KEY CONCLUSIONS OF THE FIRST INTERNATIONAL URBAN LAND SURFACE MODEL COMPARISON PROJECT

The First International Urban Land Surface Model Comparison was designed to identify three aspects of the urban surface–atmosphere interactions: 1) the dominant physical processes, 2) the level of complexity required to model these, and 3) the parameter requirements for such a model. Offline simulat...

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Published in:Bulletin of the American Meteorological Society Vol. 96; no. 5; pp. 805 - 822
Main Authors: Best, M. J., Grimond, C. S. B.
Format: Journal Article
Language:English
Published: Boston American Meteorological Society 01-05-2015
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Abstract The First International Urban Land Surface Model Comparison was designed to identify three aspects of the urban surface–atmosphere interactions: 1) the dominant physical processes, 2) the level of complexity required to model these, and 3) the parameter requirements for such a model. Offline simulations from 32 land surface schemes, with varying complexity, contributed to the comparison. Model results were analyzed within a framework of physical classifications and over four stages. The results show that the following are important urban processes: i) multiple reflections of shortwave radiation within street canyons; ii) reduction in the amount of visible sky from within the canyon, which impacts the net longwave radiation; iii) the contrast in surface temperatures between building roofs and street canyons; and iv) evaporation from vegetation. Models that use an appropriate bulk albedo based on multiple solar reflections, represent building roof surfaces separately from street canyons and include a representation of vegetation demonstrate more skill, but require parameter information on the albedo, height of the buildings relative to the width of the streets (height to width ratio), the fraction of building roofs compared to street canyons from a plan view (plan area fraction), and the fraction of the surface that is vegetated. These results, while based on a single site and less than 18 months of data, have implications for the future design of urban land surface models, the data that need to be measured in urban observational campaigns, and what needs to be included in initiatives for regional and global parameter databases.
AbstractList The First International Urban Land Surface Model Comparison was designed to identify three aspects of the urban surface-atmosphere interactions: 1) the dominant physical processes, 2) the level of complexity required to model these, and 3) the parameter requirements for such a model. Offline simulations from 32 land surface schemes, with varying complexity, contributed to the comparison. Model results were analyzed within a framework of physical classifications and over four stages. The results show that the following are important urban processes: i) multiple reflections of shortwave radiation within street canyons; ii) reduction in the amount of visible sky from within the canyon, which impacts the net longwave radiation; iii) the contrast in surface temperatures between building roofs and street canyons; and iv) evaporation from vegetation. Models that use an appropriate bulk albedo based on multiple solar reflections, represent building roof surfaces separately from street canyons and include a representation of vegetation demonstrate more skill, but require parameter information on the albedo, height of the buildings relative to the width of the streets (height to width ratio), the fraction of building roofs compared to street canyons from a plan view (plan area fraction), and the fraction of the surface that is vegetated. These results, while based on a single site and less than 18 months of data, have implications for the future design of urban land surface models, the data that need to be measured in urban observational campaigns, and what needs to be included in initiatives for regional and global parameter databases.
The urban heat island results from differences in surface energy exchanges between the urban environment and its surrounding rural area. [...]an understanding of these differences is needed to interpret the urban heat island. [...]a larger proportion of this energy for heating is held within the fabric of the buildings, given the large thermal inertia of the materials, resulting in changes in the diurnal cycle of urban temperatures. [...]an additional source of heating within the urban areas comes from human activities such as transport, the internal heating of the buildings, and the metabolic rates of the people themselves (e.g., Sailor and Lu 2004).
Audience Trade
Academic
Author Grimond, C. S. B.
Best, M. J.
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  givenname: C. S. B.
  surname: Grimond
  fullname: Grimond, C. S. B.
  organization: University of Reading, Reading, United Kingdom
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Snippet The First International Urban Land Surface Model Comparison was designed to identify three aspects of the urban surface–atmosphere interactions: 1) the...
The urban heat island results from differences in surface energy exchanges between the urban environment and its surrounding rural area. [...]an understanding...
The First International Urban Land Surface Model Comparison was designed to identify three aspects of the urban surface-atmosphere interactions: 1) the...
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SubjectTerms Atmospheric boundary layer
Atmospheric models
Buildings
Canyons
Climate change
Climate models
Environmental aspects
Heat flux
Heating
Hurricanes
Measurement
Meteorology
Meteors
Metropolitan areas
Modeling
Mortality
Natural history
Parametric models
Rural areas
Solar radiation
Urban areas
Urban environments
Urban heat islands
Weather
Title KEY CONCLUSIONS OF THE FIRST INTERNATIONAL URBAN LAND SURFACE MODEL COMPARISON PROJECT
URI https://www.jstor.org/stable/26219612
https://www.proquest.com/docview/1692750104
https://search.proquest.com/docview/1701489902
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