Articles | Volume 15, issue 18
https://doi.org/10.5194/acp-15-10309-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-10309-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
18 Sep 2015
Research article |
| 18 Sep 2015
Sensitivity estimations for cloud droplet formation in the vicinity of the high-alpine research station Jungfraujoch (3580 m a.s.l.)
E. Hammer
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
now at: Grolimund + partner AG – environmental engineering, 3018 Bern, Switzerland
N. Bukowiecki
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
B. P. Luo
Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
U. Lohmann
Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
C. Marcolli
Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
Marcolli Chemistry and Physics Consulting GmbH, 8092 Zurich, Switzerland
E. Weingartner
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
now at: Institute for Aerosol and Sensor Technology, University of Applied Sciences and Arts Northwestern Switzerland, Switzerland
U. Baltensperger
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
C. R. Hoyle
CORRESPONDING AUTHOR
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen PSI, Switzerland
Swiss Federal Institute for Forest Snow and Landscape Research (WSL)-Institute for Snow and Avalanche Research (SLF), Davos, Switzerland
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Cited
13 citations as recorded by crossref.
- Observational constraint of in-cloud supersaturation for simulations of aerosol rainout in atmospheric models N. Moteki et al. 10.1038/s41612-019-0063-y
- Stage-resolved in-cloud scavenging of submicron and BC-containing particles: A case study Y. Yang et al. 10.1016/j.atmosenv.2020.117883
- On the CCN (de)activation nonlinearities S. Arabas & S. Shima 10.5194/npg-24-535-2017
- Analysis algorithm for sky type and ice halo recognition in all-sky images S. Boyd et al. 10.5194/amt-12-4241-2019
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Aerosol and dynamical contributions to cloud droplet formation in Arctic low-level clouds G. Motos et al. 10.5194/acp-23-13941-2023
- Aitken mode particles as CCN in aerosol- and updraft-sensitive regimes of cloud droplet formation M. Pöhlker et al. 10.5194/acp-21-11723-2021
- Persistence of orographic mixed‐phase clouds U. Lohmann et al. 10.1002/2016GL071036
- Chemical and physical influences on aerosol activation in liquid clouds: a study based on observations from the Jungfraujoch, Switzerland C. Hoyle et al. 10.5194/acp-16-4043-2016
- Hygroscopicity of aerosol particles and CCN activity of nearly hydrophobic particles in the urban atmosphere over Japan during summer S. Ogawa et al. 10.1002/2015JD024636
- Aerosol–landscape–cloud interaction: signatures of topography effect on cloud droplet formation S. Romakkaniemi et al. 10.5194/acp-17-7955-2017
- Cloud droplet size distribution broadening during diffusional growth: ripening amplified by deactivation and reactivation F. Yang et al. 10.5194/acp-18-7313-2018
- Chemical and physical influences on aerosol activation in liquid clouds: an empirical study based on observations from the Jungfraujoch, Switzerland C. Hoyle et al. 10.5194/acpd-15-15469-2015
12 citations as recorded by crossref.
- Observational constraint of in-cloud supersaturation for simulations of aerosol rainout in atmospheric models N. Moteki et al. 10.1038/s41612-019-0063-y
- Stage-resolved in-cloud scavenging of submicron and BC-containing particles: A case study Y. Yang et al. 10.1016/j.atmosenv.2020.117883
- On the CCN (de)activation nonlinearities S. Arabas & S. Shima 10.5194/npg-24-535-2017
- Analysis algorithm for sky type and ice halo recognition in all-sky images S. Boyd et al. 10.5194/amt-12-4241-2019
- On the drivers of droplet variability in alpine mixed-phase clouds P. Georgakaki et al. 10.5194/acp-21-10993-2021
- Aerosol and dynamical contributions to cloud droplet formation in Arctic low-level clouds G. Motos et al. 10.5194/acp-23-13941-2023
- Aitken mode particles as CCN in aerosol- and updraft-sensitive regimes of cloud droplet formation M. Pöhlker et al. 10.5194/acp-21-11723-2021
- Persistence of orographic mixed‐phase clouds U. Lohmann et al. 10.1002/2016GL071036
- Chemical and physical influences on aerosol activation in liquid clouds: a study based on observations from the Jungfraujoch, Switzerland C. Hoyle et al. 10.5194/acp-16-4043-2016
- Hygroscopicity of aerosol particles and CCN activity of nearly hydrophobic particles in the urban atmosphere over Japan during summer S. Ogawa et al. 10.1002/2015JD024636
- Aerosol–landscape–cloud interaction: signatures of topography effect on cloud droplet formation S. Romakkaniemi et al. 10.5194/acp-17-7955-2017
- Cloud droplet size distribution broadening during diffusional growth: ripening amplified by deactivation and reactivation F. Yang et al. 10.5194/acp-18-7313-2018
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Latest update: 11 Dec 2024
Short summary
An important quantity which determines aerosol activation and cloud formation is the effective peak supersaturation. The box model ZOMM was used to simulate the effective peak supersaturation experienced by an air parcel approaching a high-alpine research station in Switzerland. With the box model the sensitivity of the effective peak supersaturation to key aerosol and dynamical parameters was investigated.
An important quantity which determines aerosol activation and cloud formation is the effective...
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