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Fallow is used to increase soil moisture under rainfed conditions, but its effectiveness is dependent on climate and soil conditions of each region. Simulations were performed to evaluate fallow at 5 locations in east Azarbaijan (Ahar, Maragheh, Minab, Sarab and Tabriz) using 23 years weather data. Results indicated that at the end of seasonal fallow (SF: form September to March) 79-140 mm water is stored, which is 50 to 60 % of precipitation. Soil evaporation was the most important loss thatdoi:10.22067/gsc.v5i2.930 doaj:518a4a433a184b4f92c68fa5d7e5e5e1 fatcat:ucurakr6drezde42a2fmfl66we