Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia

The atmospheric composition in urban areas is one of the primary tasks in air pollution studies. The research aims to provide a statistically reliable assessment of the atmospheric composition climate of the city of Sofia—typical and extreme features of the special/temporal behavior, annual means, s...

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Autores principales: Vladimir Ivanov, Ivelina Georgieva
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/8b43c9b8330a485b88546dac2dd4e082
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spelling oai:doaj.org-article:8b43c9b8330a485b88546dac2dd4e0822021-11-25T16:44:56ZBasic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia10.3390/atmos121114502073-4433https://doaj.org/article/8b43c9b8330a485b88546dac2dd4e0822021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1450https://doaj.org/toc/2073-4433The atmospheric composition in urban areas is one of the primary tasks in air pollution studies. The research aims to provide a statistically reliable assessment of the atmospheric composition climate of the city of Sofia—typical and extreme features of the special/temporal behavior, annual means, seasonal and diurnal variations. For that purpose, extensive numerical simulations of the atmospheric composition fields in Sofia city have been performed. Three models were chosen as modeling tools. We used WRF as a meteorological pre-processor, CMAQ as a chemical transport model, and SMOKE as the emission pre-processor of Models-3 system. We developed the following conclusions. The daily concentration changes of the two essential air pollution species—nitrogen dioxide (NO<sub>2</sub>) and fine particle matters (FPRM, particulate matter (PM<sub>2.5</sub>), which has a diameter between 0 and 2.5 micrometers)—have different magnitudes. Second, the emissions relative contributions to the concentration of different species could be different, varying from 0% to above 100%. The contributions of different emission categories to other species surface concentrations have various diurnal courses. Last, the total concentration change (ΔC) is different for each pollutant. The sign of the contributions of some processes is evident. Still, some may have different signs depending on the type of emissions, weather conditions, or topography.Vladimir IvanovIvelina GeorgievaMDPI AGarticleatmospheric compositiondynamic and chemical processesensemble of numerical simulationprocess analysiscontribution of different emission sourcesMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1450, p 1450 (2021)
institution DOAJ
collection DOAJ
language EN
topic atmospheric composition
dynamic and chemical processes
ensemble of numerical simulation
process analysis
contribution of different emission sources
Meteorology. Climatology
QC851-999
spellingShingle atmospheric composition
dynamic and chemical processes
ensemble of numerical simulation
process analysis
contribution of different emission sources
Meteorology. Climatology
QC851-999
Vladimir Ivanov
Ivelina Georgieva
Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
description The atmospheric composition in urban areas is one of the primary tasks in air pollution studies. The research aims to provide a statistically reliable assessment of the atmospheric composition climate of the city of Sofia—typical and extreme features of the special/temporal behavior, annual means, seasonal and diurnal variations. For that purpose, extensive numerical simulations of the atmospheric composition fields in Sofia city have been performed. Three models were chosen as modeling tools. We used WRF as a meteorological pre-processor, CMAQ as a chemical transport model, and SMOKE as the emission pre-processor of Models-3 system. We developed the following conclusions. The daily concentration changes of the two essential air pollution species—nitrogen dioxide (NO<sub>2</sub>) and fine particle matters (FPRM, particulate matter (PM<sub>2.5</sub>), which has a diameter between 0 and 2.5 micrometers)—have different magnitudes. Second, the emissions relative contributions to the concentration of different species could be different, varying from 0% to above 100%. The contributions of different emission categories to other species surface concentrations have various diurnal courses. Last, the total concentration change (ΔC) is different for each pollutant. The sign of the contributions of some processes is evident. Still, some may have different signs depending on the type of emissions, weather conditions, or topography.
format article
author Vladimir Ivanov
Ivelina Georgieva
author_facet Vladimir Ivanov
Ivelina Georgieva
author_sort Vladimir Ivanov
title Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
title_short Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
title_full Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
title_fullStr Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
title_full_unstemmed Basic Facts about Numerical Simulations of Atmospheric Composition in the City of Sofia
title_sort basic facts about numerical simulations of atmospheric composition in the city of sofia
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/8b43c9b8330a485b88546dac2dd4e082
work_keys_str_mv AT vladimirivanov basicfactsaboutnumericalsimulationsofatmosphericcompositioninthecityofsofia
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