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Tests of three urban energy balance models

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TLDR
In this paper, the authors used observations of surface characteristics, meteorological conditions and energy balance components from Vancouver, B.C. to test the validity of the output from three one-dimensional surface energy balance models.
Abstract
Observations of surface characteristics, meteorological conditions and energy balance components from Vancouver, B.C. are used to test the validity of the output from three one-dimensional surface energy balance models. The results show that whereas all of the models provide good simulations of net radiation, none can consistently predict the turbulent fluxes of sensible and latent heat using easily available input data. Inability to handle the role of water availability and its impact on evapotranspiration is identified as the principal problem.

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A physically-based scheme for the urban energy budget in atmospheric models

TL;DR: In this paper, an urban surface scheme for atmospheric mesoscale models is presented, which is aimed to be as general as possible, to represent any city in the world, for any time or weather condition (heat island cooling by night, urban wake, water evaporation after rainfall and snow effects).
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The urban energy balance

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The micrometeorology of the urban forest

TL;DR: In this paper, the radiative, aerodynamic, thermal and moisture properties of urban trees are discussed in relation to other urban materials and surfaces in terms of their exchanges of heat, mass and momentum with the atmosphere, and their ability to produce shade, coolness, shelter, moisture and air filtration makes them flexible tools for environmental design.
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An evapotranspiration‐interception model for urban areas

TL;DR: In this article, a model to calculate evapotranspiration from urban areas over a wide range of meteorological conditions is presented, which is applicable to areas ranging from the size of city blocks to land use zones and time periods of one hour and longer.
References
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Journal ArticleDOI

Boundary Layer Climates.

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Boundary layer climates

TL;DR: This modern climatology textbook explains those climates formed near the ground in terms of the cycling of energy and mass through systems.
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Evaporation into the atmosphere

TL;DR: In this paper, the authors describe the process of evaporation into the atmosphere and its effect on the environment. But they do not discuss its application in the field of meteorology.
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Canyon geometry and the nocturnal urban heat island: Comparison of scale model and field observations

TL;DR: 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.
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