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41 of the assumed normal 50 Solar Radiation cloudless weather amount. In spring the relative availability of direct irradiance has been to some extent larger than in summer and its interannual variation smaller. Slopes of the linear trends were found to be smallest in the case of using conventional mean as a central tendency measure. It leads to underestimation of the dimming and brightening trends in the cases when linear approximation is appropriate for their description. In summer months, in most cases, small brightening trends were found.

E. relative humidity or wind speed). In this sense we measured R, Ta, To, Ts, and Eobs, in order to model E from R, ΔTa = To – Ta, and ΔTs = To – Ts. Namely Emod = a1 R + a2 ΔTa + a3 ΔTs; where Emod is the model E, and the coefficients a1, a2, and a3 are determined through multiple regression. Therefore the model provides also a preliminary assessment of the relative importance of energy fluxes. That is, making E = Eobs, Rn = a1 R, H = a2 ΔTa, and G = a3 ΔTs, we get a1 R = Eobs - a2 ΔTa - a3 ΔTs.

2006. Proxy-based reconstruction of erythemal UV doses over Estonia for 1955-2004. Ann. , Ansko I. 2010. Interannual variations of available solar radiation on seasonal level in 1955-2006 at Tartu Tõravere Meteorological station. Theor. Appl. , Jaagus J. 1996. The impact of climate change on hydrological regime and water resources in Estonia. In: Punning J-M (ed) Estonia in the system of global climate change. , Ohvril H. 2005. 100 Years of Solar Radiation Measurements in Estonia. In:World Climate Research Programme.

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