Anthropogenic Vehicular Heat and Its Influence on Urban Planning

被引:4
|
作者
Grajeda-Rosado, Ruth M. [1 ]
Alonso-Guzman, Elia M. [2 ]
Escobar-Del Pozo, Carlos [3 ]
Esparza-Lopez, Carlos J. [4 ]
Sotelo-Salas, Cristina [5 ]
Martinez-Molina, Wilfrido [2 ]
Mondragon-Olan, Max [1 ]
Cabrera-Macedo, Alfonso [4 ]
机构
[1] Univ Veracruzana, Architecture Program, Xalapa 94294, Veracruz, Mexico
[2] Univ Michoacana, Civil Engn Sch, Morelia 58040, Michoacan, Mexico
[3] Univ Colima, Fac Mech & Elect Engn, Colima 28040, Mexico
[4] Univ Colima, Fac Architecture & Design, Colima 28040, Mexico
[5] Univ Autonoma Baja California, Fac Architecture & Design, Mexicali 21280, Baja California, Mexico
关键词
anthropogenic vehicular heat; urban canyon; urban heat island; THERMAL COMFORT; ISLAND; CITY; IMPACT; TEMPERATURE; ENVIRONMENT; EMISSIONS; CANYON; LAYER;
D O I
10.3390/atmos13081259
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Anthropogenic heat (QF) is one of the parameters that contributes to the urban heat island (UHI) phenomenon. Usually, this variable is studied holistically, among other anthropogenic flux such as industrial, vehicular, buildings, and human metabolism, due to the complexity of data collection through field measurements. The aim of this paper was to weigh vehicular anthropogenic heat and its impact on the thermal profile of an urban canyon. A total of 108 simulations were carried out, using the ANSYS Fluent (R) software, incorporating variables such as the number of vehicles, wind speed, urban canyon orientation, and urban canyon aspect ratio. The results were compared with a database of 61 American cities in 2015 and showed that orientation is the main factor of alteration in vehicular heat flow, increasing it in a range of 2 degrees C to 6.5 degrees C, followed by the wind speed (1.2 to 2.2 m/s), which allows for decreases of 1 to 3.8 degrees C. The exploration of these variables and their weighing in the definition of urban street canyon temperature profiles at the canopy level of urban structures provides valuable information on the hygrothermal comfort of its inhabitants; its appropriate quantification can be an example of many urban energy balances altering processes.
引用
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页数:16
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