2019
DOI: 10.1002/qj.3505
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On‐ and off‐line evaluation of the single‐layer urban canopy model in London summertime conditions

Abstract: Urban canopy models are essential tools for forecasting weather and air quality in cities. However, they require many surface parameters, which are uncertain and can reduce model performance if inappropriately prescribed. Here, we evaluate the model sensitivity of the single‐layer urban canopy model (SLUCM) in the Weather Research and Forecasting (WRF) model to surface parameters in two different configurations, one coupled to the overlying atmosphere (on‐line) in a 1D configuration and one without coupling (o… Show more

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Cited by 11 publications
(24 citation statements)
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“…Boundary conditions for the 1-D WRF model are applied in the form of subsidence, geostrophic wind, and advection tendency terms for potential temperature, moisture, and u and v wind components. Geostrophic wind is derived from 6-hourly ECMWF operational reanalysis data (ECMWF, 2012) in combination with a 3-D WRF simulations (hourly data) (Steeneveld et al, 2017;Tsiringakis et al, 2019). Geostrophic wind values are given as 6-hourly means, with a tendency term applied to the u and v geostrophic wind components at each time step (of 1-D WRF) to ensure a smooth change in geostrophic wind through the 6-hourly blocks and avoid oscillations from imbalance between actual and geostrophic wind speeds.…”
Section: Case Study Descriptionmentioning
confidence: 99%
See 1 more Smart Citation
“…Boundary conditions for the 1-D WRF model are applied in the form of subsidence, geostrophic wind, and advection tendency terms for potential temperature, moisture, and u and v wind components. Geostrophic wind is derived from 6-hourly ECMWF operational reanalysis data (ECMWF, 2012) in combination with a 3-D WRF simulations (hourly data) (Steeneveld et al, 2017;Tsiringakis et al, 2019). Geostrophic wind values are given as 6-hourly means, with a tendency term applied to the u and v geostrophic wind components at each time step (of 1-D WRF) to ensure a smooth change in geostrophic wind through the 6-hourly blocks and avoid oscillations from imbalance between actual and geostrophic wind speeds.…”
Section: Case Study Descriptionmentioning
confidence: 99%
“…Here we briefly evaluate the 50 m air temperature and net all-wave radiation (Q * ). For a more extensive evaluation see Tsiringakis et al (2019).…”
Section: Model Evaluation For the Reference Model Setupmentioning
confidence: 99%
“…At present, research on urban heat environment risk focuses on mapping heat risk and vulnerability in various environments [5][6][7], especially in the context of global climate change and heat waves [8][9][10]. Researchers have endeavored to employ theoretical and technical methods, such as statistical [11][12][13][14][15][16][17][18][19], energy-balance [3,4,20], numerical [21][22][23], analytical [24], and physical models [25]. For this process, researchers usually grade and evaluate air temperature data from meteorological stations and the LST data observed via remote sensing from the perspective of climate vulnerability or human exposure [26], and developed some vulnerability and risk indexes, such as manual indicator removal [27], as well as more complicated techniques, such as Monte Carlo simulation and variance-based global sensitivity analysis [28].…”
Section: Introductionmentioning
confidence: 99%
“…The scheme translates modelled values of heat, wind etc. down from the first model level into an urban canyon value when coupled to the actual atmospheric model (Tsiringakis et al, 2019). Since the UCM is only one layer, it circumvents the erratic vertical behaviour of turbulent quantities in the urban canyon.…”
Section: The Urban Problemmentioning
confidence: 99%
“…Most urban model studies are specifically interested in the Urban Canopy Layer and its vertical interactions with the air aloft and the surface (e.g. Tsiringakis et al, 2019), rather than the UBL as a whole. The bulk model is however very suitable to research how the different urban surface influences the entire boundary layer on a larger scale: the effect of the entire city, as it were.…”
Section: Conceptual Modellingmentioning
confidence: 99%