Ramón Jardí i Borrás falling. If the rain is heavy enough, it can exceed the device's capacity. At that level, the regulating hole is uncovered, discarding the excess water. If the rain decreases, the buoy drops at the same speed -as the cylindrical reservoir empties. The pluviometer recorded precipitation in Barcelona for 95 years and in places such as Hong-Kong). To measure the average intensity of rainfall in a certain interval of time, the Pluviometer of intensities uses the formula: Intensity varies over time. The pluviometer records instantaneous rain intensity (as its name defines): Ramón Jardí i Borrás Ramon Jardí i Borras (Tivissa, November
Besov measure from the generalized Gaussian measure on formula_19 with Lebesgue probability density function proportional to formula_20. Informally, formula_12 can be said to have a probability density function proportional to formula_22 with respect to infinite-dimensional Lebesgue measure (which does not make rigorous sense), and is therefore a natural candidate for a “typical” element of formula_10. It can be shown that the series defining formula_12 converges in formula_25 almost surely for any <math>t, and therefore gives a well-defined formula_25-valued random variable. Note that in particular this random variable is almost surely "not" in formula_27. The space formula_27 is rather the Cameron-Martin space of