ERA-Interim¶
ECMWF Interim Reanalysis (ERA-Interim)
Discontinued
No longer updated
Production stopped on 31 August 2019, and ERA-Interim has been superseded by ERA5. Web API (Public Datasets) access ended on 1 June 2023; the data remain available through the Climate Data Store (CDS) API "until further notice", by script only (no web-form download). A copy is also kept at NCAR GDEX. Unless you are reproducing older studies, use ERA5.
Successor: ERA5 — 1940 to present, about 31 km, 137 levels, hourly. ECMWF strongly advises ERA-Interim users to migrate to ERA5. The two use different models and data assimilation systems, so climatologies and trends can differ — do not splice them into one time series.
At a glance¶
| Item | Details |
|---|---|
| Section | Atmosphere › Reanalyses |
| Type | Reanalysis |
| Domains | Atmosphere, Land, Ocean waves |
| Provider | ECMWF (now distributed by the Copernicus Climate Change Service, C3S) |
| Period | 1979-01 ~ 2019-08 |
| Coverage | Global |
| Horizontal resolution | Spectral T255 / reduced Gaussian grid N128 (around 80 km) / ocean waves 1.0° × 1.0° |
| Vertical resolution | 60 model levels (top at 0.1 hPa) / 37 pressure levels (1000–1 hPa) / 16 potential temperature levels / potential vorticity level ±2 PVU |
| Temporal resolution | Analyses 6-hourly (00, 06, 12, 18 UTC), forecasts 3-hourly (monthly means provided separately) |
| Update frequency | Ended (August 2019) |
| Licence | ERA-Interim Product licence (CDS) / NCAR GDEX copy under CC BY 4.0 + ECMWF terms of use |
| Account required | Yes |
Note on period: 1 January 1979 to 31 August 2019. The 1979–1988 segment was produced later, in 2011.
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¶
The ECMWF global atmospheric reanalysis that succeeded ERA-40, covering 1 January 1979 to 31 August 2019. It was the first ECMWF reanalysis to make full use of 12-hour 4D-Var data assimilation and variational bias correction of satellite radiances (VarBC), and was among the most widely cited reanalyses in climate research of the 2010s. It has been superseded by ERA5.
What changed from the previous dataset
What changes with the successor¶
ERA-Interim → ERA5¶
Transition: 2019-08
Much higher resolution (79 km→31 km, 60→137 levels) and output frequency (6-hourly→hourly), plus ensemble-based uncertainty estimates and climate-oriented forcing; distribution moved to the CDS.
| Aspect | ERA-Interim | ERA5 |
|---|---|---|
| Period | 1979-01–2019-08 (ended) | 1940-01–present (near-real-time updates, about 5-day latency) |
| Horizontal resolution | About 79 km (T255) | About 31 km (TL639); ensemble about 62–63 km |
| Vertical resolution and model top | 60 levels, top at 0.1 hPa | 137 levels, top at 0.01 hPa |
| Model and data assimilation | IFS CY31r2, 4D-Var | IFS CY41r2, 4D-Var |
| Output frequency | Analyses 6-hourly, forecasts 3-hourly | Hourly for both analyses and forecasts (ensemble 3-hourly) |
| Uncertainty information | None | Uncertainty from a 10-member Ensemble of Data Assimilations (EDA) |
| Forcing (SST, sea ice, radiation) | As in operations at the time (inconsistent SST) | Climate-oriented (CMIP5 greenhouse gases, volcanic aerosols, etc.; consistent SST and sea ice) |
| Observations and bias correction | ERA-40 observations + GTS; VarBC for satellite radiances only; RTTOV-7 clear-sky radiances | Reprocessed datasets and new satellites added; VarBC extended to ozone, aircraft and surface pressure; RTTOV-11 all-sky radiances |
| Number of single-level parameters | About 100 | More than 240 (some ERA-Interim parameters are not available) |
| Accumulation reference | Accumulated from the start of the forecast | Accumulated since the previous post-processing (1-hour accumulations in the hourly data) |
| Performance | Global-mean correlation with GPCP monthly precipitation 67% | Correlation 77%; better fit to radiosondes for tropospheric temperature, wind and humidity; reforecast skill improved by up to one day |
| Distribution | ECMWF Public Datasets / Web API (closed 2023) → now CDS API only | Copernicus Climate Data Store (CDS) |
Things to watch when switching
- Do not splice the two into one series. Climatologies and trends differ even over the 1979–2019 overlap, so long-term analyses are safest recomputed entirely with ERA5.
- The accumulation convention differs. ERA-Interim accumulates from the forecast start (3, 6, 9, 12 hours, etc.) and needs differencing, whereas ERA5 hourly data are 1-hour accumulations. Running old scripts unchanged will give wrong precipitation and radiation.
- ERA5 has a pronounced cold bias in the lower stratosphere in 2000–2006, for which a separate rerun, ERA5.1, exists. If you work on stratospheric temperature, humidity or ozone, use ERA5.1 for that period.
- ERA5 provides ensemble spread, but the ensemble has a different resolution and output interval (3-hourly) from the main (HRES) data.
Sources: ECMWF — What are the changes from ERA-Interim to ERA5 and ERA5-Land? · Hersbach et al. (2020), The ERA5 global reanalysis, QJRMS · Dee et al. (2011), The ERA-Interim reanalysis, QJRMS · ECMWF Technical Memo — Global stratospheric temperature bias and other stratospheric aspects of ERA5 and ERA5.1 · NCAR GDEX — ERA5.1 Corrections to ERA5 Stratospheric Temperature 2000-2006
Available variables¶
Main parameters from the parameter tables of the official ECMWF ERA-Interim documentation and the ERA-Interim archive report. Names are ECMWF GRIB short names. The data are GRIB1, and accumulated fields (precipitation, radiation, heat fluxes) are accumulated from the start of the forecast.
Time-stamp convention — instantaneous, mean or accumulated? — click to show
Analysis fields are instantaneous values at 00, 06, 12 and 18 UTC. Accumulated fields such as precipitation, radiation and heat fluxes come only from forecasts started at 00 or 12 UTC, and are accumulated from the start of the forecast to the selected step (3, 6, 9, 12 hours, etc.).
- Accumulations run from the start of the forecast. Example: tp at step 12 of the 00 UTC forecast = 12-hour precipitation from 00 to 12 UTC. Get 3-hour amounts by differencing adjacent steps (step 6 − step 3).
- ECMWF's guidance for daily precipitation is to add step 12 of the 00 UTC forecast and step 12 of the 12 UTC forecast.
- To convert accumulated radiation and heat fluxes in W m-2 s (= J m-2) to mean fluxes (W m-2), divide by the accumulation period in seconds (e.g. 43200 for 12 hours).
- Minimum/maximum fields (e.g. mx2t) refer to the period since the previous post-processing (archived step). Example: step 9 of the 00 UTC forecast = 06–09 UTC.
- Among the monthly means, moda (monthly means of daily means) holds analysis and instantaneous forecast fields only; monthly means of accumulated fields are in the separate mdfa stream (monthly means of daily forecast accumulations).
Source: ERA-Interim documentation (Copernicus Knowledge Base)
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
Surface and single level¶
| Variable | Short name | Units | Time convention | Notes |
|---|---|---|---|---|
| 2 metre temperature | 2t |
K | instantaneous | |
| 2 metre dewpoint temperature | 2d |
K | instantaneous | |
| 10 metre U wind component | 10u |
m s-1 | instantaneous | |
| 10 metre V wind component | 10v |
m s-1 | instantaneous | |
| Mean sea level pressure | msl |
Pa | instantaneous | |
| Surface pressure | sp |
Pa | instantaneous | |
| Sea surface temperature | sst |
K | instantaneous | |
| Sea-ice cover | ci |
0-1 | instantaneous | |
| Skin temperature | skt |
K | instantaneous | |
| Total cloud cover | tcc |
0-1 | instantaneous | |
| Total column water vapour | tcwv |
kg m-2 | instantaneous | |
| Boundary layer height (forecast) | blh |
m | instantaneous | Forecast only (value at the forecast step) |
Accumulated forecast fields¶
| Variable | Short name | Units | Time convention | Notes |
|---|---|---|---|---|
| Total precipitation | tp |
m of water | Since forecast start accumulated | |
| Surface solar radiation downwards | ssrd |
W m-2 s | Since forecast start accumulated | |
| Surface thermal radiation downwards | strd |
W m-2 s | Since forecast start accumulated | |
| Top net thermal radiation | ttr |
W m-2 s | Since forecast start accumulated | |
| Surface sensible heat flux | sshf |
W m-2 s | Since forecast start accumulated | |
| Surface latent heat flux | slhf |
W m-2 s | Since forecast start accumulated |
Pressure levels (37 levels)¶
| 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 | |
| U component of wind | u |
m s-1 | instantaneous | |
| V component of wind | 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 | |
| Specific cloud liquid and ice water content | clwc, ciwc |
kg kg-1 | instantaneous |
Ocean waves (1.0° grid)¶
| Variable | Short name | Units | Time convention | Notes |
|---|---|---|---|---|
| Significant height of combined wind waves and swell | swh |
m | instantaneous | |
| Mean wave direction | mwd |
degree | instantaneous | |
| Mean wave period | mwp |
s | instantaneous |
Land surface and invariants¶
| 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 | |
| Land-sea mask | lsm |
0-1 | static | |
| Geopotential at the surface (orography) | z |
m2 s-2 | static | divide by 9.80665 for terrain height (m) |
The full variable list is in the official documentation.
How to get the data¶
- Copernicus Climate Data Store (CDS) — ERA-Interim — CDS API (cdsapi) scripts only
- Requires an ECMWF account, and you must first accept the ERA-Interim Product licence on the dataset page. There is no web-form download; data can be retrieved only with scripts as described on the ECMWF help page. Format is GRIB1.
- ECMWF help — How to download ERA-Interim data from the ECMWF data archive — Documentation (example CDS API requests)
- NSF NCAR GDEX — ERA-Interim Project (d627000) — Web download / subsetting / NCAR HPC (GLADE)
- NCAR account required (for subsetting, etc.). GRIB1, about 39 TB in total. GDEX flags this dataset as recommended for ancillary use only and superseded by a newer dataset.
Practical tips¶
- ECMWF known issue: CAPE is zero at forecast step 3 (03 and 15 UTC) because of an error in how ERA-Interim calculated CAPE at that step. Do not use CAPE at those times.
- At forecast steps 3/6/9/15/18/21, SST over land is 0 °C rather than missing. Always mask out land with the land-sea mask (lsm).
- The NCAR Climate Data Guide lists as main limitations an overly strong hydrological cycle over the oceans (precipitation and evaporation) and a warm, moist bias below 850 hPa in the Arctic relative to radiosondes.
- Old Web API scripts (ecmwfapi, class=ei) have not worked since June 2023. To reproduce earlier work, rewrite them for the CDS API or use the NCAR copy.
Notices and change history¶
2024-09-26 · Warning · Goodbye legacy Climate Data Store — ERA-Interim CDS API scripts also need a new account and key
The legacy CDS has been decommissioned and replaced by the new CDS. Because ERA-Interim is available only through the CDS API, scripts that use an old .cdsapirc (url and key) must be updated with the new ECMWF account details.
2023-06-01 · Critical · Decommissioning of ECMWF Public Datasets service (Web API)
As announced on 2 March 2023, the ECMWF Public Datasets service was retired on 1 June 2023, so ERA-Interim can no longer be retrieved with the Web API (ecmwfapi). ECMWF strongly advises migrating to ERA5 and keeps CDS API access open for those who still need ERA-Interim.
2019-08-31 · Info · ERA-Interim production stopped
Production of ERA-Interim stopped on 31 August 2019. Its successor is ERA5.
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¶
CDS dataset — DOI 10.24381/cds.f2f5241d
Copernicus Climate Change Service (2023): ERA-Interim atmospheric reanalysis. ECMWF. DOI: 10.24381/cds.f2f5241d (Accessed on DD-MMM-YYYY)
Show BibTeX
NCAR GDEX copy (d627000) — DOI 10.5065/D6CR5RD9
European Centre for Medium-Range Weather Forecasts (2009): ERA-Interim Project. NSF National Center for Atmospheric Research. https://doi.org/10.5065/D6CR5RD9 (Accessed DD MMM YYYY)
Show BibTeX
Reference papers¶
ERA-Interim reference paper — DOI 10.1002/qj.828
Dee, D. P., Uppala, S. M., Simmons, A. J., Berrisford, P., Poli, P., Kobayashi, S., et al. (2011): The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Quarterly Journal of the Royal Meteorological Society, 137(656), 553–597.
Show BibTeX
@article{dee2011erainterim,
author = {Dee, D. P. and Uppala, S. M. and Simmons, A. J. and Berrisford, P. and Poli, P. and Kobayashi, S. and others},
title = {The {ERA-Interim} reanalysis: configuration and performance of the data assimilation system},
journal = {Quarterly Journal of the Royal Meteorological Society},
volume = {137},
number = {656},
pages = {553--597},
year = {2011},
doi = {10.1002/qj.828}
}
Archive (data organisation) report (optional)
Berrisford, P., Dee, D. P., Poli, P., Brugge, R., Fielding, M., Fuentes, M., Kållberg, P. W., Kobayashi, S., Uppala, S., Simmons, A. (2011): The ERA-Interim archive Version 2.0. ERA Report Series No. 1, ECMWF, Reading.
Acknowledgements¶
If you obtained the data from the CDS, give the CDS DOI above and the access date, and attribute the Copernicus programme/C3S. If you used the NCAR copy, also give the GDEX DOI and, under the ECMWF terms of use, acknowledge ECMWF as the source of the data.
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Please add the sentence below to the Acknowledgements of your paper.