By E. Babatunde

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2005). 3. Composing of annual cloudless-sky cycles The interpolated annual cycles of clear-sky daily Gclear and I’clear for the study site (Eerme et al, 2006) are presented in Fig. 1. 35 Clear global Daily sum (MJ·m -2 ) 30 Clear direct 25 20 15 10 5 0 0 50 100 150 200 250 300 350 Day in year Fig. 1. Graph of the daily global and direct broad-band radiation in MJ·m-2 on cloudless day vs day in the year for Tartu-Tõravere Meteorological Station site Selection of cloudless days was based on the daily sums of direct irradiance and sunshine duration with inclusion of the hourly values, if necessary, and on the cloud visual inspection data.

Journal of Hydrology Vol. 319, pp. 83-95. Pavia, E. G. (2008) Evaporation from a thin layer of wet sand. Geophysical Research Letters Vol. 1029/2008GL033465. Pavia, E. G. & Velázquez, I. (2010) Does wet sand evaporate more than water in the Guadalupe Valley? In The Ocean, The Wine, and The Valley: The Lives of Antoine Badan, Pavia, E. ; Sheinbaum, J. & Candela, J. (eds), CICESE, Ensenada, Mexico, ISBN 978-0-557-94026-4, pp. 331. Penman, H. L. (1948) Natural evaporation from open water, bare soil and grass.

Typical histogram of monthly distribution in bright half-year is shown in Fig 10. In Table 3, the monthly average together with maximum and minimum values of the ratio Mean/Trimean are presented as well as the coefficients of linear correlation of this ratio with the kurtosis and skewness of distribution. Variations in spread characteristics have been largest in StDevMed, but only moderately larger than those in two other spread characteristics. For all the months except November, the StDevTri in most cases happened to be the smallest.

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