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Coupled decadal variability of the North Atlantic Oscillation, regional rainfall and karst spring discharges in the Campania region (southern Italy)

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Figure

Fig. 1. Hydrogeological map of the Campania region. Hydrostratigraphic units and key to symbols: (1) alluvial and epiclastic units (Quater-nary); (2) volcanic units (Pliocene-Quaternary); (3) late orogenic molasses and terrigenous units (Upper Miocene-Pliocene); (4) pre-orogenicand syn-orogenic terrigenous units of inner and thrust-top basins series (Cretaceous-Upper Miocene); (5) siliceous-marly units of outer basinseries (Trias-Paleogene); (6) limestone and dolomitic limestone units of carbonate platform series (Jurassic-Paleogene); (7) dolomitic units ofcarbonate platform series (Trias-Jurassic); (8) main basal springs of carbonate karst aquifers; (9) groundwater head contour lines in alluvialand volcanic aquifers; (10) main preferential drainage axes of groundwater flow in alluvial aquifers; (11) identification of the carbonate karstaquifers analysed: (a) Matese Mount; (b) Terminio Mount; (c) Cervialto Mount; (12) regional boundary; (13) rain gauge stations; (14) airtemperature monitoring stations.
Fig. 2. Time series of (a) winter NAOI time series monitored between Lisbon (Portugal) and Stykkisholmur/Reykjavik (Iceland)
Fig. 4. Cross-correlation analysis between the winter NAOI and theMAPI carried out on (a) the original time series and (b) the 11-yrmoving average time series.
Fig. 7. Comparison between the 11-yr moving averages of the NAOItime series and the MADImax, MADI and MADImin time series ofthe Sanit`a spring.
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