Abstract

Hydrological monitoring systems relying on radar data and distributed hydrological models are now feasible at large-scale and represent effective early warning systems for flash floods. Here we describe a system that allows hydrological occurrences in terms of streamflow at a national scale to be monitored. We then evaluate its operational application in Italy, a country characterized by various climatic conditions and topographic features. The proposed system exploits a modified conditional merging (MCM) algorithm to generate rainfall estimates by blending data from national radar and rain-gauge networks. Then, we use the merged rainfall fields as input for the distributed and continuous hydrological model, Continuum, to obtain real-time streamflow predictions. We assess its performance in terms of rainfall estimates from MCM, using cross-validation and comparison with a conditional merging technique at an event-scale. We also assess its performance against rainfall fields from ground-based data at catchment-scale. We further evaluate the performance of the hydrological system in terms of streamflow against observed data (relative error on high flows less than 25% and Nash–Sutcliffe Efficiency greater than 0.5 for 72% and 46% of the calibrated study sections, respectively). These results, therefore, confirm the suitability of such an approach, even at national scale, over a wide range of catchment types, climates, and hydrometeorological regimes, and for operational purposes.

Highlights

  • Zanchetta and Coulibaly in [8] suggest the use of flow-based flash flood early warning systems relying on (i) radar rainfall estimates and (ii) distributed and mixed conceptually–physically based hydrological models, such as Continuum [9], in large domains covered by a radar network

  • In this work we developed a new method that uses as starting point the CM, called modified conditional merging (MCM)

  • This work analyzes the performance of a national-scale hydrological monitoring system by a multi-sensor based rainfall

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Radar data and hydrological models are useful tools to monitor, in real-time intense rainfall and the flash-flood events they frequently generate These tools are widely used by institutions in charge of forecasting and monitoring natural disasters around the world. Zanchetta and Coulibaly in [8] suggest the use of flow-based flash flood early warning systems relying on (i) radar rainfall estimates and (ii) distributed and mixed conceptually–physically based hydrological models, such as Continuum [9], in large domains covered by a radar network. We describe and evaluate a system that monitors hydrological occurrences in terms of streamflow at the Italian scale, by exploiting rain-gauge and radar data as input for the hydrological model, Continuum [9]. This work contributes to showing the suitability of this approach even at a national scale, over different catchment types, climates, and hydrometeorological regimes, and for operational purposes

Study Area and Period
Characteristics of radars data composing thehourly
Description of the Method
Analysis of Rainfall
Operational Hydrological Model at National Scale
Ensemble
Performances of Hydrological
Findings
Conclusions
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