“…These models use the daily air temperature range to estimate atmospheric transmissivity: on the one hand, cloud cover decreases daily maximum temperature because of the smaller input of short wave radiation; on the other hand, cloud cover increases the minimum air temperature during night time because of the greater emissivity of clouds compared to a clear sky. Examples of this approach are the works of Brinsfield et al (1984), Bristow and Campbell (1984), Hargreaves et al (1985), Donatelli and Marletto (1994), Donatelli and Campbell (1998). Other methods also use rainfall measurements (Hodges et al, 1985;Reddy, 1987;McCaskill, 1990;Bindi and Miglietta, 1991;Hook and McClendon, 1992;Nikolov and Zeller, 1992;Elizondo et al, 1994).…”