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- W3180317967 abstract "<p>Aerosol effects on clouds&#8217;&#160;microphysics and dynamics are still considered as an important open question that contributes a major uncertainty to climate research and prediction. Using 7 years of observational and reanalysis data, we show a non-monotonic trend in convective cloud properties and rain intensity as a function of aerosol optical depth&#160;(AOD). The invigoration effect shifts into weak suppression beyond an optimal AOD ( of ~ 0.3-0.4). Using a cloud model we explain this shift in trend as the result of a competition between two types of microphysical processes: cloud-core-based invigorating processes vs. peripheral suppressive processes. We show that the optimal AOD, for which cloud and rain reach their maximal values, depends on the environmental thermodynamic conditions&#160;and it is higher for more unstable or more humid conditions. Our findings improve the&#160;understanding of aerosol-cloud interaction and their link to environmental conditions. It can aid in the improvement of&#160;parameterizations of clouds in climate models.</p>" @default.
- W3180317967 created "2021-07-19" @default.
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- W3180317967 date "2021-03-03" @default.
- W3180317967 modified "2023-09-23" @default.
- W3180317967 title "Non-Monotonic Aerosol Effect on Precipitation over the ITCZ" @default.
- W3180317967 doi "https://doi.org/10.5194/egusphere-egu21-3892" @default.
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