The urban heat island effect refers to the phenomenon where urban areas experience higher temperatures than their rural surroundings due to human activities, land-use changes, and alterations in the natural energy balance. The main causes of this effect can be understood through both physical and anthropogenic mechanisms. One of the primary causes is the replacement of natural vegetation with impervious surfaces such as concrete, asphalt, and buildings. These surfaces have high heat storage capacity and low albedo, meaning they absorb large amounts of solar radiation during the day and release it slowly at night, resulting in higher ambient temperatures. Urban geometry also plays a critical role; tall buildings and narrow streets create what is called the “canyon effect,” trapping heat and limiting air circulation, which further intensifies warming. Additionally, human activities like vehicular traffic, industrial operations, and air conditioning contribute anthropogenic heat to the urban atmosphere. The reduction of vegetation not only removes natural cooling through evapotranspiration but also reduces shading, which would otherwise limit surface heating. Air pollution, through the presence of greenhouse gases and aerosols, can trap outgoing longwave radiation, thereby exacerbating local warming. Together, these mechanisms create a localized thermal anomaly, especially pronounced during nighttime, when rural areas cool more rapidly than cities. The impacts of the urban heat island effect are