Toward robust fine-scale decadal precipitation forecasts through dynamically consistent subsampling
Abstract. Reliable decadal predictions of regional precipitation are critical for managing water-resources and developing climate services, yet they remain a major challenge. To address this gap, we present a 5-step framework that integrates recent advances in decadal predictions of large-scale sea-level pressure (SLP) modes to enhance prediction skill of precipitation at a fine scale resolution. We first identify key atmospheric indices controlling precipitation variability over France, including the winter and summer North Atlantic Oscillation (NAO), the winter West Atlantic Pressure Anomaly, and the summer Mediterranean-Scandinavia index. These indices are predicted through an improved post-processing method applied on the multi-model Decadal Climate Prediction ensemble. The resulting decadal forecasts of the indices are used to select dynamically consistent members from a large uninitialized climate model ensemble, thereby avoiding initial drift from decadal climate predictions. The selected forecasts are then statistically bias-corrected and downscaled to an 8-km grid, providing relevant predictions for local scale and impact studies. The last step of the framework is the skill evaluation: over France, winter precipitation forecast based on the NAO achieve significant Anomaly Correlation Coefficient across 70 % of grid cells. Summer skill, though weaker, improves notably when combining NAO with the North Atlantic Sea Surface Temperatures (significant over 53 % of grid cells). This approach offers a transferable pathway toward actionable, fine scale hydroclimate information at the decadal scale, potentially useful for climate services. The methodology is adaptable to other regions and variables, offering promising opportunities for improving decadal-scale hydroclimate predictions.
In this study, a methodology to produce precipitation predictions over France, at high spatial resolution and at the decadal temporal horizon, is presented and evaluated. The method consists of five sequential steps (index selection, index prediction, subsampling, downscaling, and assessment). Key findings include significant skill enhancements over the extended winter season compared to uninitialised simulations, and weaker but significant improvements over the extended summer season.
This work focuses on a specific domain (France), but the authors highlight that their procedure could be adapted to other geographical regions, which I agree with: for this reason, I believe this study fits well within ESD’s aims and scope. The methodology is novel, and the results presented are substantial and potentially relevant to stakeholders.
The authors put effort into motivating their methodological choices (e.g. Section 3.4), but the organisation of the material could be streamlined and the level of information provided improved in places. In a couple of cases, further discussion would help the interpretation of the results. Finally, this work requires careful editing as it currently contains several grammatical errors. That being said, I did not find major issues with the manuscript and my overall assessment is positive.
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References
Wilks, D., 2006. Statistical methods in the atmospheric sciences, second ed. Elsevier.