Preprints
https://doi.org/10.5194/egusphere-2024-4099
https://doi.org/10.5194/egusphere-2024-4099
15 Jan 2025
 | 15 Jan 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Long-term forest-line dynamics in the French Pyrenees: an accelerating upward shift related to forest context, global warming and pastoral abandonment

Noémie Delpouve, Laurent Bergès, Jean-Luc Dupouey, Sandrine Chauchard, Nathalie Leroy, Erwin Thirion, and Cyrille Barthélémy Karl Rathgeber

Abstract. Worldwide, the upper forest line has climbed over the past decades, shaping mountain landscapes in response to global changes. In European mountains, this recent trend is a continuation of the forest transition initiated in the mid-19th century, when forest extent was minimal. This study aimed to reconstruct the forest-line dynamics for the entire French Pyrenees from the mid-19th century until today. To ascertain the forest-line elevational shift for the 114 municipalities studied, three digital land-use maps (dated 1851, 1993 and 2010) were employed. The forest-line shift velocity was calculated for two periods delineated by these maps. We applied linear mixed-effect models to investigate the influence of human and environmental drivers on the forest-line shift. The mean upward shift was 0.9 m.yr-1 during the 1851–1993 period but was four-fold higher during the 1993–2010 period (3.5 m.yr-1). During the first period, the forest-line shift coincided with the isotherm upward shift, resulting from global warming. However, during the second period, despite an acceleration, the forest line lagged behind the isotherm upward shift, deepening its climatic debt. Furthermore, during the first period, the forest line shifted upward seven times faster in the eastern Pyrenees, where the mountain pine, a pioneer species, formed the forest line and pastoral abandonment occurred earlier, than in the western Pyrenees (1.3 vs. 0.2 m.yr-1). Conversely, in the following period, the shift occurred three times as fast in the western Pyrenees, where abandonment became widespread, as in the eastern Pyrenees (5.6 vs. 2.1 m.yr-1). In addition, during the second period, the closed forest line climbed twice as fast as the forest line (5.6 m.yr-1), indicating a pronounced densification of the subalpine forest. Our innovative approach integrates a large spatial scale and temporal depth and sheds new light on the interrelationships between global warming, pastoral abandonment and the forest-line upward shift.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Noémie Delpouve, Laurent Bergès, Jean-Luc Dupouey, Sandrine Chauchard, Nathalie Leroy, Erwin Thirion, and Cyrille Barthélémy Karl Rathgeber

Status: open (until 26 Feb 2025)

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Noémie Delpouve, Laurent Bergès, Jean-Luc Dupouey, Sandrine Chauchard, Nathalie Leroy, Erwin Thirion, and Cyrille Barthélémy Karl Rathgeber
Noémie Delpouve, Laurent Bergès, Jean-Luc Dupouey, Sandrine Chauchard, Nathalie Leroy, Erwin Thirion, and Cyrille Barthélémy Karl Rathgeber

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Short summary
Worldwide, the upper forest line has climbed over the past decades, shaping mountain landscapes in response to global changes. Thanks to historical land-use maps, we documented the forest-line rise across the entire French Pyrenees and over a long time span. The forest line has moved upward since the 1850s, driven by the regional abandonment of grazing and the presence of the mountain pine. However, despite a recent acceleration, the forest line has been unable to keep pace with global warming.