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Atmospheric model Analysis runs for the four main synoptic hours 00, 06, 12 and 18 UTC; forecast runs out to 10 days based on the 00/12 UTC analysis forecast. Data is produced at the surface, on model levels, pressure levels, isentropic levels and levels of … ...
A vast amount of data is archived daily containing IFS (Integrated Forecast System) experiments produced by ECMWF's Research Department or by Member States' users at ECMWF. Basically, an experiment can address any area of meteorology and it is archived … ...
Copernicus Emergency Management Service … Copernicus Emergency Management Service … Copernicus … CEMS … Copernicus Emergency Management … ...
The ERA-15 production system generated re-analyses for 15 years (1979-1993) using a special version of their 1995 operational data assimilation system and model. The resulting analyses include full model resolution analyses or reduced resolution analyses and … ...
ERA-40 is an ECMWF re-analysis of the global atmosphere and surface conditions for 45-years, over the period from September 1957 through August 2002. An atlas of key atmospheric variables was produced for ERA-40 … ECMWF Reanalysis - 40 years … ECMWF … ERA-40 … ...
… a range of 60 pressure levels. It’s successor is the ERA5 reanalysis from the Copernicus Climate Change Service. Users are strongly advised to migrate to ERA5 from the Climate Data Store (CDS) . … ECMWF Reanalysis - … a range of 60 pressure levels. It’s successor is the ERA5 reanalysis from the Copernicus Climate Change Service. … ...
CERA-20C is the ECMWF 10-member ensemble of coupled climate reanalyses of the 20th century, from 1901-2010. It is based on the CERA assimilation system, which assimilates only surface pressure and marine wind observations as well as ocean temperature and … ...
… towards the high resolution (0.05 degree) OSTIA sea-surface temperature analysis to avoid model drift while enabling the … on 37 pressure levels (as in  ERA-Interim ), 16 potential temperature levels, and the 2 PVU potential vorticity level. … flux, Turbulent diffusion coefficient for heat, Tendency of temperature due to physics, Tendency of specific humidity due … ...
… ensemble using: Radiative forcing from CMIP5 Sea-surface temperature (SST) and sea ice cover from HadISST2 Overview of … ensemble using: Radiative forcing from CMIP5 Sea-surface temperature (SST) and sea ice cover from HadISST2 Overview of … ...
ERA-20C is ECMWF's first atmospheric reanalysis of the 20th century, from 1900-2010. It assimilates observations of surface pressure and surface marine winds only. It is an outcome of the ERA-CLIM project. Product description The configuration of the ERA-20C … ...