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ERA-15

ECMWF 15-year Reanalysis (ERA-15)

Discontinued

No longer updated

ECMWF's first reanalysis, produced once in the mid-1990s and never extended. It is no longer listed among ECMWF's public download services and is now most easily obtained from the copies archived at NSF NCAR GDEX and CEDA (UK). GDEX recommends it for "ancillary use only", so use ERA5 unless you are reproducing older studies or comparing reanalysis generations.

Successor: ERA-40 (currently recommended: ERA5) — The direct successor was ERA-40 (1957–2002), followed by ERA-Interim; ECMWF's current reanalysis is ERA5 (1940 to present, about 31 km). The link points to the ERA5 page on the CDS.

At a glance

Item Details
Section Atmosphere › Reanalyses
Type Reanalysis
Domains Atmosphere, Land
Provider ECMWF
Period 1979-01 ~ 1993-12
Coverage Global
Horizontal resolution Spectral T106 (~1.125°) / reduced Gaussian N80 / regular 2.5° × 2.5° latitude–longitude grid
Vertical resolution 31 model levels / 17 pressure levels (1000–10 hPa)
Temporal resolution 6-hourly analyses (00, 06, 12, 18 UTC); monthly means separately
Update frequency Ended (production completed in the mid-1990s)
Licence NCAR GDEX copy — Creative Commons Attribution 4.0 International plus ECMWF Terms of Use / CEDA copy — ECMWF ERA products licence
Account required Yes

Note on period: January 1979 to December 1993 (15 years) at ECMWF and NCAR GDEX. The CEDA archive holds "a long time-series (January 1979 - February 1994) of consistent meteorological analyses", i.e. it also includes data to the end of February 1994.

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 first reanalysis, which re-analysed 1979–1993 with "a special version of their 1995 operational data assimilation system and model" held fixed throughout. It used optimal interpolation (OI) and a T106, 31-level model and, together with the contemporaneous NCEP/NCAR reanalysis, is classed as a first-generation reanalysis. Lessons learned (handling of observation biases, quality-control blacklists and more) were carried into ERA-40.

What changes with the successor

ERA-15 → ERA-40

The move from the first generation (optimal interpolation, T106L31) to the second (3D-Var, T159L60) extended the record back to 1957 and added direct assimilation of satellite radiances and a coupled ocean-wave model.

Aspect ERA-15 ERA-40
Period 1979–1993 (15 years) 1957-09 to 2002-08 (45 years)
Horizontal resolution T106 (~1.125°, ~125 km Gaussian grid) T159 (reduced Gaussian N80, ~125 km grid spacing)
Vertical resolution and model top 31 model levels (top at about 10 hPa) 60 model levels (top at about 0.1 hPa)
Pressure levels archived 17 levels (1000–10 hPa) 23 levels
Data assimilation Optimal interpolation (OI), 6-hourly cycle 3D-Var (FGAT), 6-hourly cycle
Use of satellite data TOVS cloud-cleared radiances converted by 1D-Var retrievals, used only below 100 hPa (not used above 100 hPa between 20°N and 20°S) Direct assimilation of satellite radiances from VTPR, TOVS, SSM/I, ATOVS and others (VTPR and SSU used for the first time)
Ocean waves None Coupled 1.5° ocean-wave model; significant wave height and other wave parameters provided
Model version Based on the 1995 operational system (resolution changed only) IFS CY23r4

Things to watch when switching

  • Model, assimilation and observation usage all differ, so climatologies and variability can differ. Do not mix the two, even over their 1979–1993 overlap.
  • ERA-15 has only 17 pressure levels up to 10 hPa. When reproducing older stratospheric analyses, compare only the pressure levels common to ERA-40.
  • Uppala et al. (2005) judged ERA-40 generally better than ERA-15, but noted excessive tropical oceanic precipitation in the later years and an overly strong Brewer–Dobson circulation in ERA-40. Switching to ERA-40 does not remove the limits for hydrological-cycle and stratospheric studies.
  • Both are discontinued earlier-generation products; use ERA5 for new work.

Sources: Gibson et al. (1997), ERA Description (ERA-15 Report Series No. 1) · Uppala et al. (2005), The ERA-40 re-analysis, QJRMS · Kållberg et al. (2004), The ERA-40 archive (ERA-40 Project Report Series No. 17) · Uppala (2006), From ERA-15 to ERA-40 and ERA-Interim (ECMWF/GEO Workshop) · NCAR Climate Data Guide — ERA-40 · CEDA ERA-15 parameter tables (17 pressure levels)

Compare the two side by side

Available variables

Based on the parameter tables of the ERA-15 data held at CEDA. Names are ECMWF GRIB abbreviations (upper case in the original); current ecCodes shows the same codes as lower-case short names (t, 2t, etc.). The original files are GRIB1.

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

The ERA-15 data archived at NCAR and CEDA are analyses at 00, 06, 12 and 18 UTC, and all variables listed here are instantaneous values at those times. Accumulated forecast fields such as precipitation, radiation and heat fluxes are not in the public parameter tables summarised on this page.

  • The time in the file name (HH in YYMMDDHH = 00, 06, 12, 18) is the analysis time.
  • According to ECMWF documentation, the analyses were produced by 6-hourly optimal interpolation (OI), so each value is the analysed state at that time.
  • For accumulated forecast fields (precipitation, fluxes) or monthly means, check the archive tables (monthly means and forecast accumulations) in the ERA-15 technical report; they are not included in the variable list on this page.

Source: CEDA ERA-15 parameter tables (analysis files)

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 (17)

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-velocity U m s-1 instantaneous
V-velocity V m s-1 instantaneous
Vertical velocity W Pa s-1 instantaneous
Relative humidity R % instantaneous
Vorticity (relative; spectral data) VO s-1 instantaneous
Divergence (spectral data) D s-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 u wind component 10U m s-1 instantaneous
10 metre v wind component 10V m s-1 instantaneous
Skin temperature SKT K instantaneous
Snow depth SD m of water equivalent instantaneous

Land surface

Variable Short name Units Time convention Notes
Soil temperature level 1 STL1 K instantaneous
Soil wetness level 1 SWL1 m of water instantaneous
Surface roughness SR m instantaneous Stored at each analysis time in the analysis files; whether it varies in time is not stated in the official documentation
Albedo AL - instantaneous Stored at each analysis time in the analysis files; whether it varies in time is not stated in the official documentation

The full variable list is in the official documentation.

How to get the data

Practical tips

  • According to ECMWF reports, January 1979 – August 1980 was rerun early in production because of an upper-air humidity error, and June 1990 – October 1992 was rerun because satellite cloud-motion winds (except GMS) had been omitted. If you use an old copy, check that it contains the rerun data.
  • Snow is reset by observations in every analysis cycle, so the water budget (precipitation − evaporation − runoff) does not close. The data are not suitable for hydrological budget calculations.
  • With only 17 pressure levels (top at 10 hPa) and no direct radiance assimilation, this first-generation product is unsuitable for stratospheric or long-term trend work; use ERA5.

Notices and change history

No notices yet.

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 reanalysis (d115000) — DOI 10.5065/EWRQ-NY89

European Centre for Medium-Range Weather Forecasts (1997): ERA-15 Global Surface Reanalysis. NSF National Center for Atmospheric Research. https://doi.org/10.5065/EWRQ-NY89 (Accessed DD MMM YYYY)

Show BibTeX
@misc{era15_d115000,
  author    = {{European Centre for Medium-Range Weather Forecasts}},
  title     = {{ERA-15} Global Surface Reanalysis},
  year      = {1997},
  publisher = {NSF National Center for Atmospheric Research},
  doi       = {10.5065/EWRQ-NY89},
  note      = {Accessed DD MMM YYYY}
}

NCAR GDEX upper-air analyses (d115001) — DOI 10.5065/HS1E-5D24

European Centre for Medium-Range Weather Forecasts (1997): ERA-15 Global Upper Air Analyses. NSF National Center for Atmospheric Research. https://doi.org/10.5065/HS1E-5D24 (Accessed DD MMM YYYY)

Show BibTeX
@misc{era15_d115001,
  author    = {{European Centre for Medium-Range Weather Forecasts}},
  title     = {{ERA-15} Global Upper Air Analyses},
  year      = {1997},
  publisher = {NSF National Center for Atmospheric Research},
  doi       = {10.5065/HS1E-5D24},
  note      = {Accessed DD MMM YYYY}
}

Reference papers

ERA-15 technical report (no DOI)

Gibson, J. K., Kållberg, P., Uppala, S., Hernandez, A., Nomura, A., Serrano, E. (1997): ERA Description. ECMWF Re-Analysis Project Report Series, No. 1, ECMWF, Reading, UK. (Version 2 revised 1999)

Show BibTeX
@techreport{gibson1997era15,
  author      = {Gibson, J. K. and K{\aa}llberg, P. and Uppala, S. and Hernandez, A. and Nomura, A. and Serrano, E.},
  title       = {{ERA} Description},
  institution = {European Centre for Medium-Range Weather Forecasts},
  address     = {Reading, UK},
  type        = {ECMWF Re-Analysis Project Report Series},
  number      = {1},
  year        = {1997},
  url         = {https://www.ecmwf.int/en/elibrary/9584-era-description}
}

Acknowledgements

Credit ECMWF as the producer and give the DOI or catalogue URL of the archive you actually used (NCAR GDEX or CEDA). For the CEDA copy, use the citation given in the CEDA catalogue record verbatim.

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).