Precipitation variability is a key concern in many respects for society. In Alpine valleys, precipitation variability governs both liquid and solid water resources that are essential for touristic activities, hydroelectricity production, and agriculture. Understanding the mechanisms governing precipitation variability is, therefore, an important issue, especially in a climate change context. In Europe, precipitation variability is often linked to different modes of large-scale circulation variability, in particular to the North Atlantic Oscillation (NAO) which is the first mode of variability over the North Atlantic and the only one that can be defined throughout the entire year (Barnston & Livezey, 1987). In winter, positive NAO phases are associated with increasing westerlies in a southwest-to-northeast direction, explaining positive precipitation anomalies over Northern Europe and negative precipitation anomalies over Southern Europe (Hurrell, 1995). The influence of NAO on precipitation variability in the Alpine region is however far less obvious (