Year: 2025
Type: article
Abstract: Over the past four decades, seasonal snow cover has declined rapidly in temperate alpine regions. However, the fine-scale dynamics of snowmelt preceding the ongoing warming period remain largely unknown, limiting our understanding of the long-term influence of past snow cover on alpine ecosystems. Here we rely upon the spatial similarities in melt-out patterns and a temperature-based model of fractional snow cover area, to reconstruct fine-scale snow cover changes over the past 250 years in instrumented catchments of the southwestern Alps. We provide evidence that, until the 1980s, prolonged snow cover in many late-lying snowfields delayed ecosystem development and explain why current vegetation cover, soil organic matter content, and mineral weathering are significantly lower in these areas than in surrounding ecosystems. These findings highlight the long-term legacy of snow cover on alpine landscapes and underscore the need to re-evaluate its effects on ecosystem structure, functioning, and responsiveness to ongoing changes.
Institutions: Centre National de la Recherche Scientifique, Laboratoire d'Écologie Alpine, Université Savoie Mont Blanc, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement, Laboratoire Environnements, Dynamiques et Territoires de Montagne, Institut des Géosciences de l'Environnement, Institut de Recherche pour le Développement, Université Grenoble Alpes, Jardin du Lautaret, Centre d'Études Spatiales de la Biosphère
Language: English
Subfield: Atmospheric Science
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDGs: Climate action, Life on land
Open Access status: gold
Estimated APC paid: $3,490
OpenAlex ID: W4414419320