Impact of spectral coupling between urban atmosphere and sky boundary conditions in a street canyon
Most radiative transfer models developed for the analysis of urban configurations consider a transparent urban atmosphere and gray sky conditions. The aim of the present work is to investigate these assumptions, focusing on the longwave domain. For this purpose, reference Line-by-Line Monte-Carlo ca...
Saved in:
Published in | Journal of quantitative spectroscopy & radiative transfer Vol. 326; p. 109107 |
---|---|
Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.11.2024
Elsevier |
Subjects | |
Online Access | Get full text |
Cover
Loading…
Summary: | Most radiative transfer models developed for the analysis of urban configurations consider a transparent urban atmosphere and gray sky conditions. The aim of the present work is to investigate these assumptions, focusing on the longwave domain. For this purpose, reference Line-by-Line Monte-Carlo calculations are first performed. A more efficient radiative transfer model based on the Finite Volume Method and SLW modeling is also developed to treat several street canyon configurations. The aspect ratio of the street canyon, a parameter frequently encountered in urban scenarios, is considered for the analysis. It is shown that, in most cases, real urban problems need to take into account a non-gray participating atmosphere within the streets, together with its spectral coupling with the non-gray sky downward radiation, to provide accurate net fluxes on urban surfaces and volumetric radiative powers in the urban atmosphere.
•The interaction between radiation and the atmosphere is studied in a street canyon.•The strong spectral coupling between sky emission and air absorption is analyzed.•An efficient model (FVM-SLW) is proposed to accurately simulate these interactions.•A parametric study of wall fluxes with respect to street aspect ratio is carried out. |
---|---|
ISSN: | 0022-4073 1879-1352 |
DOI: | 10.1016/j.jqsrt.2024.109107 |