Review Article
The ERA-Interim reanalysis: configuration and performance of the data assimilation system
Article first published online: 28 APR 2011
DOI: 10.1002/qj.828
Copyright © 2011 Royal Meteorological Society
Issue

Quarterly Journal of the Royal Meteorological Society
Volume 137, Issue 656, pages 553–597, April 2011 Part A
Additional Information
How to Cite
Dee, D. P., Uppala, S. M., Simmons, A. J., Berrisford, P., Poli, P., Kobayashi, S., Andrae, U., Balmaseda, M. A., Balsamo, G., Bauer, P., Bechtold, P., Beljaars, A. C. M., van de Berg, L., Bidlot, J., Bormann, N., Delsol, C., Dragani, R., Fuentes, M., Geer, A. J., Haimberger, L., Healy, S. B., Hersbach, H., Hólm, E. V., Isaksen, L., Kållberg, P., Köhler, M., Matricardi, M., McNally, A. P., Monge-Sanz, B. M., Morcrette, J.-J., Park, B.-K., Peubey, C., de Rosnay, P., Tavolato, C., Thépaut, J.-N. and Vitart, F. (2011), The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q.J.R. Meteorol. Soc., 137: 553–597. doi: 10.1002/qj.828
Publication History
- Issue published online: 28 APR 2011
- Article first published online: 28 APR 2011
- Manuscript Accepted: 23 MAR 2011
- Manuscript Revised: 22 MAR 2011
- Manuscript Received: 21 JAN 2011
- Abstract
- Article
- References
- Cited By
Keywords:
- ERA-40;
- 4D-Var;
- hydrological cycle;
- stratospheric circulation;
- observations;
- forecast model
Abstract
ERA-Interim is the latest global atmospheric reanalysis produced by the European Centre for Medium-Range Weather Forecasts (ECMWF). The ERA-Interim project was conducted in part to prepare for a new atmospheric reanalysis to replace ERA-40, which will extend back to the early part of the twentieth century. This article describes the forecast model, data assimilation method, and input datasets used to produce ERA-Interim, and discusses the performance of the system. Special emphasis is placed on various difficulties encountered in the production of ERA-40, including the representation of the hydrological cycle, the quality of the stratospheric circulation, and the consistency in time of the reanalysed fields. We provide evidence for substantial improvements in each of these aspects. We also identify areas where further work is needed and describe opportunities and objectives for future reanalysis projects at ECMWF. Copyright © 2011 Royal Meteorological Society

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