Asymmetry in snow-water nexus in mountain areas mainly governed by meteorological seasonal changes.

1 b), while in 16% of the catchments a significant trend in just one of the variables (Fig. 1 c, d) was identified.

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For instance, a positive trend in streamflow is found in catchments driven by glaciers 31 .

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Here, a similar behaviour is found with a decreasing trend in SCA and Qmean, which is also reported in the area by Rajwa-Kuligiewicz & Bojarczuk 37 .

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In Europe, when having a look at the European Alps, the annual median streamflow does not show a clear trend over the whole mountain range, but some significant trends are found when analysing catchments individually.

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The European Alps present a negative trend, especially below 2000 m.

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