Abstract

Assessing the impact of climate change on water demand is a challenging task. This paper proposes a novel methodology that quantifies this impact by establishing a link between water demand and weather based on climate change scenarios, via Coupled General Circulation Models. These models simulate the response of the global climate system to increasing greenhouse gas concentrations by reproducing atmospheric and ocean processes. In order to establish the link between water demand and weather, Random Forest models based on weather variables were used. This methodology was applied to a district metered area in Naples (Italy). Results demonstrate that the total district water demand may increase by 9–10% during the weeks with the highest temperatures. Furthermore, results show that the increase in water demand changes depending on the social characteristics of the users. The water demand of employed users with high education may increase by 13–15% when the highest temperatures occur. These increases can seriously affect the capacity and operation of existing water systems.

Highlights

  • 4.1 Prediction Accuracy of Random Forest models (RFs) based on Weather Variables

  • This study investigates the effect of weather variables on water demand in both current and future climate change scenarios

  • A novel methodology to assess the impact of climate change on water demand is presented

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Summary

Introduction

Several studies have used weather variables to explain demand variability (Slavíková et al 2013; Ashoori et al 2016; Haque et al 2017; Toth et al 2018; Manouseli et al 2019; Xenochristou et al 2020; Xenochristou et al 2021). Increases in water demand can cause imbalance in water resources and problems in storage capacity, worsening the situation of water shortages that Mediterranean countries, such as Italy, are already experiencing (La Jeunesse et al 2016). Knowing the extent of water demand changes due to climate change is needed for long-term climate adaptation planning (Wang et al 2014; Parandvash and Chang 2016)

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