On the influence of vertical mixing, boundary layer schemes, and temporal emission profiles on tropospheric NO2 in WRF-Chem – comparisons to in situ, satellite, and MAX-DOAS observations

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Abstract × NO 2 × NO 2 NO 2 - R = 0.74. The best agreement is achieved when correcting for the presumed NO y NO y HNO 3 NO 2 + R = 0.87 for monthly means. Lastly, simulated NO 2 NO 2 - + + NO 2 to the mixing processes in the boundary layer and the diurnal distribution of emissions.

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: On the influence of vertical mixing, boundary layer schemes, and temporal emission profiles on tropospheric NO₂ in WRF-Chem – comparisons to in situ, satellite, and MAX-DOAS observations ; volume:24 ; number:1 ; year:2024 ; pages:185-217 ; extent:33
Atmospheric chemistry and physics ; 24, Heft 1 (2024), 185-217 (gesamt 33)

Creator: Kuhn, Leon
Beirle, Steffen
Kumar, Vinod
Osipov, Sergey
Pozzer, Andrea
Bösch, Tim
Kumar, Rajesh
Wagner, Thomas

DOI: 10.5194/acp-24-185-2024

URN: urn:nbn:de:101:1-2024011103173305369785

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:21 AM CEST

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Kuhn, Leon
Beirle, Steffen
Kumar, Vinod
Osipov, Sergey
Pozzer, Andrea
Bösch, Tim
Kumar, Rajesh
Wagner, Thomas

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On the influence of vertical mixing, boundary layer schemes, and temporal emission profiles on tropospheric NO<sub>2</sub> in WRF-Chem – comparisons to in situ, satellite, and MAX-DOAS observations

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Other Objects (12)

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Mobile MAX-DOAS observations of tropospheric NO<sub>2</sub> and HCHO during summer over the Three Rivers’ Source region in China

Mobile MAX-DOAS observations of tropospheric NO<sub>2</sub> and HCHO during summer over the Three Rivers’ Source region in China

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