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We analyze distributions of rain-event sizes, rain-event durations, anddry-spell durations for data obtained from a network of 20 rain gaugesscattered in a region of the NW Mediterranean coast. While power-lawdistributions model the dry-spell durations with a common exponent 1.50 +-0.05, density analysis is inconclusive for event sizes and event durations, dueto finite size effects. However, we present alternative evidence of theexistence of scale invariance in these distributions by means of different datacollapses of the distributions. These results are in agreement with theexpectations from the Self-Organized Criticality paradigm, and demonstrate thatscaling properties of rain events and dry spells can also be observed formedium resolution rain data.

Scale Invariant Events and Dry Spells for Medium Resolution Local Rain Data