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ERA-40

ECMWF 40-year Reanalysis (ERA-40)

Discontinued

No longer updated

Production finished in the early 2000s and the record is no longer updated. ECMWF decommissioned its Public Datasets service (web interface and Web API) on 1 June 2023 and does not offer another public route for ERA-40. In practice the data now come from NCAR GDEX (some products openly available) or the copy at CEDA in the UK.

Successor: ERA-Interim → ERA5 — The direct successor was ERA-Interim (1979–2019), itself now discontinued; the recommended reanalysis today is ERA5 (1940 to present, about 31 km, 137 levels). ERA5 also covers 1957–1978, the period that used to require ERA-40.

At a glance

Item Details
Section Atmosphere › Reanalyses
Type Reanalysis
Domains Atmosphere, Land, Ocean waves
Provider European Centre for Medium-Range Weather Forecasts (ECMWF)
Period 1957-09 ~ 2002-08
Coverage Global
Horizontal resolution Spectral T159 / reduced Gaussian grid N80 (approximately uniform 125 km spacing) / 2.5° × 2.5° latitude-longitude grid on the public data server
Vertical resolution 60 model levels (top level 0.1 hPa) / 23 pressure levels / 15 isentropic levels
Temporal resolution 6-hourly analyses (00, 06, 12, 18 UTC); monthly means separately
Update frequency Ended (August 2002 is the last month)
Licence NCAR GDEX copies are CC BY 4.0, with acceptance of the ECMWF terms of use
Account required Yes

Note on period: September 1957 to August 2002 (45 years), starting just before the International Geophysical Year (1958).

How to read the resolution
  • Horizontal resolution lists both the native model grid and the grid you download, as given in the official documentation. The same dataset can come on different grids from different providers or products, so check the grid of your downloaded file.
  • Grid spacing is not the effective resolution. A provided grid that is finer than the native one carries no extra information.
  • Intervals and whether a value is instantaneous, mean or accumulated differ between variables — see 'Available variables' below.
  • The 'provided resolution' in lists and the comparison table is a simplified km/degree value for quick comparison. Use this page for exact values.

Overview

ECMWF's second-generation reanalysis of the global atmosphere and surface conditions for the 45 years from September 1957 to August 2002. It used 3D-Var (FGAT) data assimilation with a T159, 60-level model and was among the first reanalyses to assimilate satellite radiances (TOVS, SSM/I, etc.) directly. A coupled ocean-wave model provides wave parameters as well. ERA-40 was a standard dataset for climate research until the mid-2000s and has since been superseded by ERA5.

What changed from the previous dataset

What changes with the successor

ERA-40 → ERA-Interim

ERA-Interim replaced 3D-Var with 12-hour 4D-Var and variational bias correction of satellite radiances (VarBC) and raised the resolution to T255, addressing ERA-40's problems with the hydrological cycle, the stratospheric circulation and temporal consistency.

Aspect ERA-40 ERA-Interim
Period 1957-09 to 2002-08 1979-01 to 2019-08 (updated in near real time until August 2019)
Horizontal resolution T159 (N80, about 125 km) T255 (N128, about 79–80 km)
Vertical resolution and model top 60 model levels, top level 0.1 hPa 60 model levels, top level 0.1 hPa (unchanged)
Pressure and isentropic output levels 23 pressure levels / 15 isentropic levels 37 pressure levels / 16 isentropic levels
Model version IFS CY23r4 IFS CY31r2
Data assimilation 3D-Var (FGAT), 6-hour window 4D-Var, 12-hour window
Satellite radiance bias correction Static bias correction Variational bias correction (VarBC), adjusted automatically
Observations Observations collected and reprocessed for ERA-40 ERA-40 observations plus GTS real-time data, rain-affected SSM/I radiances (1D-Var), reprocessed Meteosat winds and more
Known problems addressed Excessive tropical oceanic precipitation, too strong Brewer-Dobson circulation, poor temporal consistency More realistic hydrological cycle (global precipitation-evaporation balance) and stratospheric circulation (age of air)
Ocean-wave grid 1.5° 1.0°

Things to watch when switching

  • Do not splice the two into one time series. Climatologies and trends can differ even over the 1979–2002 overlap.
  • ERA-40 has 23 pressure levels against ERA-Interim's 37; compare on the common levels only.
  • ERA-Interim starts in 1979. For 1957–1978, use ERA5 (from 1940) rather than ERA-40.
  • ERA-Interim still has its own limitations, such as too strong a hydrological cycle over the oceans and warm, moist low-level biases in the Arctic. Do not overstate the improvement.

Sources: Dee et al. (2011), The ERA-Interim reanalysis, QJRMS · Uppala et al. (2005), The ERA-40 re-analysis, QJRMS · ECMWF — What is the difference between ERA-Interim (1979-2019) and ERA-40 (1957-2002) · ERA-Interim documentation (Copernicus Knowledge Base) · Kållberg et al. (2004), The ERA-40 archive · Uppala (2006), From ERA-15 to ERA-40 and ERA-Interim

Compare the two side by side

Available variables

Main parameters from the parameter tables of the ERA-40 archive report (ERA-40 Project Report Series No. 17). Names are ECMWF GRIB short names (matching the parameter codes). The original data are GRIB1; accumulated parameters are forecast accumulations (W m-2 s, etc.).

Time-stamp convention — instantaneous, mean or accumulated? — click to show

Analysed fields are instantaneous values at 00, 06, 12 and 18 UTC. Accumulated quantities such as precipitation, radiation and surface fluxes come only from forecasts and are accumulated from the forecast start to the given step (the public 2.5° data offered 6-hour forecasts only).

  • Accumulations run from the start of the forecast. Forecasts start at 00 and 12 UTC (to 36 h) and at 06 and 18 UTC (to 6 h); for shorter intervals, difference consecutive forecast steps.
  • The 2.5° data on ECMWF's former public data server contained 6-hour forecasts only, so accumulations there are 6-hour totals. For files from other archives, check the forecast start time and step in the GRIB header.
  • To turn accumulated radiation and heat fluxes (W m-2 s) into mean fluxes (W m-2), divide by the accumulation period in seconds. The monthly accumulation stream (mdfa) is expressed per day: divide by 86,400 to get W m-2, and multiply precipitation by 1000 to get mm/day.
  • Fluxes in the monthly mean stream moda are in 'per six hours' units and not aligned with calendar months; ECMWF strongly recommends using mdfa instead.
  • Maximum and minimum 2 m temperature refer to the period since the previous post-processing; no monthly means were produced for them.

Source: The ERA-40 archive (ERA-40 Project Report Series No. 17)

instantaneous mean accumulated maximum minimum static — instantaneous: value at the time stamp · mean/accumulated/maximum/minimum: over the indicated interval · static: does not change with time

Pressure levels (23)

Variable Short name Units Time convention Notes
Geopotential z m2 s-2 instantaneous divide by 9.80665 for geopotential height (m)
Temperature t K instantaneous
Eastward wind component u m s-1 instantaneous
Northward wind component v m s-1 instantaneous
Vertical velocity w Pa s-1 instantaneous
Specific humidity q kg kg-1 instantaneous
Relative humidity r % instantaneous
Vorticity (relative) vo s-1 instantaneous
Divergence d s-1 instantaneous
Potential vorticity pv K m2 kg-1 s-1 instantaneous
Ozone mass mixing ratio o3 kg kg-1 instantaneous

Surface and single level

Variable Short name Units Time convention Notes
Mean sea level pressure msl Pa instantaneous
2 metre temperature 2t K instantaneous
2 metre dewpoint temperature 2d K instantaneous
10 metre eastward wind component 10u m s-1 instantaneous
10 metre northward wind component 10v m s-1 instantaneous
Sea surface temperature sst K instantaneous
Sea ice fraction ci 0-1 instantaneous
Total cloud cover tcc 0-1 instantaneous
Total column water vapour tcwv kg m-2 instantaneous

Accumulated forecast parameters

Variable Short name Units Time convention Notes
Large-scale and convective precipitation lsp, cp m of water since forecast start accumulated
Surface sensible and latent heat flux sshf, slhf W m-2 s since forecast start accumulated
Surface solar and thermal radiation downwards ssrd, strd W m-2 s since forecast start accumulated
Top thermal radiation ttr W m-2 s since forecast start accumulated
Evaporation e m of water since forecast start accumulated

Ocean waves

Variable Short name Units Time convention Notes
Significant wave height swh m instantaneous
Mean wave direction mwd degrees instantaneous
Mean wave period mwp s instantaneous

Land surface

Variable Short name Units Time convention Notes
Soil temperature level 1 stl1 K instantaneous
Volumetric soil water layer 1 swvl1 m3 m-3 instantaneous
Snow depth sd m of water equivalent instantaneous

The full variable list is in the official documentation.

How to get the data

Practical tips

  • The NCAR Climate Data Guide lists the main weaknesses: tropical moisture (precipitation, total column water) too high after 1991, precipitation well above evaporation, an overly strong Brewer-Dobson circulation and unrealistic Arctic temperature trends. Avoid ERA-40 for hydrological-cycle, stratospheric or Arctic-trend studies.
  • The observing system changes sharply around 1979 as satellite data come in. A trend over the full 1957–2002 period can carry that discontinuity.
  • With only 23 pressure levels, compare with ERA-Interim or ERA5 (37 levels) on the levels they share.

Notices and change history

2023-06-01 · Critical · Decommissioning of ECMWF Public Datasets service — ECMWF web and Web API downloads end

As announced on 2 March 2023, ECMWF decommissioned the Public Datasets service (web interface and Web API access), so ERA-40 can no longer be downloaded publicly from ECMWF. ECMWF names no alternative access route for ERA-40; use the NCAR GDEX or CEDA copies.

Read the original

2022-06 (day not given) · Info · Access disruptions during the move of the ECMWF archive (MARS) to Bologna

Because MARS moved to the new data centre in Bologna, ECMWF warned of no or degraded access to ERA-40 at times between June and October 2022 (now past).

Read the original

References for your paper

Double-check before using in a paper

The citations below were compiled by the maintainer and may contain errors. Always double-check DOIs, authors, years and access-date formats against the provider's official dataset page and your journal's guidelines.

Dataset citation

NCAR GDEX surface and flux (d117000) — DOI 10.5065/S4S2-R159

European Centre for Medium-Range Weather Forecasts (2004): ERA-40 Global Surface and Flux Data. NSF National Center for Atmospheric Research. https://doi.org/10.5065/S4S2-R159 (Accessed DD MMM YYYY)

Show BibTeX
@misc{era40_d117000,
  author    = {{European Centre for Medium-Range Weather Forecasts}},
  title     = {{ERA-40} Global Surface and Flux Data},
  year      = {2004},
  publisher = {NSF National Center for Atmospheric Research},
  doi       = {10.5065/S4S2-R159},
  note      = {Accessed DD MMM YYYY}
}

NCAR GDEX 6-hourly pressure-level analysis (d117001) — DOI 10.5065/WQZB-A142

European Centre for Medium-Range Weather Forecasts (2004): ERA-40 Global Upper Air Pressure Level Analysis. NSF National Center for Atmospheric Research. https://doi.org/10.5065/WQZB-A142 (Accessed DD MMM YYYY)

NCAR GDEX 2.5° pressure-level monthly means (d120001) — DOI 10.5065/R275-GB48

European Centre for Medium-Range Weather Forecasts (2004): ERA-40 Monthly Means of 2.5 Degree Upper Air Pressure Level Analysis. NSF National Center for Atmospheric Research. https://doi.org/10.5065/R275-GB48 (Accessed DD MMM YYYY)

Reference papers

ERA-40 reference paper — DOI 10.1256/qj.04.176

Uppala, S. M., Kållberg, P. W., Simmons, A. J., Andrae, U., Da Costa Bechtold, V., Fiorino, M., et al. (2005): The ERA-40 re-analysis. Quarterly Journal of the Royal Meteorological Society, 131(612), 2961–3012.

Show BibTeX
@article{uppala2005era40,
  author  = {Uppala, S. M. and K{\"a}llberg, P. W. and Simmons, A. J. and Andrae, U. and Da Costa Bechtold, V. and Fiorino, M. and others},
  title   = {The {ERA-40} re-analysis},
  journal = {Quarterly Journal of the Royal Meteorological Society},
  volume  = {131},
  number  = {612},
  pages   = {2961--3012},
  year    = {2005},
  doi     = {10.1256/qj.04.176}
}

ERA-40 archive report (optional, no DOI)

Kållberg, P., Simmons, A., Uppala, S., Fuentes, M. (2004): The ERA-40 archive. ERA-40 Project Report Series, No. 17, ECMWF, Reading, UK (revised October 2007).

Acknowledgements

Credit ECMWF as the producer and name the archive you actually used (the NCAR GDEX dataset DOI or the CEDA catalogue record). GDEX provides the data on condition that users accept the ECMWF terms of use.

If this page helped, please acknowledge the Korean Climate Data Navigator

Please add the sentence below to the Acknowledgements of your paper.

Acknowledgements

Information on the datasets used in this study was compiled with the help of the Korean Climate Data Navigator (KCDN) (Sim, 2026; https://doi.org/10.5281/zenodo.23300923).