Titlebook: European Solar Radiation Atlas; Solar Radiation on H Wolfgang Palz,Jürgen Greif,Commission of the Europ Book 1996Latest edition Springer-Ve

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Wolfgang Palz,Jürgen Greif,Commission of the Europ

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Introduction,mation in the original Atlas (1) (2) into a single volume. However opportunity has been taken to improve presentation and to print additional useful estimated data that was implicitly used in the development of the earlier edition, but not printed in the tables, for example the estimated diffuse rad

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Areas with missing data, Instead, the coefficients a. and b. for each heliographic station in Spain were determined by the method of Dogniaux and Lemoine (29) who proposed a linear dependence of a. and b. on geographical latitude ϕ, corrected by a site-specific index for the atmospheric transparency. Similar procedures wer

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Geographical analysis of the different radiation climates of Europe,ation has a strong influence on the definition of the different climatic zones of Europe. The variations from month to month are caused mainly by changes in the general circulation of the atmosphere over Europe and the adjacent part of the Atlantic Ocean. Different cloudiness and turbidity character

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Introductory comments on global and diffuse radiation on vertical and inclined surfaces,opean Solar Radiation Atlas (2), but the changes that have been made are relatively few, as only sites with actual radiation observations were used in preparing the original slope irradiation tables. The values of Gmax and G mean used are therefore observed values, which have not been subjected to r

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Introduction to the tables for daily global and diffuse radiation incident on slopes,arked with an asterisk if a slope table has been computed. Each inclined surface table header contains, in addition to the site name, the country name and the site reference number needed to locate the site on the site reference map. The computer file name for the clear sky slope data file then foll

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