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Canyon geometry and the nocturnal urban heat island: Comparison of scale model and field observations

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TLDR
In this paper, a simple hardware scale model is used to simulate nocturnal cooling rates for rural and urban environments under calm and cloudless conditions, and the results of the experiments show that canyon geometry in the central portion of a city (as measured by the sky view factor) is a relevant variable in producing nocturnurnal urban heat islands due to its role in regulating long-wave radiative heat loss.
Abstract
A simple hardware scale model is used to simulate nocturnal cooling rates for rural and urban environments under calm and cloudless conditions. Comparison with field observations gathered under similar conditions shows the model capable of reproducing many of the features of the temporal development of urban heat islands and the long-wave radiative exchange in urban canyons. The model is used to investigate the roles played by rural/urban differences in geometry and thermal admittance. The results of the experiments show that canyon geometry in the central portion of a city (as measured by the sky view factor) is a relevant variable in producing nocturnal urban heat islands due to its role in regulating long-wave radiative heat loss. It is also demonstrated that this measure is central to the relationship between city size and heat island intensity. The importance of canyon geometry as a feature of urban design is discussed. Thermal admittance differences can also produce realistic heat island features but their magnitude requires quantification in the field.

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Citations
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Spatio-temporal patterns in green infrastructure as driver of land surface temperature variability: The case of Sydney

TL;DR: Results for spatial clustering demonstrate that the GIT scheme can be implemented for a rapid identification of hotspots to prioritise urban areas for heat mitigation and statistical results confirm that LST differences among GIT classes are statistically significant for different times of the day and seasons.
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Simulation and validation of radiative transfers in urbanised areas

TL;DR: In this article, a 3D-numeric simulation of heat transfer in an urban canyon and the validation of the appropriate algorithms and results is presented, where the simulation procedure and parameterisation of the surface elements are briefly described.
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Effects of urban and landscape elements on air temperature in a high-density subtropical city

TL;DR: In this article, the authors examined the effects of key urban and landscape parameters on air temperature, and the impacts of weather conditions on landscape-temperature relationship, and found that the effect of weather (cloud amount, solar radiation and wind speed) on landscape temperature relationships were minor.
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Derivation of sky-view factors from lidar data

TL;DR: In this article, the Lidar data is used to generate a spatial map of SVFs which are then compared against photographically-derived SVF at selected point locations, finding that there was generally good agreement between the two methodologies, although with decreasing SVF the LIDar-derived technique tended to overestimate the SVF.
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Characterization of the urban heat island at Toronto: Revisiting the choice of rural sites using a measure of day-to-day variation

TL;DR: In this article, the authors revisited the selection of three rural stations (Albion Field Centre, Millgrove, and King Smoke Tree) and two urban stations (Toronto and Toronto Pearson International Airport) that have previously been used to perform UHI analysis in Toronto, Ontario, Canada.
References
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Journal ArticleDOI

City size and the urban heat island

TL;DR: In this article, the authors demonstrate the relationship existing between the size of a village, town or city and the magnitude of the urban heat island it produces by analyzing data gathered by automobile traverses in 10 settlements on the St. Lawrence Lowland, whose populations range from 1000 to 2 million inhabitants.
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The distinction between canopy and boundary‐layer urban heat islands

TL;DR: In this paper, air temperature measurements from car traverses in and near Vancouver, BC are used to test two urban heat island models: one an empirical model, the other a theoretical advective model.
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Satellite Estimation of the Surface Energy Balance, Moisture Availability and Thermal Inertia.

TL;DR: In this article, a method for inferring the distribution of surface heat and evaporative fluxes and the ground moisture availability and thermal inertia (ground conductive capacity) was used to analyze two urbanized areas, Los Angeles and St. Louis.
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Urban heat island dynamics in Montreal and Vancouver

TL;DR: In this paper, the role of urban and rural surfaces in the growth and decay of the urban heat island was investigated and the results suggest that nocturnal energy exchange in the city is complex.