Ensemble Data Assimilation without Perturbed Observations
NOAA Earth System Research Laboratory
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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
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Keywords
- Data assimilation
- Assimilation (phonology)
- Meteorology
- Environmental science
- Climatology
- Geology
- Geography
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