Abstract
We study the full distribution of , , where is an Ornstein-Uhlenbeck process. We find that for the long-time () scaling form of the distribution is of the anomalous form where is the difference between and its mean value, and the anomalous exponents are , and . The rate function , that we calculate exactly, exhibits a first-order dynamical phase transition which separates between a homogeneous phase that describes the Gaussian distribution of typical fluctuations, and a "condensed" phase that describes the tails of the distribution. We also calculate the most likely realizations of and the distribution of at an intermediate time conditioned on a given value of . Extensions and implications to other continuous-time systems are discussed.
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