Ensemble Data Assimilation without Perturbed Observations
Top Cited Papers
- 1 July 2002
- journal article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 130 (7) , 1913-1924
- https://doi.org/10.1175/1520-0493(2002)130<1913:edawpo>2.0.co;2
Abstract
The ensemble Kalman filter (EnKF) is a data assimilation scheme based on the traditional Kalman filter update equation. An ensemble of forecasts are used to estimate the background-error covariances needed to compute the Kalman gain. It is known that if the same observations and the same gain are used to update each member of the ensemble, the ensemble will systematically underestimate analysis-error covariances. This will cause a degradation of subsequent analyses and may lead to filter divergence. For large ensembles, it is known that this problem can be alleviated by treating the observations as random variables, adding random perturbations to them with the correct statistics. Two important consequences of sampling error in the estimate of analysis-error covariances in the EnKF are discussed here. The first results from the analysis-error covariance being a nonlinear function of the background-error covariance in the Kalman filter. Due to this nonlinearity, analysis-error covariance estimates ... Abstract The ensemble Kalman filter (EnKF) is a data assimilation scheme based on the traditional Kalman filter update equation. An ensemble of forecasts are used to estimate the background-error covariances needed to compute the Kalman gain. It is known that if the same observations and the same gain are used to update each member of the ensemble, the ensemble will systematically underestimate analysis-error covariances. This will cause a degradation of subsequent analyses and may lead to filter divergence. For large ensembles, it is known that this problem can be alleviated by treating the observations as random variables, adding random perturbations to them with the correct statistics. Two important consequences of sampling error in the estimate of analysis-error covariances in the EnKF are discussed here. The first results from the analysis-error covariance being a nonlinear function of the background-error covariance in the Kalman filter. Due to this nonlinearity, analysis-error covariance estimates ...Keywords
This publication has 21 references indexed in Scilit:
- An Ensemble Adjustment Kalman Filter for Data AssimilationMonthly Weather Review, 2001
- Distance-Dependent Filtering of Background Error Covariance Estimates in an Ensemble Kalman FilterMonthly Weather Review, 2001
- Adaptive Sampling with the Ensemble Transform Kalman Filter. Part I: Theoretical AspectsMonthly Weather Review, 2001
- A Monte Carlo Implementation of the Nonlinear Filtering Problem to Produce Ensemble Assimilations and ForecastsMonthly Weather Review, 1999
- ReplyMonthly Weather Review, 1999
- Construction of correlation functions in two and three dimensionsQuarterly Journal of the Royal Meteorological Society, 1999
- Analysis Scheme in the Ensemble Kalman FilterMonthly Weather Review, 1998
- Assimilation of Geosat Altimeter Data for the Agulhas Current Using the Ensemble Kalman Filter with a Quasigeostrophic ModelMonthly Weather Review, 1996
- Sequential data assimilation with a nonlinear quasi‐geostrophic model using Monte Carlo methods to forecast error statisticsJournal of Geophysical Research: Oceans, 1994
- A square root formulation of the Kalman covariance equations.AIAA Journal, 1968