2015
DOI: 10.1016/j.uclim.2015.09.007
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Evaluation of the seasonal effect of increasing albedo on urban climate and energy consumption of buildings in Montreal

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Cited by 32 publications
(7 citation statements)
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“…Furthermore, higher ground albedo leads to a decrease of air temperature, which agrees with previous studies. When the albedo of road increased from 0.2 to 0.45, the daily-averaged urban heat island intensity of the urban area decreased by about 0.1 • C in Montreal [83]. Similarly, in Rome, a higher improvement of urban temperature is noticed during the daytime where temperature is decreased by 4 • C if the albedo of surfaces increases [84].…”
Section: Discussionmentioning
confidence: 94%
“…Furthermore, higher ground albedo leads to a decrease of air temperature, which agrees with previous studies. When the albedo of road increased from 0.2 to 0.45, the daily-averaged urban heat island intensity of the urban area decreased by about 0.1 • C in Montreal [83]. Similarly, in Rome, a higher improvement of urban temperature is noticed during the daytime where temperature is decreased by 4 • C if the albedo of surfaces increases [84].…”
Section: Discussionmentioning
confidence: 94%
“…The uncontrollable factors, on the other hand, are connected to environment and climate, which consequently lie beyond our control. The warmth produced by anthropogenic sources heats up the urban environment directly, while the solar radiation is partially absorbed by the urban surface and heats up the environment indirectly, over a longer period of time (Touchaei & Akbari, 2015). It is worth to point out here that even though direct solar heating affects urban and rural surface in the same way, it is the indirect solar heating that is one of the biggest causes of UHI and makes the biggest difference.…”
Section: Urban Heat Islandsmentioning
confidence: 94%
“…Temporary effect variables can be cloud cover or wind speed; permanent effect variables are building material, sky view factor or urban green areas system (urban areas contain less vegetation in comparison to rural areas). The cyclic effect variables are solar radiation (which can heat up the environment directlyalbedo or indirectly, by absorbing the heat and emit it slower over time (Touchaei & Akbari, 2015)) and other anthropogenic heat sources (Rizwan et al, 2008). Those are mainly caused by heat released by cars, air conditioning systems or power plants.…”
Section: Urban Heat Islandsmentioning
confidence: 99%
“…The use of trees (Akbari et al, 2001;Krayenhoff and Voogt, 2007) and greening surfaces (Coccolo et al, 2018) improve the urban comfort and the air quality. Moreover, by increasing the albedo using reflective materials in urban areas, the heat storage and buildings energy consumption can be reduced (Morini et al, 2016;Touchaei and Akbari, 2015). To model these UHI mitigation strategies and to increase the understanding of the phenomenon, different urban climate models have been developed.…”
Section: Introductionmentioning
confidence: 99%