New Evidence of Climate Warming Found in European Alpine Caves

New research shows rising temperatures in Alpine caves, threatening subterranean ecosystems, ice deposits, and geological stability.

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Between 2000 and 2020, researchers documented temperature increases in four Alpine caves, showing a rise of approximately 0.2 °C per decade. This rate is half that of the surface temperatures observed across Europe. This subtle yet consistent warming in Alpine caves lags behind surface warming, signaling that atmospheric temperature changes are reaching deep into the earth’s interior. Such subsurface warming shows remarkable spatial consistency, affirming a direct link to broader climate changes affecting the Alps.

Environmental and Ecological Impacts

Mean annual cave temperatures (dots) compared to calculated temperatures outside of the caves (thick solid lines) and HISTALP data for selected Greater Alpine Regions (thin lines).
Mean annual cave temperatures (dots) compared to calculated temperatures outside of the caves (thick solid lines) and HISTALP data for selected …

The warming trend affects more than just temperature. Caves like Spannagelhöhle and Schrattenhöhle exhibit shifting airflows and altered hydrology, which disrupts delicate subterranean ecosystems. Stalactites, stalagmites, and even karst hydrology—key elements of cave environments—are vulnerable to these changes. In particular, the warming trend threatens to melt perennial ice deposits in some caves, paralleling the retreat of surface glaciers and the melting of permafrost observed throughout the Alps. This loss could occur within the next decade, eliminating a vital reservoir supporting downstream ecosystems during dry periods.

Changes in Cave Microclimates and Ventilation

The research highlights that caves with restricted ventilation retain colder temperatures, creating “cold traps” that preserve ice longer. In contrast, well-ventilated caves like Schrattenhöhle display greater temperature fluctuations, especially near entrances. This “chimney effect,” driven by seasonal airflows, accelerates warming and affects the stability of ice near cave openings.

Regional Climate and Broader Implications

The Alps are warming twice as fast as the global average. Alpine streams, lakes, and groundwater have shown similar warming trends, with outside temperatures near caves rising at approximately 0.5 °C per decade. As cave temperatures continue to rise, increased cave ventilation, ice melt, and potential habitat loss could further impact regional hydrology and biodiversity.

Mean air temperature observed at site HA-29 during consecutive stake measurements (red line) and concurrent surface height changes of ice located at the same location in HA (blue line).
Mean air temperature observed at site HA-29 during consecutive stake measurements (red line) and concurrent surface height changes of ice located at …

Future Implications: Monitoring and Mitigation

The study underscores the need for continuous monitoring of Alpine caves. As natural climate archives, caves offer valuable data to help track climate change impacts and inform broader environmental strategies. Comprehensive research on subterranean ecosystems, climate modeling, and data collection will be essential for understanding and mitigating the impact of warming trends on these unique environments.

Environment + Energy Leader