The regional reanalysis system for Continental Europe matches the domain of the CORDEX EURO-11 specifications, albeit at a higher spatial resolution, i.e., 0.055° (6 km) instead of 0.11° (12 km). It comprises
Determining concentrations of cloud condensation nuclei (CCN) is one of the first steps in the chain in analysis of cloud droplet formation, the direct microphysical link between aerosols and cloud droplets,
ModE-RA is a monthly 3-dimensional reanalysis product covering the period from 1421 to 2008. It was created by combining information on historical climate - including early instrumental data, documentary
Please note: ModE-RAclim is only a side product of the ModE project. ModE-RAclim does not contain centennial scale climate variability. For most users the main product ModE-RA therefore should be used
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
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
ECMWF has in the past produced three major reanalyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
ECMWF has in the past produced three major reanalyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA-Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
ECMWF has in the past produced three major reanalyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA-Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
ECMWF has in the past produced three major re-analyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA-Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
This experiment contains the re-analysis (acronym rean) and subsequent forecasts (acronym fore) from the COSMO high resolution model of DWD (2.8km horizontal resoultion and 50 model levels) for the entire
ECMWF has in the past produced three major reanalyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA-Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
The German partner of the "Estimating the Circulation and Climate of the Ocean" (GECCO) consortium provided a dynamically consistent estimate of the time-varying ocean circulation over the 50-year period
ECMWF has in the past produced three major reanalyses: FGGE, ERA-15 and ERA-40. Now progress is being made in producing 'ERA-Interim'. ERA-Interim has progressed beyond the end of ERA-40. After completion
The data represent 6-hourly values of selected variables from the ECMWF reanalysis ERA-40 processed for using as input to the COSMO-model preprocessor INT2LM. The preprocessor INT2LM performs the interpolation