EGU2020-2630
https://doi.org/10.5194/egusphere-egu2020-2630
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Time evolution of activated aerosol particles in low clouds

Naděžda Zíková1, Petra Pokorná1, Petr Pešice2, Pavel Sedlák2, and Vladimír Ždímal1
Naděžda Zíková et al.
  • 1Institute of Chemical Process Fundamentals, Department of Aerosol Chemistry and Physics, Prague, Czechia (zikova@icpf.cas.cz)
  • 2Institute of Atmospheric Physics, Department of Meteorology, Czech Academy of Sciences, Prague, Czechia

Atmospheric aerosol (AA) influences cloud formation, lifetime and other properties; the processes between AA and clouds are source of uncertainty in weather and climate changes estimations [1]. Apart from airborne measurements, the processes in clouds can be also studied on fogs, or low clouds present at a station with high frequency of fog occurrence, such as at Milešovka, Czech Republic, where fog is present for almost 55 % of the time [2]. At the observatory located on the top of the mountain, with a professional meteorological station and measurements of fog/cloud characterization and vertical cloud profile, an additional measurement of aerosol particle number size distributions (PNSD) was done. PNSD from 10 nm to 20 µm was conducted using SMPS and APS spectrometers, measuring activated and interstitial particles. From the activated PNSD (aPNSD), the activated fraction (AF) was estimated [3] i.e. size dependent share of activated particles from all available ones. The AF was fitted with Sigmoidal function and the inflection point, D50, a lower estimate for an activation diameter of fog [4], was calculated.

The changes in the aPNSD at the beginning of each fog episode have been studied. The largest changes in aPNSD and AF were found within the first two or three hours of the fog episode durations. During the episode, the D50 shifted to the smaller particles, and the AF became steeper. For most episodes, 120 minutes after their beginning the size-dependent AF reached a steady-state. The exceptions  were observed during fog episodes preceded by another hydrometeor-related episode. Under such circumstances, the shift in the AF was not observed, as the steady state had been already reached during the preceding episode.

If the time evolution during whole episodes is taken into account, two main groups of AF behavior in time were also found, based on the meteorological situation prior episode beginning. For one group, there is a strong decrease in the D50 in the first three hours, and later the D50 reaches almost a constant value. The steady value is of about 200 nm for all the episodes, independently of the time of the fog occurrence (time of day, season). In the second group, part of a long-term hydrometeor-related situations, the decrease at the beginning of the episode is not visible and the D50 only fluctuates around its original value. Depending on the air mass origin, it is either 90 or 200 nm.

This work was supported by the Czech Science Foundation under grant P209/18/15065Y.

[1]           IPCC, 2013. Cambridge Univ. Press, Cambridge, UK, and New York, 2013.

[2]           J. Fišák et al., Soil Water Res., vol. 196, pp. 273–285, 2009.

[3]           E. Asmi et al., Atmos. Chem. Phys., vol. 12, no. 23, pp. 11589–11607, 2012.

[4]           E. Hammer et al., Atmos. Chem. Phys., vol. 14, no. 19, pp. 10517–10533, 2014.

How to cite: Zíková, N., Pokorná, P., Pešice, P., Sedlák, P., and Ždímal, V.: Time evolution of activated aerosol particles in low clouds, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2630, https://doi.org/10.5194/egusphere-egu2020-2630, 2020

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