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The New Canadian Urban Modelling System: Evaluation for Two Cases from the Joint Urban 2003 Oklahoma City Experiment

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Abstract

A new Canadian numerical urban modelling system has been developed at the Meteorological Service of Canada to represent surface and boundary-layer processes in the urban environment. In this system, urban covers are taken into account by including the Town Energy Balance urban-canopy parameterization scheme in the Global Environmental Multiscale meteorological model. The new modelling system is run at 250-m grid size for two intensive observational periods of the Joint Urban 2003 experiment that was held in Oklahoma City, U.S.A. An extensive evaluation against near-surface and upper-air observations has been performed. The Town Energy Balance scheme correctly simulates the urban micro-climate, more particularly the positive nighttime urban heat island, and also reproduces the “cool” island during the morning but does not succeed in maintaining it during all of the daytime period. The vertical structure of the boundary layer above the city is reasonably well simulated, but the simulation of the nocturnal boundary layer is difficult, due to the complex interaction with the nighttime southerly low-level jet that crosses the domain. Sensitivity tests reveal that the daytime convective boundary layer is mainly driven by dry soil conditions in and around Oklahoma City and that the nighttime low-level jet reinforces the urban heat island in the first 300m through large-scale advection, leading to the development of a less stable layer above the city.

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Authors and Affiliations

  1. Meteorological Research Branch, Meteorological Service of Canada, Environment Canada, Dorval, QC, Canada

    Aude Lemonsu, Stephane Belair & Jocelyn Mailhot

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  1. Aude Lemonsu
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  2. Stephane Belair
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  3. Jocelyn Mailhot
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Correspondence to Aude Lemonsu.

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Lemonsu, A., Belair, S. & Mailhot, J. The New Canadian Urban Modelling System: Evaluation for Two Cases from the Joint Urban 2003 Oklahoma City Experiment. Boundary-Layer Meteorol 133, 47–70 (2009). https://doi.org/10.1007/s10546-009-9414-2

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  • DOI: https://doi.org/10.1007/s10546-009-9414-2

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