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title | Data and metadata known issues table |
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Known issue number | Centre | Forecasts or Hindcasts | Start dates(1) | Description |
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D1. | Met Office (all systems) | Both | All | Near-surface temperatures (6-hourly and daily minimum and maximum) and dewpoint temperature are encoded as being calculated at a height of 2m. Those parameters are calculated at 1.5 meters height in Met Office seasonal forecast systems | D2. | Met Office (system=12) | Both
| Hindcasts: May-Dec and January Forecasts: Sep2017 to Jan2018 | Global grid is incomplete (just 180 latitude points, between 90S and 89N) Requests with MARS-based interpolations (i.e. using "grid=NN/NN") won't work unless a suitable regional subselection is requested (with "area=LL/LL/LL/LL") Note that additionally, in this grid all points are set at integer values of latitude/longitude | D3. | All parameters on pressure levels are not globally complete, having "missing value indicators" in points below the orography. | D4. | Météo-France (system=5) | Forecasts | All | There is an issue with the postprocessing used at origin of the lagged start dates. Only members #27 to #51 are affected having data with a time shift of 7 days (168 hours). For instance, data with date/time labelled as YYYYMM08 00h would in fact correspond to YYYYMM01 00h. | D5. | CMCC (system=3) | Hindcasts | Years between 1993 and 1999 | There are anomalous values of SST (and associated parameters, e.g. fluxes, and vertical oceanic temperature profiles) appearing in the first hours of a very limited number of ensemble members of forecasts. The issue is caused by a bug in the oceanic perturbation generation tools used at origin to produce the ocean initial conditions. The errors/perturbations appear initially as excessively high SST values, confined to the reported hindcast years, in a limited number of grid points all in the tropical Pacific. They are very quickly dissipated by the coupled model physics and dynamics, affecting, therefore, only the first 24 hours of the forecasts at most. | D6. | CMCC (system=3) | Both | All | There are some variables affected by a spin-up issue. This affects just some ensemble members depending on the initial conditions each member started from. Unfortunately, as the selection of the forecast members is done randomly from a bigger pool of initial conditions, there is no metadata describing this in the current service based on GRIB files stored in ECMWF's MARS archive. | D7. | DWD (system=2) | Hindcasts | All 2017 start dates | For this forecasting system, year 2017 start dates have been computed as hindcasts and not real-time forecasts. | D8. | CMCC (system=3) | Both | All | For this forecasting system, the evaporation field is masked over the ocean (only land points are available) | D9. | Met Office (system=12,13) | Both | All | The fractional land-sea mask doesn't match the masked (land-only or sea-only) fields. For the files affected, the land-sea mask provided was produced as the result of a 1-degree interpolation of the binary land-sea mask in the native model resolution | D10. | ECMWF (system=51) | Both | All 1981-2016 start dates 2017-2022 January to July November 2022 to June 2023 | Volumetric soil moisture data in GRIB2 is encoded using GRIB simple_packing instead of the default CCSDS packing for this variable | D11. | BoM (system=2) | Both | All | The outputs from ACCESS-S2 in vertical pressure levels haven't been postprocessed to fill the holes below the terrain. In those grid points where the pressure at the surface is lower than a given pressure level the variables have been set to a missing value indicator and therefore they have not been extrapolated to produce a globally complete field. Due to this, the T850 and 500hPa graphical products from BOM include missing values, and BOM is excluded from the multi-system combination for these variables. |
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Data gaps
Note: (1) See description of nominal start dates here
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title | Data irregularities table |
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CentreForecast system | Forecast or hindcast | Description |
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I1. | MetOffice (all systems) | Forecasts | MetOffice real-time component is designed to produce a constant number of members each start date (see Description of the C3S seasonal multi-system). In those rare occasions when the MetOffice is not able to produce some of the expected members for a given start date, the affected members will be missing. Instead of re-running precisely those missing members, the MetOffice system schedules the run on a later start date of as many additional members as they were missing. The following table records all the occurrences of this irregularity by listing the dates when some members are missing (and how many of them) and the dates when additional members were produced. System | Missing members | Additional members |
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Start date |
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12 | 20170822 | 2 | 20170823 | 2 | 13 | 20180621 | 1 | 20180628 | 1 | 13 | 20181010 | 2 | 20181011 | 2 | 600 | 20210202 | 1 | 20210204 | 1 | 600 | 20210608 | 2 | 20210614 | 1 | 20210615 | 1 | 600 | 20211121 | 2 | 20211123 | 2 | 602 | 20231203 | 2 | 20231207 | 2 | 603 | 20240805 | 2 | 20240808 | 2 | 603 | 20240903 | 1 | 20240905 | 1 |
| I2. | BOM ACCESS-S2 (system=2) | Forecasts | BOM ACCESS-S2 real-time component is designed to produce a constant number of members (11) each start date (see Description of the C3S seasonal multi-system). The contribution to C3S includes all the members on the first of each month and from the previous 10 days, giving a total of 121 members. In those rare occasions when the BOM is not able to produce some of the expected members for a given start date, or when due to technical issues it is not feasible to correctly deliver them in time, all the members from the affected start date will be missing. Note that for C3S products only the 55 more recent available members are used. The following table records all the occurrences of this irregularity by listing the dates where no members from BOM ACCESS-S2 where archived at C3S. Nominal start date | Available members | Missing start dates (number of members) |
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June 2025 | 110 | 20250522 (11) | July 2025 | 110 | 20250621 (11) |
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