The urban climate change conundrum

One of the fundamental cornerstones of progress of a country is urbanization. The term "urbanization" is closely linked to the term "development". Bangladesh has a high urbanization rate (Ahmed and Ahmed, 2017), and it is visible that the country is rapidly developing. The transition from an under-developed to a developing country was not easy. However, these advancements came at a price. Change in temperature is one of the outcomes of that price. The climate of Bangladesh was not the same half a century ago. In recent years, there have been considerable temperature fluctuations. During the last few years, Bangladesh's weather has been rapidly altering, reaching a critical point. Between the years of 1976 to now, Bangladesh has had an average temperature increase of 0.5°C. The rise in maximum temperature has not been consistent throughout the country. For example, maximum temperatures in the eastern portions (Chattogram and Sylhet divisions) of Bangladesh rose by 0.9°C, compared to a 0.5°C rise in the central parts spanning Dhaka and nearby districts. As a result summers are elongated, winters are warmer, and the monsoon is becoming increasingly unpredictable. Rapid urbanization creates a significant impact on urban land use and land cover , increasing the land surface temperature. Land use and land cover fluctuations are intimately linked to variations in land surface temperature and the intensity of Urban Heat Islands (UHI). The UHI phenomenon is caused by the fact that urban regions have greater air and surface temperatures than rural and suburban locations. The UHI effect arises as buildings, roads, and infrastructure absorb heat, causing temperatures in urban areas to be 1 to 7 degrees Fahrenheit hotter than in outlying areas. Although the impact is greater during the day, the slow release of heat from infrastructure overnight can keep cities substantially hotter than surrounding locations. 

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