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@ARTICLE{Rosati:811715,
author = {Rosati, Bernadette and Gysel, Martin and Rubach, Florian
and Mentel, Thomas F. and Goger, Brigitta and Poulain,
Laurent and Schlag, Patrick and Miettinen, Pasi and
Pajunoja, Aki and Virtanen, Annele and Klein Baltink, Henk
and Henzing, J. S. Bas and Größ, Johannes and Gobbi, Gian
Paolo and Wiedensohler, Alfred and Kiendler-Scharr, Astrid
and Decesari, Stefano and Facchini, Maria Cristina and
Weingartner, Ernest and Baltensperger, Urs},
title = {{V}ertical profiling of aerosol hygroscopic properties in
the planetary boundary layer during the {PEGASOS} campaigns},
journal = {Atmospheric chemistry and physics},
volume = {16},
number = {11},
issn = {1680-7324},
address = {Katlenburg-Lindau},
publisher = {EGU},
reportid = {FZJ-2016-04099},
pages = {7295 - 7315},
year = {2016},
abstract = {Vertical profiles of the aerosol particles hygroscopic
properties, their mixing state as well as chemical
composition were measured above northern Italy and the
Netherlands. An aerosol mass spectrometer (AMS; for chemical
composition) and a white-light humidified optical particle
spectrometer (WHOPS; for hygroscopic growth) were deployed
on a Zeppelin NT airship within the PEGASOS project. This
allowed one to investigate the development of the different
layers within the planetary boundary layer (PBL), providing
a unique in situ data set for airborne aerosol particles
properties in the first kilometre of the atmosphere.
Profiles measured during the morning hours on 20 June 2012
in the Po Valley, Italy, showed an increased nitrate
fraction at ∼ 100 m above ground level (a.g.l.)
coupled with enhanced hygroscopic growth compared to
∼ 700 m a. g. l. This result was derived
from both measurements of the aerosol composition and direct
measurements of the hygroscopicity, yielding hygroscopicity
parameters (κ) of 0.34 ± 0.12 and
0.19 ± 0.07 for 500 nm particles, at
∼ 100 and ∼ 700 m a. g. l.,
respectively. The difference is attributed to the structure
of the PBL at this time of day which featured several
independent sub-layers with different types of aerosols.
Later in the day the vertical structures disappeared due to
the mixing of the layers and similar aerosol particle
properties were found at all probed altitudes (mean
κ ≈ 0.18 ± 0.07). The aerosol properties
observed at the lowest flight level (100 m a. g. l.)
were consistent with parallel measurements at a ground site,
both in the morning and afternoon. Overall, the aerosol
particles were found to be externally mixed, with a
prevailing hygroscopic fraction. The flights near Cabauw in
the Netherlands in the fully mixed PBL did not feature
altitude-dependent characteristics. Particles were also
externally mixed and had an even larger hygroscopic fraction
compared to the results in Italy. The mean κ from direct
measurements was 0.28 ± 0.10, thus considerably
higher than κ values measured in Italy in the fully mixed
PBL.},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {243 - Tropospheric trace substances and their
transformation processes (POF3-243)},
pid = {G:(DE-HGF)POF3-243},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000378354600037},
doi = {10.5194/acp-16-7295-2016},
url = {https://juser.fz-juelich.de/record/811715},
}