Quantifying rates of climate change in mountain regions is of considerable interest, not least
because mountains are viewed as climate “hotspots” where change can anticipate or …

Abstract Purpose of Review Highlight significant developments that have recently been
made to enhance our understanding of how snow responds to climate forcing and the role …

The cryosphere (including, snow, glaciers, permafrost, lake and river ice) is an integral
element of high mountain regions, which are home to roughly 10% of the global population …

In Alpine regions, future changes in glacier and snow cover are expected to change runoff
regimes towards higher winter but lower summer discharge. The low summer discharge will …

As droughts propagate both in time and space, their impacts increase because of changes
in drought properties. Because temporal and spatial drought propagation are mostly studied …

Hydrology plays a central role in applied and fundamental environmental sciences, but it is
well known to suffer from an overwhelming diversity of models, particularly to simulate …

We project climate change induced changes in fluvial flood risks for six global warming
levels between 1.5 and 4° C by 2100, focusing on the major river basins of six countries …

Streamflow regimes are changing and expected to further change under the influence of
climate change, with potential impacts on flow variability and the seasonality of extremes …

Streamflow droughts are governed by different hydro‐meteorological processes, whose
relative importance may change over time, with potential impacts on drought severity. Here …

Alpine catchments show a high sensitivity to climate variation as they include the elevation
range of the snow line. Therefore, the correct representation of climate variables and their …