@Article{SchulzSHACSDFJKKMMPSVWZZAAMPWB:2018:AiObIs,
author = "Schulz, Christiane and Schneider, Johannes and Holanda, Bruna
Amorim and Appel, Oliver and Costa, Anja and S{\'a}, Suzane S. de
and Dreiling, Volker and F{\"u}tterer, Daniel and
Jurkat-Witschas, Tina and Klimach, Thomas and Kr{\"a}mer, Martina
and Martin, Scot T. and Mertes, Stephan and P{\"o}hlker, Mira L.
and Sauer, Daniel and Voigt, Christiane and Weinzierl, Bernadett
and Ziereis, Helmut and Z{\"o}ger, Martin and Andreae, Meinrat O.
and Artaxo, Paulo and Machado, Luiz Augusto Toledo and
P{\"o}schl, Ulrich and Wendisch, Manfred and Borrmann, Stephan",
affiliation = "{Max Planck Institute for Chemistry} and {Max Planck Institute for
Chemistry} and {Max Planck Institute for Chemistry} and {Max
Planck Institute for Chemistry} and {Institut f{\"u}r Energie-
und Klimaforschung (IEK7)} and {Harvard University} and {German
Aerospace Center (Deutsches Zentrum f{\"u}r Luft- und Raumfahrt)}
and {German Aerospace Center (Deutsches Zentrum f{\"u}r Luft- und
Raumfahrt)} and {German Aerospace Center (Deutsches Zentrum
f{\"u}r Luft- und Raumfahrt)} and {Max Planck Institute for
Chemistry} and {Institut f{\"u}r Energie- und Klimaforschung
(IEK7)} and {Harvard University} and {Leibniz Institute for
Tropospheric Research} and {Max Planck Institute for Chemistry}
and {German Aerospace Center (Deutsches Zentrum f{\"u}r Luft- und
Raumfahrt)} and {German Aerospace Center (Deutsches Zentrum
f{\"u}r Luft- und Raumfahrt)} and {German Aerospace Center
(Deutsches Zentrum f{\"u}r Luft- und Raumfahrt)} and {German
Aerospace Center (Deutsches Zentrum f{\"u}r Luft- und Raumfahrt)}
and {German Aerospace Center (Deutsches Zentrum f{\"u}r Luft- und
Raumfahrt)} and {Max Planck Institute for Chemistry} and
{Universidade de S{\~a}o Paulo (USP)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Max Planck Institute for
Chemistry} and {University of Leipzig} and {Max Planck Institute
for Chemistry}",
title = "Aircraft-based observations of isoprene epoxydiol-derived
secondary organic aerosol (IEPOX-SOA) in the tropical upper
troposphere over the Amazon region",
journal = "Atmospheric Chemistry and Physics Discussion",
year = "2018",
volume = "2018",
number = "232",
abstract = "During the ACRIDICON-CHUVA field project (SeptemberOctober 2014;
based in Manaus, Brazil) aircraft-based in-situ measurements of
aerosol chemical composition were conducted in the tropical
troposphere over the Amazon using the High Altitude and Long Range
Research Aircraft (HALO), covering altitudes from the boundary
layer height up to 14.4\ km. The submicron non-refractory
aerosol was characterized by flash-vaporization/electron
impact-ionization aerosol particle mass spectrometry. The results
show that significant secondary organic aerosol (SOA) formation by
isoprene oxidation products occurs in the upper troposphere,
leading to increased organic aerosol mass concentrations above
10\ km altitude. The median organic mass concentrations in
the upper troposphere above 10\ km range between 1.0 and
2.1\ \μg\ m\−3 (referring to standard
temperature and pressure; STP) with interquartile ranges of 0.6 to
3.0\ \μg\ m\−3 (STP), representing
70\ % of the total submicron non-refractory aerosol
particle mass. The presence of isoprene epoxydiol-derived isoprene
secondary organic aerosol (IEPOX-SOA) was confirmed by marker
peaks in the mass spectra. We estimate the contribution of
IEPOX-SOA to the total organic aerosol in the upper troposphere to
be about 20\ %. After isoprene emission from vegetation,
oxidation processes occur at low altitudes and/or during transport
to higher altitudes, which may lead to the formation of IEPOX (one
oxidation product of isoprene). Reactive uptake or condensation of
IEPOX on pre-existing particles leads to IEPOX-SOA formation and
subsequently increasing organic mass in the upper troposphere.
This organic mass increase was accompanied by an increase of the
nitrate mass concentrations, most likely due to NOx production by
lightning. We further found that the ammonium contained in the
aerosol particles is not sufficient to neutralize the particulate
sulfate and nitrate. Analysis of the ion ratio of NO+ to NO2+
indicated that nitrate in the upper troposphere exists mainly in
the form of organic nitrate. IEPOX-SOA and organic nitrates are
coincident with each other, indicating that IEPOX-SOA forms in the
upper troposphere either on acidic nitrate particles forming
organic nitrates derived from IEPOX or on already neutralized
organic nitrate aerosol particles.",
doi = "10.5194/acp-2018-232",
url = "http://dx.doi.org/10.5194/acp-2018-232",
issn = "1680-7367",
language = "en",
targetfile = "schulz_aircraft.pdf",
urlaccessdate = "25 abr. 2024"
}