4.4 Article

Evaluation of the SPARTACUS-Urban Radiation Model for Vertically Resolved Shortwave Radiation in Urban Areas

Journal

BOUNDARY-LAYER METEOROLOGY
Volume 184, Issue 2, Pages 301-331

Publisher

SPRINGER
DOI: 10.1007/s10546-022-00706-9

Keywords

The DART model; Shortwave radiation; The SPARTACUS-Urban model; Urban form

Funding

  1. Scenario NERC Doctoral Training Partnership Grant
  2. EPSRC [2130186]
  3. EPRSC DARE [EP/P002331/1]
  4. ERC urbisphere [855005]
  5. Newton Fund/Met Office CSSP China NGC
  6. European Research Council (ERC) [855005] Funding Source: European Research Council (ERC)

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The study evaluates a multi-layer radiative transfer model, SPARTACUS-Urban, for numerical weather prediction. The model accurately predicts shortwave fluxes when building distribution assumptions are fulfilled. However, it underestimates albedo and ground absorption, and overestimates wall-plus-roof absorption for realistic geometry.
The heterogenous structure of urban environments impacts interactions with radiation, and the intensity of urban-atmosphere exchanges. Numerical weather prediction (NWP) often characterizes the urban structure with an infinite street canyon, which does not capture the three-dimensional urban morphology realistically. Here, the SPARTACUS (Speedy Algorithm for Radiative Transfer through Cloud Sides) approach to urban radiation (SPARTACUS-Urban), a multi-layer radiative transfer model designed to capture three-dimensional urban geometry for NWP, is evaluated with respect to the explicit Discrete Anisotropic Radiative Transfer (DART) model. Vertical profiles of shortwave fluxes and absorptions are evaluated across domains spanning regular arrays of cubes, to real cities (London and Indianapolis). The SPARTACUS-Urban model agrees well with the DART model (normalized bias and mean absolute errors < 5.5%) when its building distribution assumptions are fulfilled (i.e., buildings randomly distributed in the horizontal). For realistic geometry, including real-world building distributions and pitched roofs, SPARTACUS-Urban underestimates the effective albedo (< 6%) and ground absorption (< 16%), and overestimates wall-plus-roof absorption (< 15%), with errors increasing with solar zenith angle. Replacing the single-exponential fit of the distribution of building separations with a two-exponential function improves flux predictions for real-world geometry by up to half. Overall, SPARTACUS-Urban predicts shortwave fluxes accurately for a range of geometries (cf. DART). Comparison with the commonly used single-layer infinite street canyon approach finds SPARTACUS-Urban has an improved performance for randomly distributed and real-world geometries. This suggests using SPARTACUS-Urban would benefit weather and climate models with multi-layer urban energy balance models, as it allows more realistic urban form and vertically resolved absorption rates, without large increases in computational cost or data inputs.

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