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This article highlights major differences between ERA-Interim and ERA5 but is not exhaustive. In particular changes to the computation of individual atmospheric parameters (due to the change in the assimilation system from 31r2 to 41r2) are not listed here.

Changes for all ERA5 datasets

 ERA-InterimERA5
Period covered1979 - present1979 - present
Production PeriodAugust 2006 – end 2018Jan 2016 – end 2017, then continued in near real-time
Assimilation systemIFS Cycle 31r2 4D-VarIFS Cycle 41r2 4D-Var
Model inputAs in operations (inconsistent SST)Appropriate for climate (e.g. CMIP5 greenhouse gases, volcanic eruptions, SST and sea-ice cover)
Input observationsAs in ERA-40 and from Global Telecommunication SystemIn addition, various newly reprocessed datasets and recent instruments that could not be ingested in ERA-Interim
Variational bias schemeSatellite radiancesAlso ozone, aircraft and surface pressure data
Satellite dataRTTOV-7, clear-sky, 1D-VAR rainy radiancesRTTOV-11, all-sky for various components
New parameters 

tbd

Parameters removed 

tbd

Handling of accumulated parametersAccumulated from the beginning of the forecast

Accumulated from previous post-processing

Does this mean from beginning of the Step?

Product main pagehttp://www.ecmwf.int/en/research/climate-reanalysis/era-interimhttp://climate.copernicus.eu/climate-reanalysis
Technical documentationBerrisford et al 2011: The ERA-Interim archive Version 2.0 ERA5 data documentation
Additional innovations Long-term evolution of CO2 in RTTOV, cell-pressure correction SSU, improved bias correction for radiosondes, EDA perturbations for sea-ice cover

Changes for daily dataset

 ERA-InterimERA5
Spatial resolution79 km globally, 60 levels to 0.1 hPa31 km globally, 137 levels to 0.01 hPa
Output frequency (temporal resolution)6-hourly analysis, 3-hourly forecast fieldsHourly analysis and forecast fields, 3-hourly for the Ensemble of Data Assimilations (EDA)
Uncertainty estimatesNoneFrom a 10-member Ensemble of Data Assimilations (EDA) at 63 km resolution
Additional innovations Long-term evolution of CO2 in RTTOV, cell-pressure correction SSU, improved bias correction for radiosondes, EDA perturbations for sea-ice cover
  

New parameters:

 

  

Parameters removed:

 

Changes for temporal aggregation sets

 ERA-InterimERA5
   
   
   

 

 

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