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No longer updated
Production finished in the early 2000s and the record is no longer updated.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
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¶
- NSF NCAR GDEX — ERA-40 Global Surface and Flux Data (d117000) — Web download (HTTPS) / Globus / subsetting and format conversion
- 6-hourly surface and flux data on the Gaussian grid. Subsetting and format conversion require an NCAR login.
- NSF NCAR GDEX — ERA-40 Monthly Means of 2.5 Degree Upper Air Pressure Level Analysis (d120001) — Web download (HTTPS) / Globus / subsetting
- NSF NCAR GDEX — ERA-40 2.5° surface and flux monthly means (d120000) — Web download (HTTPS) / Globus / subsetting
- NSF NCAR GDEX — ERA-40 Global Upper Air Pressure Level Analysis (d117001) — On request
- When checked on 2026-10-11 the dataset was marked as containing files that are not currently available, so request them through GDEX Contact Us. The 2.5° 6-hourly pressure-level (d118001) and surface (d118000) datasets are in the same state.
- CEDA Archive — ERA-40 model data — Web download
- Requires a CEDA account. Holds data on the reduced Gaussian grid and the regular 2.5° grid; ECMWF data conditions apply.
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.
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).
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
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.
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Please add the sentence below to the Acknowledgements of your paper.