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 |
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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. |
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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. |
Author_xml | – sequence: 1 givenname: M. J. surname: Best fullname: Best, M. J. organization: Met Office, Exeter, United Kingdom, and King’s College London, London, United Kingdom – sequence: 2 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 |
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