Abstract
We present a modified ensemble Kalman filter that allows a non-Gaussian background error distribution. Using a distribution that decays more slowly than a Gaussian allows the filter to make a larger correction to the background state in cases where it deviates significantly from the truth. For high-dimensional systems, this approach can be used locally. We compare this non-Gaussian filter to its Gaussian counterpart (with multiplicative variance inflation) with the three-dimensional Lorenz-63 model, the 40-dimensional Lorenz-96 model, and Molteni's SPEEDY model, a global model with ∼105 state variables. When observations are sufficiently infrequent and noisy, the non-Gaussian filter yields a significant improvement in analysis and forecast errors.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 225-237 |
| Number of pages | 13 |
| Journal | Tellus, Series A: Dynamic Meteorology and Oceanography |
| Volume | 59 |
| Issue number | 2 |
| DOIs | |
| State | Published - Mar 2007 |
All Science Journal Classification (ASJC) codes
- Oceanography
- Atmospheric Science
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