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Secondary droplet activation during condensational growth in convective clouds and its detection from satellites
Journal article   Open access   Peer reviewed

Secondary droplet activation during condensational growth in convective clouds and its detection from satellites

Avichay Efraim, Ramon C. Braga, Daniel Rosenfeld, Oliver Lauer, Marco A. Franco, Leslie A. Kremper, Christopher Pöhlker, Meinrat O. Andreae, Cléo Q. Dias-Junior and Mira L. Pöhlker
Atmospheric research, Vol.299, 107196
01/04/2024
DOI: https://doi.org/10.1016/j.atmosres.2023.107196
Appears in  Recent Faculty of Science and Engineering Publications
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Abstract

Clouds Remote sensing Microphysics Aerosols
By acting as cloud condensation nuclei (CCN), aerosol particles play a key role in the climate system. The CCN can be activated into cloud droplets at the cloud base (i.e., primary activation), or above it (i.e., secondary activation). This study shows the conditions required for secondary activation during the condensational growth phase in convective clouds. It also proposes a methodology for detecting this secondary activation from satellites. Using a spectral bin adiabatic parcel model, we simulate the vertical profile of cloud microphysical properties and demonstrate how different aerosol size distributions and updraft velocities greatly affect the secondary activation initiation and the cloud properties. The secondary activation slows down the cloud drop effective radius (re) growth rate with increasing height, and decreasing temperature (T), due to the relatively larger population of smaller droplets in the cloud parcel. Therefore, the vertical profile of re growth with height is slower than the adiabatic rate when the secondary activation occurs. The proposed physical principle was verified by satellite-retrieved T-re profiles and adiabatic cloud drop number concentrations (Nd) over the Amazon region. The results obtained from this study can be utilized to identify the secondary droplet activation during the condensational growth phase, which can lead to an overestimation of the retrieved Nd as well as suppression of warm rain. This improves our knowledge and observational capabilities of the role of aerosol particles in the microphysics, dynamics, and precipitation behavior of convective clouds.

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