Thermal Regime Characteristics of Alpine Springs in the Marginal Periglacial Environment of the Southern Carpathians

Oana Berzescu, Florina Ardelean, Petru Urdea, Andrei Ioniță and Alexandru Onaca ()
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Oana Berzescu: Institute for Advanced Environmental Research (ICAM), West University of Timisoara, 300223 Timisoara, Romania
Florina Ardelean: Department of Geography, West University of Timisoara, 300223 Timisoara, Romania
Petru Urdea: Institute for Advanced Environmental Research (ICAM), West University of Timisoara, 300223 Timisoara, Romania
Andrei Ioniță: Institute for Advanced Environmental Research (ICAM), West University of Timisoara, 300223 Timisoara, Romania
Alexandru Onaca: Institute for Advanced Environmental Research (ICAM), West University of Timisoara, 300223 Timisoara, Romania

Sustainability, 2025, vol. 17, issue 9, 1-15

Abstract: Mountain watersheds play a crucial role in sustaining freshwater resources, yet they are highly vulnerable to climate change. In this study, we investigated the summer water temperature of 35 alpine springs in the highest part of the Retezat Mountains, Southern Carpathians, between 2020 and 2023. During the four-year monitoring period, water temperatures across all springs ranged from 1.2 °C to 10.5 °C. Springs emerging from rock glaciers had the lowest average temperature (2.37 °C), while those on cirque and valley floors were the warmest (6.20 °C), followed closely by springs from meadow-covered slopes (6.20 °C) and those from scree and talus slopes (4.70 °C). However, only four springs recorded summer temperatures below 2 °C, suggesting a direct interaction with ground ice. The majority of springs exhibited temperatures between 2 and 4 °C, exceeding conventional thresholds for permafrost presence. This challenges the applicability of traditional thermal indicators in marginal periglacial environments, where reduced ground ice content within rock glaciers and talus slopes can lead to spring water temperatures ranging from 2 °C to 4 °C during summer. Additionally, cold springs emerging from rock glaciers displayed minimal daily and seasonal temperature fluctuations, highlighting their thermal stability and decoupling from atmospheric conditions. These findings underscore the critical role of rock glaciers in maintaining alpine spring temperatures and acting as refugia for cold-adapted organisms. As climate change accelerates permafrost degradation, these ecosystems face increasing threats, with potential consequences for biodiversity and hydrological stability. This study emphasizes the need for long-term monitoring and expanded investigations into water chemistry and discharge dynamics to improve our understanding of high-altitude hydrological systems. Furthermore, it provides valuable insights for the sustainable management of water resources in Retezat National Park, advocating for conservation strategies to mitigate the impacts of climate change on mountain hydrology and biodiversity.

Keywords: permafrost; spring water temperature; rock glaciers; periglacial environments; Southern Carpathians (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2025
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