Preprints
https://doi.org/10.5194/egusphere-2026-4515
https://doi.org/10.5194/egusphere-2026-4515
30 Jul 2026
 | 30 Jul 2026
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

A nested time-window framework for evaluating sub-daily precipitation extremes in two convection permitting model datasets

Oliver Carlo, Giusy Fedele, Paolo Stocchi, Sandro Calmanti, Mario Raffa, Paola Mercogliano, and Piero Lionello

Abstract. High-resolution convection-permitting models (CPMs) provide vital datasets for studying localized extreme precipitation and associated multi-hazard risks like landslides and floods. Yet validating CPM datasets against observations remains a challenge. This study evaluates two sub-daily CPM datasets, VHR-REA_IT and LAM-HIND, against observations over a 10-year period across two Italian regions: Emilia-Romagna and Campania. Extreme precipitation is defined using the 95th percentile of wet-event intensities across accumulation durations of 1, 2, 4, 12, and 24 hours.

Conventional verification metrics only partially assess dataset performance and hide differences in the temporal organization of precipitation extremes. Therefore, a new nested time-window framework is presented to better capture the association between short- and long-duration time window extremes (STWEs and LTWEs, respectively). Observations show that STWEs and LTWEs are only partially associated. Depending on region and season, around 7–15 % of observed 1-hour STWEs are embedded within 24-hour LTWEs. CPMs reproduce this cross-timescale organisation substantially better than ERA5, yet are overestimated, indicating excess temporal persistence of simulated heavy-rainfall. Consequently, LTWEs are more dependable than STWEs, as CPMs distribute short extreme precipitation bursts into longer durations with persistently higher volumes.

Differences between the CPM datasets are small. LAM-HIND exhibits subtly higher detection and event-overlap scores but a higher false-alarm rate and stronger cross-timescale coupling overestimation. VHR-REA_IT more closely reproduces the observed temporal association between short- and long-duration extremes. These differences may stem from the ‘double penalty’ effect, choice of an intermediate nesting strategy, and sensitivity in resolving sub-grid turbulent fluxes. However, they are both substantially improved over coarse products like ERA5 for sub-daily extreme precipitation.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Natural Hazards and Earth System Sciences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Share
Oliver Carlo, Giusy Fedele, Paolo Stocchi, Sandro Calmanti, Mario Raffa, Paola Mercogliano, and Piero Lionello

Status: open (until 10 Sep 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Oliver Carlo, Giusy Fedele, Paolo Stocchi, Sandro Calmanti, Mario Raffa, Paola Mercogliano, and Piero Lionello
Oliver Carlo, Giusy Fedele, Paolo Stocchi, Sandro Calmanti, Mario Raffa, Paola Mercogliano, and Piero Lionello
Metrics will be available soon.
Latest update: 30 Jul 2026
Download
Short summary
Conventional metrics miss the temporal organization of precipitation extremes linked to multi-risk hazards. We present a nested time-window framework to capture the coupling between short- and long-duration extremes (STWEs/LTWEs) across two CPM datasets. While CPMs replicate this cross-timescale association substantially better than ERA5 compared to observations, they still overestimate the coupling, indicating an increased temporal persistence bias.
Share