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Title: Long-term observations of cloud condensation nuclei in the Amazon rain forest - Part 1: Aerosol size distribution, hygroscopicity, and new model parametrizations for CCN prediction
Authors: Pöhlker, Mira L.
Pöhlker, Christopher
Ditas, Florian
Klimach, Thomas
Angelis, Isabella Hrabe de
Araüjo, Alessandro Carioca de
Brito, Joel F.
Carbone, Samara
Cheng, Yafang
Chi, Xuguang
Ditz, Reiner
Gunthe, Sachin S.
Kesselmeier, Jürgen
Könemann, Tobias
Lavric, J. V.
Martin, Scot T.
Mikhailov, Eugene F.
Morán-Zuloaga, Daniel
Rose, Diana
Saturno, Jorge
Su, Hang
Thalman, Ryan M.
Walter, David
Wang, Jian
Wolff, Stefan
Barbosa, H. M. J.
Artaxo, Paulo
Andreae, Meinrat O.
Pöschl, Ulrich
Keywords: Aerosol
Atmospheric Modeling
Chemical Composition
Cloud Condensation Nucleus
Observational Method
Size Distribution
Amazon Basin
Issue Date: 2016
metadata.dc.publisher.journal: Atmospheric Chemistry and Physics
metadata.dc.relation.ispartof: Volume 16, Número 24, Pags. 15709-15740
Abstract: Size-resolved long-term measurements of atmospheric aerosol and cloud condensation nuclei (CCN) concentrations and hygroscopicity were conducted at the remote Amazon Tall Tower Observatory (ATTO) in the central Amazon Basin over a 1-year period and full seasonal cycle (March 2014-February 2015). The measurements provide a climatology of CCN properties characteristic of a remote central Amazonian rain forest site. The CCN measurements were continuously cycled through 10 levels of supersaturation (S = 0.11 to 1.10%) and span the aerosol particle size range from 20 to 245nm. The mean critical diameters of CCN activation range from 43nm at S = 1.10 % to 172nm at S = 0.11%. The particle hygroscopicity exhibits a pronounced size dependence with lower values for the Aitken mode (κAit = 0.14 ± 0.03), higher values for the accumulation mode (κAcc = 0.22 ± 0.05), and an overall mean value of κmean = 0.17 ± 0.06, consistent with high fractions of organic aerosol. The hygroscopicity parameter, κ, exhibits remarkably little temporal variability: no pronounced diurnal cycles, only weak seasonal trends, and few short-term variations during long-range transport events. In contrast, the CCN number concentrations exhibit a pronounced seasonal cycle, tracking the pollution-related seasonality in total aerosol concentration. We find that the variability in the CCN concentrations in the central Amazon is mostly driven by aerosol particle number concentration and size distribution, while variations in aerosol hygroscopicity and chemical composition matter only during a few episodes. For modeling purposes, we compare different approaches of predicting CCN number concentration and present a novel parametrization, which allows accurate CCN predictions based on a small set of input data. © The Author(s) 2016.
metadata.dc.identifier.doi: 10.5194/acp-16-15709-2016
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