Abstract. Ultraviolet solar irradiance (290-385 nm) was analyzed in Valencia and
IntroductionUltraviolet solar radiation has a significant influence on the Earth's atmosphere. In the stratosphere the absorption of ultraviolet radiation causes an increase of the air temperature in the upper atmospheric layers and is the origin of the existence and variability of stratospheric ozone. On the surface, UV solar radiation represents a small part of the spectrum, although it is an important part because of its biological and photochemical effects. Thus a clear awareness of its availability and its variation, both temporal and spatial, is of great importance in many research areas: (1) Several studies have been conducted to quantify the attenuation of UV radiation by clouds. Factors such as cloud location, percent cover, cloud optical thickness, liquid water content, and particle distribution make it difficult to develop a quantitative relationship relating cloud properties to the attenuation of UV radiation. Some authors [Zavodska and Reichrt, 1985] classify the daily total and UV radiation measurements using the cloud amount as a parameter. Cloud cover is not a very objective measurement because it may be related to very different sky conditions, depending on the relative Sun-cloud position. In this sense, Estupi•an et al. [1996] showed that for the same cloud cover, reductions of up to 99% or increases of up to 27% of UV radiation may be produced with respect to the same measurement on clear days in terms of whether or 4759