Response of Pinios hydrologic observatory (Agia basin-Thessaly, Greece) to storm Daniel

Extreme weather events are becoming increasingly frequent and intense due to climate change, posing significant challenges to water resource management in vulnerable agricultural regions. Understanding how aquifer systems respond to such events is critical for ensuring long-term groundwater sustainability. Continuous, high-resolution monitoring is essential to capture the dynamics of recharge processes, particularly during intense storms. This study presents novel observations from the Pinios Hydrological Observatory (PHO), located in the Pinios River Basin in Thessaly, Greece one of the country’s most important agricultural areas, heavily dependent on groundwater for irrigation. The PHO, part of the Greek Long-Term Ecological Research Network, is equipped with automated sensors that provided rare, event-scale data during Storm Daniel, a major hydrometeorological event that impacted the region in September 2023. The sensors recorded the passage of the flood wave in near-real time, enabling a detailed analysis of groundwater recharge dynamics. Hourly groundwater level data from fourteen monitoring wells were analyzed in conjunction with meteorological data using advanced time-series techniques, including Dynamic Time Warping (DTW), to detect temporal shifts in aquifer response. Lag times between rainfall and groundwater rise ranged from 3 to 10 days, depending on local hydrogeological conditions. Piezometric surface maps generated through Inverse Distance Weighting (IDW) interpolation highlighted widespread recharge across alluvial deposits, with groundwater levels increasing from approximately 70 to 72.2 meters above sea level in some areas. These results underscore the value of real-time monitoring networks in capturing aquifer responses to extreme events, contributing to more informed and adaptive water management strategies. • In September 2023, Storm Daniel brought catastrophic rainfall over 72 hours. • High-resolution sensors reveal aquifer recharge dynamics during storms. • DTW revealed how geology influences groundwater response times. • Understanding aquifer behavior during extreme rainfall is key for effective water management and disaster preparedness

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Publication Details

Journal
Groundwater for Sustainable Development
Published
2025-10-09
DOI
https://doi.org/10.1016/j.gsd.2025.101528
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
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article

Response of Pinios hydrologic observatory (Agia basin-Thessaly, Greece) to storm Daniel

Gaetano Daniele Fiorese, Maria Rosaria Alfio, Anna Chatzi, Vassilios Pisinaras et al.
Groundwater for Sustainable Development
Groundwater and Isotope Geochemistry
article

Response of Pinios hydrologic observatory (Agia basin-Thessaly, Greece) to storm Daniel

Gaetano Daniele Fiorese, Maria Rosaria Alfio, Anna Chatzi, Vassilios Pisinaras, Konstantinos Babakos, Gabriella Balacco, Andreas Panagopoulos, Ayesha Nawaz
article en

Abstract

Extreme weather events are becoming increasingly frequent and intense due to climate change, posing significant challenges to water resource management in vulnerable agricultural regions. Understanding how aquifer systems respond to such events is critical for ensuring long-term groundwater sustainability. Continuous, high-resolution monitoring is essential to capture the dynamics of recharge processes, particularly during intense storms. This study presents novel observations from the Pinios Hydrological Observatory (PHO), located in the Pinios River Basin in Thessaly, Greece one of the country’s most important agricultural areas, heavily dependent on groundwater for irrigation. The PHO, part of the Greek Long-Term Ecological Research Network, is equipped with automated sensors that provided rare, event-scale data during Storm Daniel, a major hydrometeorological event that impacted the region in September 2023. The sensors recorded the passage of the flood wave in near-real time, enabling a detailed analysis of groundwater recharge dynamics. Hourly groundwater level data from fourteen monitoring wells were analyzed in conjunction with meteorological data using advanced time-series techniques, including Dynamic Time Warping (DTW), to detect temporal shifts in aquifer response. Lag times between rainfall and groundwater rise ranged from 3 to 10 days, depending on local hydrogeological conditions. Piezometric surface maps generated through Inverse Distance Weighting (IDW) interpolation highlighted widespread recharge across alluvial deposits, with groundwater levels increasing from approximately 70 to 72.2 meters above sea level in some areas. These results underscore the value of real-time monitoring networks in capturing aquifer responses to extreme events, contributing to more informed and adaptive water management strategies. • In September 2023, Storm Daniel brought catastrophic rainfall over 72 hours. • High-resolution sensors reveal aquifer recharge dynamics during storms. • DTW revealed how geology influences groundwater response times. • Understanding aquifer behavior during extreme rainfall is key for effective water management and disaster preparedness

Groundwater for Sustainable DevelopmentVol. 31
Hellenic Centre for Marine Research (GR), University of Bari Aldo Moro (IT), Polytechnic University of Bari (IT)
Openalex Percentile: Top 77%
Groundwater and Isotope Geochemistry
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