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Enhanced spring warming in a Mediterranean mountain by atmospheric circulation
E Bruley1,2, F Mouillot3, T Lauvaux4
1Centre d'Ecologie Fonctionnelle et Evolutive CEFE, UMR5175, CNRS, Université de Montpellier, Université Paul-Valéry Montpellier, EPHE, 1919 Route de Mende, 34293, Montpellier Cedex 5, France.
Forest expansion in Cévennes National Park cools maximum air temperatures, slowing warming trends. This climate change impact is influenced by land cover changes and regional weather patterns.
Area of Science:
- Environmental Science
- Climate Science
- Ecology
Background:
- Cévennes National Park, Southern France, is a mid-altitude coastal mountain region.
- The area experiences Mediterranean Sea influences and is impacted by climate change.
- Significant land cover changes are occurring, with forests expanding at the expense of rangelands.
Purpose of the Study:
- To analyze air temperature trends in Cévennes National Park.
- To investigate the impact of forest expansion on local climate.
- To understand the relationship between climate change, land cover, and temperature variations.
Main Methods:
- Analysis of air temperature data since 1980.
- Monitoring of forest cover changes.
- Application of an intrinsic biophysical mechanism model to assess forest surface temperature compared to grasslands.
- Correlation analysis between temperature trends and weather patterns (e.g., Western Mediterranean Oscillation - WeMO).
Main Results:
- Maximum April-June temperatures increased by up to +0.124 °C/year, uniform across altitudes.
- Minimum temperatures increased by +0.058 °C/year at 500m and +0.089 °C/year at 1500m.
- Forest cover increased by +0.51%/year.
- Forest surfaces were 1.7-3.1 °C cooler than grasslands.
- Forest expansion led to a cooling effect of 0.023 °C/year on maximum air temperatures by decreasing albedo.
- Spring warming trends correlated with negative Western Mediterranean Oscillation phases.
Conclusions:
- Forest expansion in Cévennes National Park has a cooling effect on maximum air temperatures, partially mitigating regional warming.
- Land cover change, specifically afforestation, plays a significant role in modulating local climate responses to broader climate change.
- Atmospheric humidity and radiative forcing, influenced by large-scale weather patterns, are key drivers of temperature rise in the region.
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