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In this study a new model for quantifying the effect of evaporative cooling produced by the evapotranspiration from trees on the air temperature of AliAl Sharqi town, south of Iraq, (lat. 32.1N, long 46.85E) was suggested. The ASCE and FAO Penman Monteith model was used to calculate the actual evapotranspiration from a tree in the selected town. The dispersion of moisture from trees in the neighborhood in the three dimensions by using the Gaussian dispersion model was estimated. The decreasing of air temperature due to the moisture added by trees on a specific control volume was calculated by using the psychometric chart. The maximum cooling degree achieved by the suggested model reached to 2.6 C in July while minimum value was (1.8 C) and appeared in April. The results of applying the model on a hot and dry day indicated that the higher cooling degree can be obtained reach to 3.6 C at the noon time.

A Model for Modification of Air in a Small Town by Using the Evaporative Cooling Method.