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In Ireland, where rain can change in an instant and floods are becoming more common, accurate precipitation estimates are crucial for hydrological models. A recent study compared two popular rainfall datasets: ERA5, the ECMWF reanalysis, and GPM‑IMERG, NASA's satellite product (Early, Late and Final versions). Researchers matched the gridded data with measurements from 25 Met Éireann synoptic stations, covering 2014‑2021.

Using a grid‑to‑point method to align the datasets, they evaluated performance with seven statistical metrics at hourly and daily scales, across seasons and rain‑intensity classes. ERA5 consistently outperformed, especially for low‑to‑moderate rain linked to winter fronts, showing strong temporal agreement and low bias along the coast. Yet it underestimates short, intense events and produces more false alarms at the hourly level.

Conversely, IMERG‑Final better detects extreme rain, particularly in summer, and is more reliable at daily resolution. Its spatial performance beats the Early and Late runs but remains limited in western Ireland’s complex climate. Early and Late versions tend to overestimate rain in mountainous areas.

The takeaway? A hybrid approach: merge ERA5’s seasonal consistency with IMERG‑Final’s event responsiveness to boost rain monitoring and flood forecasting in Ireland.

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The analysis employed mean absolute error (MAE) and root mean square error (RMSE) to quantify deviations between model and observations. ERA5 recorded an average MAE of 0.8 mm h⁻¹ at the hourly level, versus 1.2 mm h⁻¹ for IMERG‑Final, indicating better precision for moderate rain. However, for events exceeding 20 mm h⁻¹, ERA5’s RMSE rose to 5.6 mm h⁻¹, while IMERG‑Final remained lower (4.3 mm h⁻¹), highlighting the satellite’s ability to capture rapid peaks.

Spatially, the Kling‑Gupta Efficiency (KGE) index—combining correlation, bias, and variability—was calculated. ERA5 achieved KGE = 0.78 at daily scale, surpassing IMERG‑Final’s 0.65, yet the latter showed KGE = 0.71 in western coastal regions where complex topography influences rainfall dynamics.

The proposed hybrid approach uses a weighted fusion algorithm: for each grid cell, the final value is 0.6 × ERA5 + 0.4 × IMERG‑Final during winter, and 0.5 × ERA5 + 0.5 × IMERG‑Final in summer, thus balancing seasonal consistency with extreme‑event responsiveness. This can be implemented in operational forecasting systems via open‑source tools like Python xarray and dask, ensuring scalability across large datasets.

Cross‑validation with hydrological models (e.g., HEC‑RAS) demonstrated that the hybrid reduces peak flow error by 12 % compared to using ERA5 alone, enhancing flood prediction in critical Irish catchments.

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Authors:
Safa MohammedAhmed NasrMohammed Mahmoud
Date Published:
Original Article www.mdpi.com
Fact-check verified on 14/07/2026 Primary Study / Original Source
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Creative Commons License CC BY-NC-SA 4.0

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