Articles | Volume 22, issue 13
https://doi.org/10.5194/acp-22-8973-2022
https://doi.org/10.5194/acp-22-8973-2022
Research article
 | 
12 Jul 2022
Research article |  | 12 Jul 2022

Do Arctic mixed-phase clouds sometimes dissipate due to insufficient aerosol? Evidence from comparisons between observations and idealized simulations

Lucas J. Sterzinger, Joseph Sedlar, Heather Guy, Ryan R. Neely III, and Adele L. Igel

Related authors

Above-cloud concentrations of cloud condensation nuclei help to sustain some Arctic low-level clouds
Lucas J. Sterzinger and Adele L. Igel
Atmos. Chem. Phys., 24, 3529–3540, https://doi.org/10.5194/acp-24-3529-2024,https://doi.org/10.5194/acp-24-3529-2024, 2024
Short summary

Cited articles

Bergeron, T.: On the physics of clouds and precipitation, Proc. 5th Assembly U. G. G. I., Lisbon, Portugal, 1935, pp. 156–180, https://ci.nii.ac.jp/naid/10024028214/ (last access: 14 January 2022), 1935. a
Bharadwaj, N.: Millimeter Wavelength Cloud Radar (MMCRMOM), Department of Energy Atmospheric Radiation Measurement user facility [data set], https://doi.org/10.5439/1025228, 2010. a
Birch, C. E., Brooks, I. M., Tjernström, M., Shupe, M. D., Mauritsen, T., Sedlar, J., Lock, A. P., Earnshaw, P., Persson, P. O. G., Milton, S. F., and Leck, C.: Modelling atmospheric structure, cloud and their response to CCN in the central Arctic: ASCOS case studies, Atmos. Chem. Phys., 12, 3419–3435, https://doi.org/10.5194/acp-12-3419-2012, 2012. a
Birmili, W., Stratmann, F., and Wiedensohler, A.: Design of a DMA-based Size Spectrometer for a Large Particle Size Sange and Stable Operation, J. Aerosol Sci., 30, 549–553, https://doi.org/10.1016/S0021-8502(98)00047-0, 1999. a
Brooks, I. M., Tjernström, M., Persson, P. O. G., Shupe, M. D., Atkinson, R. A., Canut, G., Birch, C. E., Mauritsen, T., Sedlar, J., and Brooks, B. J.: The Turbulent Structure of the Arctic Summer Boundary Layer During The Arctic Summer Cloud-Ocean Study, J. Geophys. Res.-Atmos., 122, 9685–9704, https://doi.org/10.1002/2017JD027234, 2017. a, b
Download
Short summary
Aerosol particles are required for cloud droplets to form, and the Arctic atmosphere often has much fewer aerosols than at lower latitudes. In this study, we investigate whether aerosol concentrations can drop so low as to no longer support a cloud. We use observations to initialize idealized model simulations to investigate a worst-case scenario where all aerosol is removed from the environment instantaneously. We find that this mechanism is possible in two cases and is unlikely in the third.
Share
Altmetrics
Final-revised paper
Preprint