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Optimising ensemble streamflow predictions with bias correction and data assimilation techniques

Tanguy, Maliko ORCID: https://orcid.org/0000-0002-1516-6834; Eastman, Michael ORCID: https://orcid.org/0000-0002-8212-5872; Chevuturi, Amulya ORCID: https://orcid.org/0000-0003-2815-7221; Magee, Eugene ORCID: https://orcid.org/0009-0004-9043-7886; Cooper, Elizabeth ORCID: https://orcid.org/0000-0002-1575-4222; Johnson, Robert H.B. ORCID: https://orcid.org/0009-0009-9413-3413; Facer-Childs, Katie ORCID: https://orcid.org/0000-0003-1060-9103; Hannaford, Jamie ORCID: https://orcid.org/0000-0002-5256-3310. 2025 Optimising ensemble streamflow predictions with bias correction and data assimilation techniques. Hydrology and Earth System Sciences, 29 (6). 1587-1614. 10.5194/hess-29-1587-2025

Abstract
This study evaluates the efficacy of bias correction (BC) and data assimilation (DA) techniques in refining hydrological model predictions. Both approaches are routinely used to enhance hydrological forecasts, yet there have been no studies that have systematically compared their utility. We focus on the application of these techniques to improve operational river flow forecasts in a diverse dataset of 316 catchments in the United Kingdom (UK), using the ensemble streamflow prediction (ESP) method applied to the (Génie Rural à 4 paramètres Journalier) (GR4J) hydrological model. This framework is used in operational seasonal forecasting, providing a suitable test bed for method application. Assessing the impacts of these two approaches on model performance and forecast skill, we find that BC yields substantial and generalised improvements by rectifying errors after simulation. Conversely, DA, adjusting model states at the start of the forecast period, provides more subtle enhancements, with the biggest effects seen at short lead times in catchments impacted by snow accumulation or melting processes in winter and spring and catchments with a high baseflow index (BFI) in summer. The choice between BC and DA involves trade-offs considering conceptual differences, computational demands, and uncertainty handling. Our findings emphasise the need for selective application based on specific scenarios and user requirements. This underscores the potential for developing a selective system (e.g. a decision tree) to refine forecasts effectively and deliver user-friendly hydrological predictions. While further work is required to enable implementation, this research contributes insights into the relative strengths and weaknesses of these forecast enhancement methods. These could find application in other forecasting systems, aiding the refinement of hydrological forecasts and meeting the demand for reliable information by end-users.
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