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- W2556149643 abstract "Narrowing down uncertainties in aerosol indirect effect estimates requires improvements in understanding of cloudaerosol interactions, which involve many different processes. Cloud related vertical motions can transport aerosols from the boundary layer to higher altitudes. Microphysical interactions involve processes that change physical and chemical properties of aerosol particles and cloud droplets, including nucleation scavenging, collision-coalescence, and aqueous chemistry. Evaluating relative contributions of these processes using insitu measurements is difficult because of sampling issues. Remote sensing can provide a more representative sampling and a number of recent studies reported positive correlations between retrieved cloud fraction and aerosol optical depth (AOD) in neighboring cloud-free regions. Possible physical mechanisms that might lead to higher AOD in the vicinity of clouds include growth of aerosol particle size due to water uptake in near cloud regions of enhanced humidity (or cloud halos) and increase in aerosol concentration due to either clouddriven transport of particles from other layers or production of new particles in cloud outflows. Alternatively, these findings could be largely a result of cloud-aerosol radiative interactions when areas around clouds are brightened by the sunlight scattered by cloud particles. This cloudinduced enhancement of reflectance then leads to a high bias in the AOD retrieved using a plane-parallel approximation. This study is aimed at unraveling roles of various processes in these complex interactions through closer integration of modeling and observational approaches. 2. APPROACH" @default.
- W2556149643 created "2016-11-30" @default.
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- W2556149643 date "2007-01-01" @default.
- W2556149643 modified "2023-09-27" @default.
- W2556149643 title "DYNAMICAL, MICROPHYSICAL, AND RADIATIVE INTERACTIONS BETWEEN AEROSOLS AND CUMULUS CLOUDS" @default.
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