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Such higher emissions, especially from fossil-fuel power plants, worsen air pollution and add greenhouse gases to the atmosphere. Furthermore, warmer city air can speed up chemical reactions that produce ground-level ozone. These combined impacts raise health risks, which leads directly to the need for practical responses.

These design choices often replace trees and soil with dark asphalt and dense concrete. As a result, less shade and evapotranspiration are available to cool the air, while more sunlight is absorbed by urban surfaces. This stored heat becomes the key driver of temperature differences discussed next.

This stored heat is released slowly after sunset, so nights remain unusually warm in built-up areas. Therefore, people rely more heavily on air conditioning to maintain comfort. That increased electricity demand sets up the next effect: higher emissions from power generation.

Urban planners use the term "urban heat island" to describe cities that stay warmer than nearby rural areas. This difference is not random; it emerges from repeated design choices in buildings, roads, and vegetation. The following explanation traces how those choices create a chain of causes and effects.

Ultimately, the same causal chain suggests clear solutions: expand tree cover, use reflective roofs, and design cooler streetscapes. In conclusion, reducing heat absorption lowers night-time temperatures, which cuts energy use and limits pollution. This sequence shows how urban form can either amplify or reduce environmental harm.