorithm to retrieve cloud-top height and cloud-top albedo. ROCINN uses the cloud fraction input from OCRA as one starting point. Early versions of ROCINN used a transmittance model to compute simulated radiances, but the latest versions are based on the use of the VLIDORT radiative transfer scattering model.\r\nFor GOME and GOME-2, ROCINN Version 2.0 is the current operational algorithm in the GDP [GOME Data Processor]. This version is based on the assumption that clouds are simply Lambertian reflecting surfaces so the two main retrieval products are the cloud-top height and the cloud-top albedo itself. This is the “clouds-as-reflecting-boundaries” (CRB) model; see for example [van Roozendael et al., 2006] for GOME and [Loyola et al., 2011] for GOME 2.\r\nAlthough ROCINN 2.0 is the heritage algorithm, there is an important point of departure for S5P. For TROPOMI/S5P, ROCINN Version 3.0 was initially used, which is based on a more realistic treatment of clouds as optically uniform layers of light-scattering particles (water droplets). This is the “clouds-as-layers\" (CAL) model – here, the two main retrieval products are the cloud-top height and the cloud optical thickness. Details of this algorithm prototype may be found in [Schuessler et al., 2014]. Although the CAL model will be the default for S5P, it has been requested that the CRB method should also be retained as an option. CAL is the preferred method for the relatively small TROPOMI/S5P ground pixels (5.5 x 3.5\r\nkm2). The CRB approach works best with large pixels such as those from GOME (footprint 320 x 40 km2). [Schuessler et al., 2014] has shown that for the smaller GOME-2 pixels, CAL retrieval produces more reliable cloud information than that from CRB, not only with regard to the accuracy of the cloud parameters themselves but also with regard to the effect of cloud parameter uncertainties on total ozone accuracy. In OCRA, the intensity is regarded as a linear function of the radiometric cloud cover, and in\r\nROCINN, TOA radiances for partially cloudy scenarios are computed using a linearly weighted mean of the clear-sky and fully-cloudy calculations, the weighting factor being the cloud fraction. In the context of this IPA model, the two algorithms are consistent. With the notably smaller pixel size that comes with higher spatial resolution, 3-D cloud radiative effects will become an important consideration in error budgeting for the cloud algorithms. For more information on the processing chain please see the ATBD document.",
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                    "title": "Level 2 UV Aerosol Index processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 2 processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data. MORE INFORMATION TO FOLLOW",
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                    "title": "Level 2 processing algorithm applied to Sentinel 1 raw data, Instrument Processing Facility (IPF) version 3",
                    "abstract": "Level-2 consists of geo-located geophysical products derived from Level-1. Level-2 Ocean (OCN) products for wind, wave and currents applications may contain the following geophysical components derived from the SAR data:\r\n- Ocean Wind field (OWI)\r\n- Ocean Swell spectra (OSW)\r\n- Surface Radial Velocity (RVL)\r\nThe availability of components depends on the acquisition mode. The OSW component cannot be generated from IW and EW mode, since individual looks with sufficient time separation are required. The obtained inter look time separation within one burst is too short due to the progressive scanning (i.e. short dwell time).\r\n\r\nThe metadata referring to OWI are derived from an internally processed GRD product. The metadata referring to RVL (and OSW, for SM and WV mode) are derived from an internally processed SLC product.\r\n\r\nFor more information on the changes for this processing version please see the Sentinel 1 document libary under the docs tab.",
                    "keywords": "Synthetic Aperture Radar, Sentinel 1, Level 1, algorithm, SAR",
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                    "abstract": "Level-2 consists of geo-located geophysical products derived from Level-1. Level-2 Ocean (OCN) products for wind, wave and currents applications may contain the following geophysical components derived from the SAR data:\r\n- Ocean Wind field (OWI)\r\n- Ocean Swell spectra (OSW)\r\n- Surface Radial Velocity (RVL)\r\nThe availability of components depends on the acquisition mode. The OSW component cannot be generated from IW and EW mode, since individual looks with sufficient time separation are required. The obtained inter look time separation within one burst is too short due to the progressive scanning (i.e. short dwell time).\r\n\r\nThe metadata referring to OWI are derived from an internally processed GRD product. The metadata referring to RVL (and OSW, for SM and WV mode) are derived from an internally processed SLC product.\r\n\r\nFor more information on the changes for this processing version please see the Sentinel 1 document libary under the docs tab.",
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                    "title": "Level 1B processing algorithm applied to Sentinel 5P TROPOspheric Monitoring Instrument (TROPOMI) raw data",
                    "abstract": "This computation involves the Level 1b processing algorithm applied to raw TROPOspheric Monitoring Instrument (TROPOMI) data.\r\n\r\nThe Earth radiance measurements form the bulk of the measurements. Apart from the optical properties of the instrument, there is some flexibility in the electronics that determine the Earth's radiance ground pixel size. The co-addition period determines the ground pixel size in the along-track direction. Row binning (which is possible for UVN-DEMs only) determines the ground pixel size across track. The parameter space is limited, however, as choosing a smaller ground pixel size will increase the data rate and will decrease the signal-to-noise ratio for the individual ground pixels. The data rate is limited by both internal interfaces within the instrument as well as by the platform’s on-board storage and down-link capabilities. \r\nFor the Earth's radiance measurements, the co-addition period can be set to either 1080ms or 840ms. This\r\neffectively results in a ground pixel size of approximately 7km or 5.5km along-track. The co-addition period is set in the instrument configuration, initially, the nominal operations phase was started with 1080ms. For the SWIR-DEM, which contains a CMOS detector, row binning is not supported. This means that, effectively, the binning factor is 1 for the SWIR bands (Band 7 and Band 8), resulting in a ground pixel size across-track between 7km at the center and 34km at the edges of the across-track field of view. The ground pixel size varies across-track since the spatial dispersion (degrees/pixel) is constant, resulting in a ground pixel size that becomes larger towards the edges of the across-track field of view due to the Earth’s curvature.\r\nApart from the binning factor and the co-addition period, the remaining configuration parameters for\r\nthe Earth radiance measurements, including exposure time and gains, have been optimized during in-flight\r\ncommissioning for the best signal-to-noise ratio while minimizing the saturation of the detector or electronics. This optimization was based on scenes with the highest radiance levels, typically clouded scenes. Since the highest radiance level changes as a function of latitude, a total of five different settings for different latitude zones are created. For bands 4 and 6 saturation, it has not been possible to exclude saturation completely due to instrument limitations.\r\n\r\nFor more information please see the ATBD document linked in the docs tab.",
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                    "abstract": "30-year (1980-2010) time-series have been extracted from a global gridded surface meteorology dataset (Global Soil Wetness Project Phase 3) for the grid cells containing the Earth System Model - Snow Model Intercomparison Project (ESM-SnowMIP) reference sites, interpolated to one-hour timesteps and bias corrected. Although applied to all sites. The bias corrections are particularly important for mountain sites that are hundreds of meters higher than the grid elevations; as a result, uncorrected air temperatures are too high and snowfall amounts are too low in comparison with in situ measurements.\r\n\r\nThe ten in situ sites are characterised as maritime (Sapporo, Japan), arctic (Sodankylä, Finland), boreal (Old Aspen, Old Jack Pine and Old Black Spruce, Saskatchewan, Canada) and mid-latitude alpine (Col de Porte, France; Reynolds Mountain East, Idaho, USA, Senator Beck and Swamp Angel, Colorado, USA; Weissfluhjoch, Switzerland). The locations of the in situ measurement sites are listed as follows: \r\n\r\nCDP (Col de Porte),  Latitude: 45.29, Longitude: 5.77,  Elevation: 1325.0 m,  Location: France;\r\nOAS (Old Aspen), Latitude: 54.05, Longitude: -106.33,  Location: Canada;\r\nOBS (Old Black Spruce), Latitude: 54.65, Longitude: -105.20, Location: Canada;\r\nOJP (Old Jack Pine), Latitude: 54.53, Longitude: -105.00, Location: Canada; \r\nRME (Reynolds Mountain East), Latitude: 43.19, Longitude: -116.78, Location: United States;\r\nSAP (Sapporo), Latitude: 43.06, Longitude: 141.33, Elevation: 17.0 m, Location: Japan;\r\nSNB (Senator Beck Basin Study Area (SBBSA)), Latitude: 37.91, Longitude: -107.73, Location: United States;\r\nSOD (Sodankyla), Latitude: 67.42, Longitude: 26.59, Location: Finland; \r\nSWA (Swamp Angel Study Plot (SASP)), Latitude: 37.91, Longitude: -107.71, Elevation: 3371.0 m, Location: United States; \r\nWFJ (Weissfluhjoch), Latitude: 46.83, Longitude: 9.81, Location: Switzerland.",
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                    "abstract": "The GlobBiomass retrieval algorithm is used to derive estimates of forest above-ground biomass (AGB) from satellite data for the year 2017 as part of the Biomass CCI project.\r\n\r\nFirst,  per-pixel estimates of growing stock volume (GSV, unit: m3/ha) were obtained from spaceborne SAR images acquired in 2017 (ALOS-2 PALSAR-2, Sentinel-1) with the BIOMASAR algorithm, adapted specifically to ALOS-2 PALSAR-2 and Sentinel-1 data. Individual per-pixel GSV estimates were then combined with a set of merging rules to form the final per-pixel estimate of GSV. The retrieval was supported by LiDAR (ICESAT) data and auxiliary datasets . AGB was then obtained from GSV with a set of Biomass Expansion and Conversion Factors (BCEF) following approaches to extend on ground estimates of wood density and stem-to-total biomass expansion factors to obtain a global raster dataset.\r\n\r\nSee the Algorithm Theoretical Basis Document for details on the EO datasets, the biomass retrieval algorithms and the estimation of the BCEF (see http://cci.esa.int/biomass)",
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                    "abstract": "The GOSAT  spectral data were inputted into the UoL-FP retrieval algorithm where the Proxy retrieval approach was used to obtain the column-averaged dry-air mole fraction of methane (XCH4).  See the linked documentation for further information",
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