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The ensemble transform Schmidt–Kalman filter: A novel method to compensate for observation uncertainty due to unresolved scales

Abstract Data assimilation is a mathematical technique that uses observations to improve model predictions through consideration of their respective uncertainties. Observation error due to unresolved scales occurs when there is a difference in scales observed and modeled. To obtain an optimal estima...

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Detalles Bibliográficos
Principais autores: Zackary Bell, Sarah L. Dance, Joanne A. Waller
Formato: Artigo
Idioma:Inglês
Publicado: Wiley 2025-05-01
Series:Atmospheric Science Letters
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Acceso en liña:https://doi.org/10.1002/asl.1296
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