The Urban Livablility Index (ULI) is a spatial model that measures the impact of the urban heat island effect on New York City from an engineering and socioeconomic perspective. The ULI is a function of the intensity of the urban heat island effect, peak electricity load connected to the ...
Another study of densely built-up Manhattan in New York City revealed that during the winter, the quantity of heat produced by combustion alone was 2 times greater than the amount of solar energy reaching the ground. In summer, the figure dropped to 1/6....
For example, the blanket of pollutants over a city contributes to the heat island by absorbing a portion of the upward-directed long-wave radiation emitted at the surface and re-emitting some of it back to the ground.例如,城市上空的污染物覆盖层通过吸收在地面发射的一部分向上的长波辐射,并将...
¶A mesoscale analysis of the Urban Heat Island (UHI) of New York City (NYC) is performed using a mesoscale network of weather stations. In all seasons the UHI switches on rapidly in late afternoon and shuts down even more rapidly shortly after dawn. It averages about 4 °C in summe...
showed that the annual heat production in those cities was equal to approximately one-third of that received from solar radiation.Another study of densely built-up Manhattan in New York City revealed that during the winter, the quantity of heat produced by combustion alone was 2 ½ times great...
Lundi said on average cities can be up to 22° F hotter than surrounding natural areas. Furthermore, apartments and homes without air conditioners can be 20° F warmer than the outside. This is why each year in New York City, more than 1,100 people are hospitalized for hea...
showed that the annual heat production in those cities was equal to approximately one-third of that received from solar radiation. Another study of densely built-up Manhattan in New York City revealed that during the winter, the quantity of heat produced by combustion alone was 2 times greater ...
A high frequency of weak elevated inversion layers at an average height of 310 m was observed over the city.The average intensity of the urban heat island, i.e., urban temperature excess, was a maximum near the surface and decreased to zero at 300 m. On mornings with relatively strong ...
showed that the annual heat production in those cities was equal to approximately one-third of that received from solar radiation. Another study of densely built-up Manhattan in New York City revealed that during the winter, the quantity of heat produced by combustion alone was 2 times greater ...
Urban heat island features of southeast Australian towns. Aust. Meteorol. Mag. 2001, 50, 1–13. [Google Scholar] Ghobadi, A.; Khosravi, M.; Tavousi, T. Surveying of Heat waves Impact on the Urban Heat Islands: Case study, the Karaj City in Iran. Urban Clim. 2018, 24, 600–615....