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Interannual variability of winter precipitation in the European Alps: relations with the North Atlantic Oscillation

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Figure

Table 1. Stations used for the comparison with the gridded dataset
Fig. 2. (a) Time series of the winter total precipitation anomaly (December–March) averaged over the alpine domain; (b) Time series of theclimate indeces used in the study
Fig. 3.Coefficient of variation of the winter precipitation(December–March).
Fig. 6. (a) Map of Spearman rank correlation coefficients betweenSPI3F and East Atlantic West Russia Index; (b) red areas representregions where the correlation is significant.
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