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The climate in urban areas differs from that in neighboring rural areas, as a result of urban development. Urbanization greatly changes the form of the landscape, and also produces changes in an area's air. The study of urban climate is urban climatology. In 1950 Åke Sundborg published one of the first theories on the climate of cities. [1] [2]
Keeping these quotations in mind, bounce-back discourse has been and should continue to be an important part of urban climate resiliency framework. [44] Other theorists have critiqued this idea of bounce-back, citing this as privileging the status quo, rather advocating the notion of 'bouncing forward', permitting system evolution and improvement.
Urban climatology is the study of urban climate. It is a branch of climatology that concerns interactions between urban areas and the atmosphere , the effects they have on one another, and the varying spatial and temporal scales at which these processes (and responses) occur.
Housing conditions are a factor that contributes to urban heat inequity. Living on the top-floor, having a home with a dark roof, and poor insulation exacerbate heating conditions during hot weather. [10] Lower income individuals may also not have access to air-conditioning or be unable to afford the increased electricity usage. [10]
A definition of urban heat island is: "The relative warmth of a city compared with surrounding rural areas." [14]: 2926 This relative warmth is caused by "heat trapping due to land use, the configuration and design of the built environment, including street layout and building size, the heat-absorbing properties of urban building materials, reduced ventilation, reduced greenery and water ...
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The climate of New York City shapes the environment with its cool, wet winters and hot, humid summers with plentiful rainfall all year round. As of 2020, New York City held 44,509 acres of urban tree canopy with 24% of its land covered in trees. [1] [2] As of 2020, the population of New York City numbered 8.8 million human beings. [3]
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