Abstract. Several studies have shown that global changes have important impacts in
mountainous areas, since they affect natural hazards induced by
hydrometeorological events such as landslides. The present study evaluates,
through an innovative method, the influence of both vegetation cover and
climate change on landslide hazards in a Pyrenean valley from the present to
2100. We first focused on assessing future land use and land cover changes through
the construction of four prospective socioeconomic scenarios and their
projection to 2040 and 2100. Secondly, climate change parameters were used
to extract the water saturation of the uppermost layers, according to two
greenhouse gas emission scenarios. The impacts of land cover and climate
change based on these scenarios were then used to modulate the
hydromechanical model to compute the factor of safety (FoS) and the hazard
levels over the considered area. The results demonstrate the influence of land cover on slope stability
through the presence and type of forest. The resulting changes are
statistically significant but small and dependent on future land cover
linked to the socioeconomic scenarios. In particular, a reduction in human
activity results in an increase in slope stability; in contrast, an increase
in anthropic activity leads to an opposite evolution in the region, with
some reduction in slope stability. Climate change may also have a significant impact in some areas because of
the increase in the soil water content; the results indicate a reduction in
the FoS in a large part of the study area, depending on the landslide type
considered. Therefore, even if future forest growth leads to slope
stabilization, the evolution of the groundwater conditions will lead to
destabilization. The increasing rate of areas prone to landslides is higher
for the shallow landslide type than for the deep landslide type.
Interestingly, the evolution of extreme events is related to the frequency
of the highest water filling ratio. The results indicate that the
occurrences of landslide hazards in the near future (2021–2050 period,
scenario RCP8.5) and far future (2071–2100 period, scenario RCP8.5) are
expected to increase by factors of 1.5 and 4, respectively.