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Modeling organic aerosol over Central Europe: uncertainties linked to different chemical mechanisms, parameterizations, and boundary conditions

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985858%3A_____%2F25%3A00641253" target="_blank" >RIV/67985858:_____/25:00641253 - isvavai.cz</a>

  • Alternative codes found

    RIV/00020699:_____/25:N0000140 RIV/00216208:11320/25:10508722

  • Result on the web

    <a href="https://acp.copernicus.org/articles/25/15301/2025/acp-25-15301-2025.pdf" target="_blank" >https://acp.copernicus.org/articles/25/15301/2025/acp-25-15301-2025.pdf</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/acp-25-15301-2025" target="_blank" >10.5194/acp-25-15301-2025</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Modeling organic aerosol over Central Europe: uncertainties linked to different chemical mechanisms, parameterizations, and boundary conditions

  • Original language description

    This study explores the uncertainties in modeling organic aerosol (OA) over Central Europe, focusing on the roles of chemical mechanisms, emission parameterizations, and boundary conditions. Organic aerosols, particularly secondary organic aerosols (SOAs), significantly influence climate, health, and visibility, comprising up to 90 % of submicron particulate matter. Using the Comprehensive Air Quality Model with Extensions (CAMx) coupled with the Weather Research and Forecast Model, sensitivity analyses were conducted to assess the impact of intermediate-volatility organic compounds (IVOCs), semi-volatile organic compounds (SVOCs), and chemical boundary conditions on primary and secondary organic aerosol concentrations. Model evaluation against organic carbon measurements over the Czech Republic showed that including source-specific IVOC and SVOC emissions significantly improved CAMx's performance, particularly when using the 1.5-dimensional Volatility Basis Set framework with activated chemical aging. For example, the domain-averaged SOA concentrations increased by up to 1.17 µg m−3 during summer when both IVOC and SVOC emissions were included. Furthermore, incorporating OA into the boundary conditions enhanced model predictions, with the accuracy of modeled organic carbon concentrations significantly improved during summer at some monitoring sites. Despite these improvements, challenges remain due to uncertainties in emission estimates, parameterization schemes, and the spatial resolution of the models. The findings underscore the importance of refined parameterizations for IVOC and SVOC emissions, higher temporal and spatial resolution in chemical boundary conditions, and better representation of chemical aging. Addressing these gaps in future studies will further enhance the understanding and prediction of OA dynamics in regional air quality modeling.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10509 - Meteorology and atmospheric sciences

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Atmospheric Chemistry and Physics

  • ISSN

    1680-7316

  • e-ISSN

    1680-7324

  • Volume of the periodical

    25

  • Issue of the periodical within the volume

    21

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    28

  • Pages from-to

    15301-15328

  • UT code for WoS article

    001610229900001

  • EID of the result in the Scopus database

    2-s2.0-105021269174