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Time-correlated model error in the (ensemble) Kalman smoother.
Javier Amezcua1, Peter Jan van Leeuwen1
1Department of Meteorology and National Centre for Earth Observation, University of Reading, UK.
Incorrectly modeling temporal correlations in model errors significantly impacts data assimilation solutions. Overestimating correlation timescales in Kalman smoothers yields worse results than underestimating them.
Area of Science:
- Data assimilation
- Numerical modeling
- Geosciences
Background:
- Data assimilation often assumes perfect models, neglecting model equation errors.
- Current methods for incorporating model errors use ad-hoc approximations with limited understanding of their impact.
- Approximations in model errors can interact with finite-ensemble-size effects.
Purpose of the Study:
- To systematically evaluate the influence of model error approximations in weak-constraint ensemble smoothers.
- To analyze the effects of incorrect temporal correlations in model errors within Kalman and ensemble Kalman smoothers.
- To understand the interaction between model error approximations and finite-ensemble-size effects.
Main Methods:
- Investigated incorrect temporal correlations in additive model errors for Kalman smoothers.
- Analyzed ensemble Kalman smoothers, considering time-correlation errors and finite ensemble effects.
- Disentangled contributions from different approximations assuming small errors.
Main Results:
- Incorrect correlation time-scales in Kalman smoothers negatively affect solutions; overestimation is worse than underestimation.
- Ensemble Kalman smoother gain is affected by time-correlation and finite ensemble errors.
- Analysis mean is impacted by time-correlation and unexpected finite-ensemble effects.
- Analysis covariance is influenced by time-correlation errors and an in-breeding term.
Conclusions:
- This study provides the first thorough analysis of time-correlation and finite-ensemble-size errors in weak-constraint ensemble smoothers.
- Findings will aid in developing more robust data assimilation methods for applications like numerical weather prediction.
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