Journal of Geophysical Research Atmospheres,
Journal Year:
2016,
Volume and Issue:
121(20)
Published: Oct. 27, 2016
Abstract
Binary
nucleation
of
sulfuric
acid
and
water
as
well
ternary
involving
ammonia
are
thought
to
be
the
dominant
processes
responsible
for
new
particle
formation
(NPF)
in
cold
temperatures
middle
upper
troposphere.
Ions
also
important
these
regions.
However,
global
models
presently
lack
experimentally
measured
NPF
rates
under
controlled
laboratory
conditions
so
at
present
must
rely
on
theoretical
or
empirical
parameterizations.
Here
with
data
obtained
European
Organization
Nuclear
Research
CLOUD
(Cosmics
Leaving
OUtdoor
Droplets)
chamber,
we
first
experimental
survey
spanning
free
tropospheric
conditions.
The
during
cover
a
temperature
range
from
208
298
K,
concentrations
between
5
×
10
1
9
cm
−3
,
mixing
ratios
zero
added
ammonia,
i.e.,
nominally
pure
binary,
maximum
~1400
parts
per
trillion
by
volume
(pptv).
We
performed
studies
neutral
ions
being
chamber
ionization
up
75
ion
pairs
s
−1
study
ion‐induced
nucleation.
found
that
contribution
is
small
248
K
when
several
pptv
higher.
presence
charges
significantly
enhances
rates,
especially
higher
independent
NH
3
levels.
compare
calculated
cluster
Atmospheric
Cluster
Dynamics
Code
evaporation
quantum
chemistry.
Atmospheric chemistry and physics,
Journal Year:
2018,
Volume and Issue:
18(2), P. 921 - 961
Published: Jan. 25, 2018
Abstract.
Airborne
observations
over
the
Amazon
Basin
showed
high
aerosol
particle
concentrations
in
upper
troposphere
(UT)
between
8
and
15
km
altitude,
with
number
densities
(normalized
to
standard
temperature
pressure)
often
exceeding
those
planetary
boundary
layer
(PBL)
by
1
or
2
orders
of
magnitude.
The
measurements
were
made
during
German–Brazilian
cooperative
aircraft
campaign
ACRIDICON–CHUVA,
where
ACRIDICON
stands
for
Aerosol,
Cloud,
Precipitation,
Radiation
Interactions
Dynamics
Convective
Cloud
Systems
CHUVA
is
acronym
Processes
Main
Precipitation
Brazil:
A
Contribution
Resolving
Modeling
GPM
(global
precipitation
measurement),
on
German
High
Altitude
Long
Range
Research
Aircraft
(HALO).
took
place
September–October
2014,
objective
studying
tropical
deep
convective
clouds
rainforest
their
interactions
atmospheric
trace
gases,
particles,
radiation.
Aerosol
enhancements
observed
consistently
all
flights
which
UT
was
probed,
using
several
metrics,
including
condensation
nuclei
(CN)
cloud
(CCN)
chemical
species
mass
concentrations.
particles
differed
sharply
composition
size
distribution
from
PBL,
ruling
out
transport
combustion-derived
(BL)
as
a
source.
air
immediate
outflow
depleted
whereas
strongly
enhanced
small
(<
90
nm
diameter)
found
regions
that
had
experienced
convection
preceding
5–72
h.
We
also
elevated
larger
(>
nm)
UT,
consisted
mostly
organic
matter
nitrate
very
effective
CCN.
Our
findings
suggest
conceptual
model,
production
new
takes
continental
biogenic
volatile
material
brought
up
converted
condensable
UT.
Subsequently,
downward
mixing
tropospheric
can
be
source
they
increase
compound
(BVOC)
oxidation
products.
This
may
an
important
Amazonian
nucleation
formation
have
not
been
observed.
propose
this
dominant
process
supplying
secondary
pristine
atmosphere,
making
control
both
removal
particles.
Atmospheric chemistry and physics,
Journal Year:
2018,
Volume and Issue:
18(19), P. 14737 - 14756
Published: Oct. 12, 2018
Abstract.
Atmospheric
new
particle
formation
(NPF)
is
an
important
phenomenon
in
terms
of
global
number
concentrations.
Here
we
investigated
the
frequency
NPF,
rates
10
nm
particles,
and
growth
size
range
10–25
using
at
least
1
year
aerosol
size-distribution
observations
36
different
locations
around
world.
The
majority
these
measurement
sites
are
Northern
Hemisphere.
We
found
that
NPF
has
a
strong
seasonal
variability.
At
analyzed
this
study,
occurs
most
frequently
March–May
(on
about
30
%
days)
December–February
(about
days).
median
rate
particles
varies
by
3
orders
magnitude
(0.01–10
cm−3
s−1)
order
(1–10
h−1).
smallest
values
both
were
observed
polar
largest
ones
urban
environments
or
anthropogenically
influenced
rural
sites.
correlation
between
event
was
best
moderate
among
sites,
as
well
belonging
to
certain
environmental
regime.
For
better
understanding
atmospheric
its
regional
importance,
would
need
more
observational
data
from
areas
practically
all
parts
world,
additional
remote
North
America,
Asia,
Southern
Hemisphere
(especially
Australia),
areas,
few
over
oceans.
Nature Communications,
Journal Year:
2019,
Volume and Issue:
10(1)
Published: Sept. 25, 2019
Abstract
Over
Boreal
regions,
monoterpenes
emitted
from
the
forest
are
main
precursors
for
secondary
organic
aerosol
(SOA)
formation
and
primary
driver
of
growth
new
particles
to
climatically
important
cloud
condensation
nuclei
(CCN).
Autoxidation
leads
rapid
Highly
Oxygenated
Molecules
(HOM).
We
have
developed
first
model
with
near-explicit
representation
atmospheric
particle
(NPF)
HOM
formation.
The
can
reproduce
observed
NPF,
gas-phase
composition
SOA
over
forest.
During
spring,
increases
CCN
concentration
by
~10
%
causes
a
direct
radiative
forcing
−0.10
W/m
2
.
In
contrast,
NPF
reduces
number
at
updraft
velocities
<
0.2
m/s,
+0.15
Hence,
while
contributes
climate
cooling,
result
in
warming
Environmental Science & Technology,
Journal Year:
2020,
Volume and Issue:
54(14), P. 8547 - 8557
Published: July 1, 2020
Understanding
the
atmospheric
new
particle
formation
(NPF)
process
within
global
range
is
important
for
revealing
budget
of
aerosols
and
their
impacts.
We
investigated
seasonal
characteristics
NPF
in
urban
environment
Beijing.
Aerosol
size
distributions
down
to
∼1
nm
H2SO4
concentration
were
measured
during
2018–2019.
The
observed
rate
1.5
particles
(J1.5)
significantly
higher
than
those
clean
environment,
e.g.,
Hyytiälä,
whereas
growth
not
different.
Both
J1.5
frequency
Beijing
show
a
clear
variation
with
maxima
winter
minima
summer,
while
rates
are
generally
same
around
year.
that
ambient
temperature
governing
factor
driving
J1.5.
In
contrast,
condensation
sink
daily
maximum
no
significant
periods.
all
four
seasons,
(H2SO4)n(amine)n
clusters
contributes
sub-3
range,
it
less
above
3
nm.
Therefore,
other
species
always
needed
larger
particles.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(1), P. 115 - 138
Published: Jan. 4, 2019
Abstract.
New
particle
formation
(NPF)
studies
in
China
were
summarized
comprehensively
this
paper.
NPF
frequency,
rate,
and
growth
rate
closely
compared
among
the
observations
carried
out
at
different
types
of
sites
regions
seasons,
with
aim
exploring
nucleation
mechanisms.
The
interactions
between
air
pollution
are
discussed,
emphasizing
properties
under
heavy
conditions.
current
understanding
cannot
fully
explain
frequent
occurrence
high
aerosol
loadings
China,
possible
reasons
for
phenomenon
proposed.
effects
some
aspects
research
requiring
further
investigation
also
Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(7)
Published: March 22, 2021
Abstract
Intense
and
frequent
new
particle
formation
(NPF)
events
have
been
observed
in
polluted
urban
environments,
yet
the
dominant
mechanisms
are
still
under
debate.
To
understand
key
species
governing
processes
of
NPF
we
conducted
comprehensive
measurements
downtown
Beijing
during
January–March,
2018.
We
performed
detailed
analyses
on
sulfuric
acid
cluster
composition
budget,
as
well
chemical
physical
properties
oxidized
organic
molecules
(OOMs).
Our
results
demonstrate
that
fast
clustering
(H
2
SO
4
)
base
triggered
events,
OOMs
further
helped
grow
newly
formed
particles
toward
climate‐
health‐relevant
sizes.
This
synergistic
role
H
,
species,
is
likely
representative
environments
where
abundant
usually
co‐exist,
with
moderately
low
volatility
when
produced
high
NO
x
concentrations.
Proceedings of the National Academy of Sciences,
Journal Year:
2020,
Volume and Issue:
117(32), P. 18998 - 19006
Published: July 27, 2020
Significance
Enhancement
of
aerosol
that
can
nucleate
cloud
droplets
increases
the
droplet
number
concentration
and
albedo
clouds.
This
amount
sunlight
reflected
to
space.
Uncertainty
in
how
aerosol−cloud
interactions
over
industrial
period
have
increased
planetary
by
this
mechanism
leads
significant
uncertainty
climate
projections.
Our
work
presents
a
method
for
observationally
constraining
change
due
anthropogenic
emissions:
hemispheric
difference
remotely
sensed
between
pristine
Southern
Ocean
(a
preindustrial
proxy)
polluted
Northern
Hemisphere.
Application
constraint
models
reduces
range
estimated
since
industrialization
suggests
current
underpredict
era.
Atmospheric chemistry and physics,
Journal Year:
2021,
Volume and Issue:
21(4), P. 2457 - 2468
Published: Feb. 18, 2021
Abstract.
New
particle
formation
(NPF)
is
one
of
the
major
sources
atmospheric
ultrafine
particles.
Due
to
high
aerosol
and
trace
gas
concentrations,
mechanism
governing
factors
for
NPF
in
polluted
boundary
layer
may
be
quite
different
from
those
clean
environments,
which
however
less
understood.
Herein,
based
on
long-term
measurements
January
2018
March
2019
Beijing,
nucleation
influences
H2SO4
concentration,
amine
concentration
are
quantified.
The
collision
H2SO4–amine
clusters
found
dominating
initialize
urban
Beijing.
coagulation
scavenging
due
a
factor
as
it
limits
new
rates.
Beijing
sometimes
limited
by
low
concentrations.
Summarizing
synergistic
effects
we
elucidate
various
conditions.