The Effect of Heat Island Phenomenon on the Local Climate Change in Ahwaz Metropolis

Abstract

Vertical and horizontal extension of cities and growing trend of industrial activities in them hasresulted in wide changes on ground physical properties, released energy, air pollution, temperatureand as a result change of local climate in metropolises. Cities are often warmer than theirenvironment. This phenomenon is determined by the difference between cities’ energy and theirenvironment’s energy. Synoptic climatology data of Ahvaz and Dezfool in a 44- year period wassurveyed and studied to specify these changes in Ahvaz metropolis. The results showed that annualaverage minimum temperature of Ahwaz in this period has a total increasing trend of 3.375 °C and(0.077 °C/1yr) yearly, whereas the corresponding parameter was without any changes in Dezfool.Temperature increasing trend in Ahwaz in comparison with Dezfool as indicated by the results whichis resulted by the heat island effect in Ahwaz and the lack of development of Dezfool with time. Thegreatest increase rate of Ahwaz average minimum temperature is 4.14 °C and (0.094 °C/1yr) yearly inAzar monthly in this period and the smallest is 2.07 °C and (0/047 °C/1yr) yearly in Esfand monthly.Usually the extent and extension of the city are known as the most important factors in the severity ofheat island effect, and population growth is among the serious factors which cause the increase of itsseverity and finally result in the change of local climate of metropolis. Population is considered asparameter which is explanatory of city’s size. In this study, a relationship has been developed for theaverage intensity of heat island effect in Ahwaz and the logarithm of population.

Keywords

• hest island
• local climate
• time series
• increasing trend
• population growth