Importance of radiative transfer processes in urban climate models: A study based on the PALM 6.0 model system

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dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/13134
dc.identifier.uri https://doi.org/10.15488/13030
dc.contributor.author Salim, Mohamed H.
dc.contributor.author Schubert, Sebastian
dc.contributor.author Resler, Jaroslav
dc.contributor.author Krč, Pavel
dc.contributor.author Maronga, Björn
dc.contributor.author Kanani-Sühring, Farah
dc.contributor.author Sühring, Matthias
dc.contributor.author Schneider, Christoph
dc.date.accessioned 2022-11-15T08:45:59Z
dc.date.available 2022-11-15T08:45:59Z
dc.date.issued 2022
dc.identifier.citation Salim, M.H.; Schubert, S.; Resler, J.; Krč, P.; Maronga, B. et al.: Importance of radiative transfer processes in urban climate models: A study based on the PALM 6.0 model system. In: Geoscientific model development : GMD 15 (2022), Nr. 1, S. 145-171. DOI: https://doi.org/10.5194/gmd-15-145-2022
dc.description.abstract Including radiative transfer processes within the urban canopy layer into microscale urban climate models (UCMs) is essential to obtain realistic model results. These processes include the interaction of buildings and vegetation with shortwave and longwave radiation, thermal emission, and radiation reflections. They contribute differently to the radiation budget of urban surfaces. Each process requires different computational resources and physical data for the urban elements. This study investigates how much detail modellers should include to parameterize radiative transfer in microscale building-resolving UCMs. To that end, we introduce a stepwise parameterization method to the Parallelized Large-eddy Simulation Model (PALM) system 6.0 to quantify individually the effects of the main radiative transfer processes on the radiation budget and on the flow field. We quantify numerical simulations of both simple and realistic urban configurations to identify the major and the minor effects of radiative transfer processes on the radiation budget. The study shows that processes such as surface and vegetation interaction with shortwave and longwave radiation will have major effects, while a process such as multiple reflections will have minor effects. The study also shows that radiative transfer processes within the canopy layer implicitly affect the incoming radiation since the radiative transfer model is coupled to the radiation model. The flow field changes considerably in response to the radiative transfer processes included in the model. The study identified those processes which are essentially needed to assure acceptable quality of the flow field. These processes are receiving radiation from atmosphere based on the sky-view factors, interaction of urban vegetation with radiation, radiative transfer among urban surfaces, and considering at least single reflection of radiation. Omitting any of these processes may lead to high uncertainties in the model results. © 2022 Mohamed H. Salim et al. eng
dc.language.iso eng
dc.publisher Katlenburg-Lindau : Copernicus
dc.relation.ispartofseries Geoscientific model development : GMD 15 (2022), Nr. 1
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject Large-Eddy Simulation eng
dc.subject Solar-Radiation eng
dc.subject Wind Flow eng
dc.subject Air-Flow eng
dc.subject Impact eng
dc.subject Balance eng
dc.subject Temperatures eng
dc.subject Sensitivity eng
dc.subject Validation eng
dc.subject Dispersion eng
dc.subject.ddc 910 | Geografie, Reisen ger
dc.title Importance of radiative transfer processes in urban climate models: A study based on the PALM 6.0 model system eng
dc.type Article
dc.type Text
dc.relation.essn 1991-9603
dc.relation.doi https://doi.org/10.5194/gmd-15-145-2022
dc.bibliographicCitation.issue 1
dc.bibliographicCitation.volume 15
dc.bibliographicCitation.firstPage 145
dc.bibliographicCitation.lastPage 171
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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