Articles | Volume 20, issue 20
https://doi.org/10.5194/acp-20-11841-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-11841-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Oct 2020
Research article |
| 21 Oct 2020
| 21 Oct 2020
Roll vortices induce new particle formation bursts in the planetary boundary layer
Janne Lampilahti
CORRESPONDING AUTHOR
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Hanna Elina Manninen
CERN, 1211 Geneva, Switzerland
Katri Leino
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Riikka Väänänen
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Antti Manninen
Finnish Meteorological Institute, Helsinki, Finland
Stephany Buenrostro Mazon
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Tuomo Nieminen
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Matti Leskinen
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Joonas Enroth
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Marja Bister
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Sergej Zilitinkevich
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Finnish Meteorological Institute, Helsinki, Finland
Department of Radiophysics, University of Nizhny, Novgorod, Russia
Juha Kangasluoma
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
Heikki Järvinen
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Veli-Matti Kerminen
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Tuukka Petäjä
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University, Nanjing, China
Markku Kulmala
Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Science and Engineering, Beijing University of Chemical Technology, Beijing, China
Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University, Nanjing, China
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Cited
8 citations as recorded by crossref.
- The striking effect of vertical mixing in the planetary boundary layer on new particle formation in the Yangtze River Delta S. Lai et al. 10.1016/j.scitotenv.2022.154607
- Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere L. Beck et al. 10.5194/acp-22-8547-2022
- Vertical transport of ultrafine particles and turbulence evolution impact on new particle formation at the surface & Canton Tower H. Wu et al. 10.1016/j.atmosres.2024.107290
- On Estimation of the Contribution of Secondary Vortex Structures to the Transport of Aerosols in the Atmospheric Boundary Layer M. Davydova et al. 10.1134/S001546282208002X
- Measurement report: Atmospheric new particle formation at a peri-urban site in Lille, northern France S. Crumeyrolle et al. 10.5194/acp-23-183-2023
- Zeppelin-led study on the onset of new particle formation in the planetary boundary layer J. Lampilahti et al. 10.5194/acp-21-12649-2021
- Rapid cloud removal of dimethyl sulfide oxidation products limits SO 2 and cloud condensation nuclei production in the marine atmosphere G. Novak et al. 10.1073/pnas.2110472118
- Clouds over Hyytiälä, Finland: an algorithm to classify clouds based on solar radiation and cloud base height measurements I. Ylivinkka et al. 10.5194/amt-13-5595-2020
7 citations as recorded by crossref.
- The striking effect of vertical mixing in the planetary boundary layer on new particle formation in the Yangtze River Delta S. Lai et al. 10.1016/j.scitotenv.2022.154607
- Diurnal evolution of negative atmospheric ions above the boreal forest: from ground level to the free troposphere L. Beck et al. 10.5194/acp-22-8547-2022
- Vertical transport of ultrafine particles and turbulence evolution impact on new particle formation at the surface & Canton Tower H. Wu et al. 10.1016/j.atmosres.2024.107290
- On Estimation of the Contribution of Secondary Vortex Structures to the Transport of Aerosols in the Atmospheric Boundary Layer M. Davydova et al. 10.1134/S001546282208002X
- Measurement report: Atmospheric new particle formation at a peri-urban site in Lille, northern France S. Crumeyrolle et al. 10.5194/acp-23-183-2023
- Zeppelin-led study on the onset of new particle formation in the planetary boundary layer J. Lampilahti et al. 10.5194/acp-21-12649-2021
- Rapid cloud removal of dimethyl sulfide oxidation products limits SO 2 and cloud condensation nuclei production in the marine atmosphere G. Novak et al. 10.1073/pnas.2110472118
Latest update: 20 Nov 2024
Short summary
In this work, by using co-located airborne and ground-based measurements, we show that counter-rotating horizontal circulations in the planetary boundary layer (roll vortices) frequently enhance regional new particle formation or induce localized bursts of new particle formation. These observations can be explained by the ability of the rolls to efficiently lift low-volatile vapors emitted from the surface to the top of the boundary layer where new particle formation is more favorable.
In this work, by using co-located airborne and ground-based measurements, we show that...
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