2023
DOI: 10.5194/egusphere-2022-978
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Effect of radiation interaction and aerosol processes on ventilation and aerosol concentrations in a real urban neighbourhood in Helsinki

Abstract: Abstract. Large eddy simulation (LES) provides an optimal tool to examine air pollutant concentrations at high temporal and spatial resolutions within urban neighborhoods. The local mixing conditions are to a large extent a result of building morphology and thermal conditions impacting mechanically and thermally driven turbulence. However, the impact of thermal conditions on local air pollutant concentrations in real urban environments is not well understood nor the importance of including thermal processes in… Show more

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“…As non-gaseous constituents, RRTM can consider aerosols and clouds, but in our current framework only clouds are considered by the mixing ratios of liquid water and cloud ice, and the effective particle radii, which are assumed to be 10 µm for cloud water and 30 µm for cloud ice. While additionally considering urban aerosol radiative effects can decrease the model temperature bias (e.g., Strömberg et al, 2023), it would significantly increase model complexity and also simulation time, because other aerosol species aside from the currently simulated BC had to be included. The radiative transfer equations are solved for the entire vertical extent of the troposphere and lower stratosphere, but of the required input data for clouds, only q c is provided with high spatial resolution within the vertical height range of the CAIRDIO computation domain.…”
Section: A2 Anelastic Approximation Cloud Microphysics and Radiative ...mentioning
confidence: 99%
“…As non-gaseous constituents, RRTM can consider aerosols and clouds, but in our current framework only clouds are considered by the mixing ratios of liquid water and cloud ice, and the effective particle radii, which are assumed to be 10 µm for cloud water and 30 µm for cloud ice. While additionally considering urban aerosol radiative effects can decrease the model temperature bias (e.g., Strömberg et al, 2023), it would significantly increase model complexity and also simulation time, because other aerosol species aside from the currently simulated BC had to be included. The radiative transfer equations are solved for the entire vertical extent of the troposphere and lower stratosphere, but of the required input data for clouds, only q c is provided with high spatial resolution within the vertical height range of the CAIRDIO computation domain.…”
Section: A2 Anelastic Approximation Cloud Microphysics and Radiative ...mentioning
confidence: 99%