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◆ Journal of Hydrology2026-05-10· Series (stratigraphy)

Simulating sub-daily rainfall time series in the absence of sub-daily observations

F. Cappelli, E. Volpi, A. Langousis, R. Deidda, SM Papalexiou, A. Perdios, S. Grimaldi

原始摘要(英文原文)· Original abstract
• Novel framework to simulate sub-daily rainfall without sub-daily data. • Combines CoSMoS-2s daily model and multifractal random cascade model. • Calibration requires only daily rainfall and IDF scaling exponent. • Tested on 70 Arno Basin stations using 15-min records as benchmark. • Accurately reproduces IDF slopes, autocorrelation, and dry frequency. This paper presents a novel framework for simulating sub-daily rainfall time series in the absence of sub-daily observations, which are typically essential for calibrating conventional approaches. The proposed approach combines two classes of models: a daily rainfall model that generates long synthetic daily time series and a disaggregation model based on multifractal theory to refine the temporal resolution to sub-daily scales. The implemented procedure is parsimonious and relies solely on the observed daily rainfall time series and the power law exponent n of the intensity–duration–frequency curves, information widely available to practitioners. The framework was tested on a challenging case study consisting of 70 rain gauges in the Arno River basin (Italy), each with 20 years of continuous 15-minute rainfall data. The performance was evaluated by comparing key statistical attributes estimated from the benchmark dataset and the simulated rainfall time series at 15-minute temporal resolution, such as the dry frequency, the autocorrelation at lags 1 and 10, and the dependence of rainfall intensity on the duration of spatial averaging and return period as embodied in the well-established notion of intensity–duration–frequency (IDF) curves. The results show promising agreement, despite the limited sample size, which introduces some calibration challenges. The relative errors of the selected attributes fall within ± 15% for most of the analyzed time series, indicating that the framework offers a valuable alternative for hydrological studies, particularly in contexts where sub-daily observations are scarce or entirely absent.
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