Rising temperatures in India’s urban landscape are attributed to the urban heat-island effect, making the metro areas significantly warmer than their surroundings
What is the Urban Heat Island Effect?
The urban heat island effect refers to higher temperatures in urban areas compared to their rural surroundings.
It occurs due to human activities and urban infrastructure that absorb and retain heat more effectively.
Causes and Effects:
Building Materials: Concrete and asphalt in cities absorb heat during the day and release it slowly, keeping temperatures elevated, especially at night.
Lack of Green Spaces: Urban areas have fewer trees and green spaces, reducing natural cooling through shade and exacerbating the heat island effect.
Energy Demands: Metropolitan cities have higher energy demands for transportation, industry, and air conditioning, releasing heat into the air and straining energy sources.
Building Density: Dense urban development limits airflow and creates heat-trapping spaces between structures, leading to higher temperatures.
Air Quality: Urban heat islands have poorer air quality due to trapped pollutants, and warm water from cities can harm nearby streams and ecosystems.
Contribution to Global Warming: Urban heat islands may contribute to overall warming by increasing temperatures locally and potentially beyond.
Energy Demands and Power Outages: High urban temperatures increase energy demands for cooling, straining energy resources and causing power outages during peak periods.
Relationship with Climate Change: Heat islands and climate change are related but not the same. Urban heat islands contribute to local temperature increases, which can exacerbate the effects of climate change.