Accounting for observation uncertainty and bias due to unresolved scales with the Schmidt-Kalman filter
Data assimilation combines observations with numerical model data, to provide a best estimate of a real system. Errors due to unresolved scales arise when there is a spatio-temporal scale mismatch between the processes resolved by the observations and model. We present theory on error, uncertainty a...
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Veröffentlicht in: | Tellus. Series A, Dynamic meteorology and oceanography Dynamic meteorology and oceanography, 2020-01, Vol.72 (1), p.1-21 |
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Format: | Artikel |
Sprache: | eng |
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