Procedure Computation Instance – Django REST framework

Get a list of ProcedureComputation objects. ProcedureComputations have a 1:1 mapping with Observations.

### 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:

- `uuid`
- `title`
- `keywords`
- `abstract`

### How to use filters:

These filters can be used like django query filters using __ for related model relationships.

- `/computations/?uuid=d594d53df2612bbd89c2e0e770b5c1a0`
- `/computations/?title__startswith!=DETAILS NEEDED - COMPUTATION CREATED FOR SATELLITE COMPOSITE`
- `/computations/?abstract__contains=HadCM3 model`

GET /api/v2/computations/31979/?format=api

HTTP 200 OK
Allow: GET, HEAD, OPTIONS
Content-Type: application/json
Vary: Accept

{
    "ob_id": 31979,
    "uuid": "66fba8679a8045cd8d8e53338f5542b5",
    "title": "Computation of UKCP Global (60km) - European Circulation Indices",
    "abstract": "The daily indices of the jet stream latitude and strength are calculated using the approach described in Woollings et al., 2010 (https://doi.org/10.1002/qj.625) This is calculated first by smoothing the tropospheric (850 hPa) zonal wind speed in the North Atlantic sector (0-60°W, 15-75°N) using a 5-day moving window. The location and magnitude of the maximum value in this smoothed daily field indicate the latitude and strength of the jet stream respectively.\r\n\r\nThe daily weather type indices were generated by classifying daily mean sea level pressure (MSLP) (changes compared to the 1981-2000 average) into 30 weather regimes which capture the full range of circulation types affecting Europe (see Neal et al., 2016,  https://doi.org/10.1002/met.1563) These 30 weather patterns are also provided as an amalgamated set of 8 weather patterns.\r\n\r\nThe winter NAO index is calculated as the seasonal mean (December-January-February) of the difference in sea level pressure between Iceland and Gibraltar (the Atlantic pressure gradient). These are calculated using the difference between the seasonal mean sea level pressure time-series between grid-boxes containing at Gibraltar (36.14N, 5.35E) and Iceland (65.07N, 22.7W).",
    "keywords": "",
    "inputDescription": null,
    "outputDescription": null,
    "softwareReference": null,
    "identifier_set": []
}