Multi-scale dynamics and mesoscale drivers of the catastrophic September 2022 Marche (central Italy) flood
4 affiliations
- 1University of Salento (Lecce, Italy)
- 2Parthenope University of Naples (Naples, Italy)
- 3University of Padua (Padua, Italy)
- 4National Research Council (Rome, Italy)
Abstract
The catastrophic flood that hit the Marche region (central Italy) on 15 September 2022 has been analyzed using high-resolution Weather Research and Forecasting (WRF) model simulations. The convective rainfall event responsible for the flood was favored by the passage of warm, moist air masses that interacted with the central Apennines. The convective cells, triggered by the rough orography of the area, formed quasi-stationary bands that caused high rainfall accumulation in limited areas. The formation of these rainbands was sustained by the interaction between the low-level flow and the local topography, which generated a persistent low-level convergence line extending downwind from Mount Amiata northeastward towards the Apennines. The observed vertical profile upstream of the orography reveals that the instability was initially suppressed by an inversion layer and was released only when the humid air arrived at low levels and eroded the inhibition. Furthermore, the simulations suggest that gravity waves induced by the mountains may have helped to sustain the vertical motion of the impinging air, and highlight the role of upper-level dynamics (passage of a jet streak). The comparison with surface stations shows that the simulation underestimates peak accumulations (160–180 mm simulated vs. over 400 mm observed), delays the event by 1–2 h, and misses the final phase. However, overall the model captures the system's spatial position, orientation, and quasi-stationary evolution associated with orographic anchoring. Rather than evaluating predictive skill in an operational-like perspective, this study investigates the physical precursors and dynamical mechanisms of the event. Sensitivity experiments reveal a strong dependence on initial and boundary conditions. A comparison of the control run (forced with Global Data Assimilation System (GDAS) analysis/forecasts) with a simulation driven by European Centre for Medium-Range Weather Forecasts (ECMWF) analysis/forecasts shows a strong sensitivity to the low-level dynamics. Although the large-scale upper-level forcing is almost identical, the ECMWF-driven forecast fails to reproduce the correct amount and distribution of rainfall due to a weaker surface pressure gradient, reduced moisture advection, and lower instability at the time of the event. Specifically, the simulation forced with the ECMWF data anticipates the arrival of the moist air mass, determining a timing mismatch between the low-level supply of moist air (and the consequent release of instability) and the upper-level forcing. This lack of synchronization shifts the rainfall away from the observed area.
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BibTeX
@article{berton2026multiscale,
title = {{Multi-scale dynamics and mesoscale drivers of the catastrophic September 2022 Marche (central Italy) flood}},
author = {Matteo Berton and Elenio Avolio and Mario Marcello Miglietta},
journal = {Natural Hazards and Earth System Sciences},
year = {2026},
month = nov,
doi = {10.5194/nhess-26-5541-2026},
url = {https://nhess.copernicus.org/articles/26/5541/2026/},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Multi-scale dynamics and mesoscale drivers of the catastrophic September 2022 Marche (central Italy) flood
AU - Matteo Berton
AU - Elenio Avolio
AU - Mario Marcello Miglietta
PY - 2026
DA - 2026/11/03
JO - Natural Hazards and Earth System Sciences
DO - 10.5194/nhess-26-5541-2026
UR - https://nhess.copernicus.org/articles/26/5541/2026/
AB - The catastrophic flood that hit the Marche region (central Italy) on 15 September 2022 has been analyzed using high-resolution Weather Research and Forecasting (WRF) model simulations. The convective rainfall event responsible for the flood was favored by the passage of warm, moist air masses that interacted with the central Apennines. The convective cells, triggered by the rough orography of the area, formed quasi-stationary bands that caused high rainfall accumulation in limited areas. The formation of these rainbands was sustained by the interaction between the low-level flow and the local topography, which generated a persistent low-level convergence line extending downwind from Mount Amiata northeastward towards the Apennines. The observed vertical profile upstream of the orography reveals that the instability was initially suppressed by an inversion layer and was released only when the humid air arrived at low levels and eroded the inhibition. Furthermore, the simulations suggest that gravity waves induced by the mountains may have helped to sustain the vertical motion of the impinging air, and highlight the role of upper-level dynamics (passage of a jet streak). The comparison with surface stations shows that the simulation underestimates peak accumulations (160–180 mm simulated vs. over 400 mm observed), delays the event by 1–2 h, and misses the final phase. However, overall the model captures the system's spatial position, orientation, and quasi-stationary evolution associated with orographic anchoring. Rather than evaluating predictive skill in an operational-like perspective, this study investigates the physical precursors and dynamical mechanisms of the event. Sensitivity experiments reveal a strong dependence on initial and boundary conditions. A comparison of the control run (forced with Global Data Assimilation System (GDAS) analysis/forecasts) with a simulation driven by European Centre for Medium-Range Weather Forecasts (ECMWF) analysis/forecasts shows a strong sensitivity to the low-level dynamics. Although the large-scale upper-level forcing is almost identical, the ECMWF-driven forecast fails to reproduce the correct amount and distribution of rainfall due to a weaker surface pressure gradient, reduced moisture advection, and lower instability at the time of the event. Specifically, the simulation forced with the ECMWF data anticipates the arrival of the moist air mass, determining a timing mismatch between the low-level supply of moist air (and the consequent release of instability) and the upper-level forcing. This lack of synchronization shifts the rainfall away from the observed area.
SN - 1684-9981
ER -