Occurrence of rainfall‐induced landslides is increasing worldwide, owing to land use and
climate changes. Although the connection between hydrology and rainfall‐induced …

Debris flows have been always a serious problem in the mountain areas. Research on the
assessment of debris flows susceptibility (DFS) is useful for preventing and mitigating debris …

Hydrological regimes of alpine catchments are expected to be strongly affected by climate
change, mostly due to their dependence on snow and ice dynamics. While seasonal …

In recent years, losses due to torrential flooding have been increasing in the Eastern
European Alps, with effects of climate change and settlement growth being postulated root …

In the Dolomites, steep rocky cliffs are marked by numerous narrow gullies. When high‐
intensity short‐duration precipitation occurs, these gullies concentrate and direct surface …

Satellite and hydrological model-based technologies provide estimates of rainfall and soil
moisture over larger spatial scales and now cover multiple decades, sufficient to explore …

The transboundary Helmand River basin (HRB) is the main drainage system for large parts
of Afghanistan and the Sistan region of Iran. Due to the reliance of this arid region on water …

The initiation of geomorphic hazards in mountainous environments is highly susceptible to
temperature and precipitation forcing. To assess future changes in these hazards, statistical …

Debris-flow activity is strongly controlled by hydro-meteorological trigger conditions, which
are expected to change in a future climate. In this study we connect a regional hydro …

Regional empirical-statistical thresholds indicating the precipitation conditions initiating
landslides are of crucial importance for landslide early warning system development. The …