Daily precipitation time series are composed of null entries corresponding to dry days and nonzero entries that describe the rainfall amounts on wet days. Assuming that wet days follow a Bernoulli process with success probability , we show that the presence of dry days induces negative correlations between record-breaking precipitation events. The resulting non-monotonic behavior of the Fano factor of the record counting process is recovered in empirical data. We derive the full probability distribution of the number of records up to time , and show that for large , its large deviation form coincides with that of a Poisson distribution with parameter . We also study in detail the joint limit , , which yields a random record model in continuous time .

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