Atmospheric chemistry and physics,
Journal Year:
2016,
Volume and Issue:
16(14), P. 8715 - 8728
Published: July 18, 2016
Abstract.
Secondary
aerosol
particle
production
via
new
formation
(NPF)
has
been
shown
to
be
a
major
contributor
the
global
load.
NPF
also
observed
frequently
in
urban
environments.
Here,
we
investigate
effect
of
regional
on
load
under
well-defined
atmospheric
conditions.
The
Carpathian
Basin,
largest
orogenic
basin
Europe,
represents
an
excellent
opportunity
for
exploring
these
interactions.
Based
long-term
observations,
revealed
that
seen
central
large
city
(Budapest)
and
its
background
occur
consistent
spatially
coherent
way
as
result
joint
phenomenon
taking
place
horizontal
scales.
We
found
events
at
site
are
usually
delayed
by
>
1
h
relative
rural
or
even
inhibited
above
critical
condensational
sink
level.
processes
require
higher
rates
growth
realized,
mean
factors
2
1.6,
respectively,
than
events.
Regional-
urban-type
sometimes
jointly
with
multiple
onsets,
while
they
often
exhibit
dynamic
timing
properties
which
different
two
event
types.
Atmospheric chemistry and physics,
Journal Year:
2015,
Volume and Issue:
15(14), P. 8217 - 8299
Published: July 24, 2015
Abstract.
The
literature
on
atmospheric
particulate
matter
(PM),
or
aerosol,
has
increased
enormously
over
the
last
2
decades
and
amounts
now
to
some
1500–2000
papers
per
year
in
refereed
literature.
This
is
part
due
enormous
advances
measurement
technologies,
which
have
allowed
for
an
increasingly
accurate
understanding
of
chemical
composition
physical
properties
particles
their
processes
atmosphere.
growing
scientific
interest
aerosol
high
importance
environmental
policy.
In
fact,
constitutes
one
most
challenging
problems
both
air
quality
climate
change
policies.
this
context,
paper
reviews
recent
results
within
sciences
policy
needs,
driven
much
increase
monitoring
mechanistic
research
decades.
synthesis
reveals
many
new
developments
science
underpinning
climate–aerosol
interactions
effects
PM
human
health
environment.
However,
while
airborne
responsible
globally
important
influences
premature
mortality,
we
still
do
not
know
relative
different
components
these
effects.
Likewise,
magnitude
overall
remains
highly
uncertain.
Despite
uncertainty
there
are
things
that
could
be
done
mitigate
local
global
PM.
Recent
analyses
shown
reducing
black
carbon
(BC)
emissions,
using
known
control
measures,
would
reduce
warming
delay
time
when
anthropogenic
temperature
exceed
°C.
cost-effective
measures
ammonia,
agricultural
precursor
gas
secondary
inorganic
aerosols
(SIA),
regional
eutrophication
concentrations
large
areas
Europe,
China
USA.
Thus,
environment
population.
A
prioritized
list
actions
full
range
currently
undeliverable
shortcomings
knowledge
science;
among
shortcomings,
roles
sources
response
land
use
remaining
century
prominent.
any
case,
evidence
from
strongly
advocates
integrated
approach
Environmental Research Letters,
Journal Year:
2018,
Volume and Issue:
13(10), P. 103003 - 103003
Published: Sept. 6, 2018
This
review
focuses
on
the
observed
characteristics
of
atmospheric
new
particle
formation
(NPF)
in
different
environments
global
troposphere.
After
a
short
introduction,
we
will
present
theoretical
background
that
discusses
methods
used
to
analyze
measurement
data
NPF
and
associated
terminology.
We
update
our
current
understanding
regional
NPF,
i.e.
taking
simultaneously
place
over
large
spatial
scales,
complement
with
full
reported
growth
rates
during
events.
shortly
at
sub-regional
scales.
Since
newly-formed
particles
into
larger
sizes
is
great
interest,
briefly
discuss
observation-based
which
gaseous
compounds
contribute
particles,
what
implications
this
have
cloud
condensation
nuclei
formation.
finish
summary
main
findings
future
outlook
outlines
remaining
research
questions
needs
for
additional
measurements.
Proceedings of the National Academy of Sciences,
Journal Year:
2015,
Volume and Issue:
112(23), P. 7123 - 7128
Published: May 26, 2015
Significance
Extremely
low
volatility
organic
compounds
(ELVOC)
are
suggested
to
promote
aerosol
particle
formation
and
cloud
condensation
nuclei
(CCN)
production
in
the
atmosphere.
We
show
that
capability
of
biogenic
VOC
(BVOC)
produce
ELVOC
depends
strongly
on
their
chemical
structure
relative
oxidant
levels.
BVOC
with
an
endocyclic
double
bond,
representative
emissions
from,
e.g.,
boreal
forests,
efficiently
from
ozonolysis.
Compounds
exocyclic
bonds
or
acyclic
including
isoprene,
emission
tropics,
minor
quantities
ELVOC,
role
OH
radical
oxidation
is
relatively
larger.
Implementing
these
findings
into
a
global
modeling
framework
shows
detailed
assessment
pathways
crucial
for
understanding
secondary
atmospheric
CCN
formation.
Annual Review of Physical Chemistry,
Journal Year:
2013,
Volume and Issue:
65(1), P. 21 - 37
Published: Nov. 18, 2013
The
recent
development
in
measurement
techniques
and
theoretical
understanding
has
enabled
us
to
study
atmospheric
vapor,
cluster
nanoparticle
concentrations,
dynamics,
their
connection
nucleation.
Here
we
present
a
summary
of
the
chemistry
clustering,
growing
nanoparticles,
precursors.
In
this
work,
focus
particularly
on
gas-to-particle
conversion
progress
its
understanding.
The Journal of Chemical Physics,
Journal Year:
2013,
Volume and Issue:
139(8)
Published: Aug. 28, 2013
The
first
step
in
atmospheric
new
particle
formation
involves
the
aggregation
of
gas
phase
molecules
into
small
molecular
clusters
that
can
grow
by
colliding
with
and
each
other.
In
this
work
we
used
principles
quantum
chemistry
combined
a
dynamic
model
to
study
steady-state
kinetics
sets
consisting
sulfuric
acid
ammonia
or
dimethylamine
molecules.
Both
were
studied
without
electrically
charged
clusters.
We
show
main
clustering
pathways
simulated
systems
together
chemical
Gibbs
free
energies
growing
acid–ammonia
system,
major
growth
exhibit
energy
barriers,
whereas
acid–dimethylamine
system
occurs
mainly
via
barrierless
condensation.
When
ions
are
present,
contribute
significantly
system.
For
role
is
minor,
except
at
very
low
concentration,
neutral.
Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
48(4)
Published: Dec. 29, 2020
Abstract
New
particle
formation
in
the
Arctic
atmosphere
is
an
important
source
of
aerosol
particles.
Understanding
processes
secondary
crucial
due
to
their
significant
impact
on
cloud
properties
and
therefore
amplification.
We
observed
molecular
new
particles
from
low‐volatility
vapors
at
two
sites
with
differing
surroundings.
In
Svalbard,
sulfuric
acid
(SA)
methane
sulfonic
(MSA)
contribute
some
extent
condensation
nuclei
(CCN).
This
occurs
via
ion‐induced
nucleation
SA
NH
3
subsequent
growth
by
mainly
MSA
during
springtime
highly
oxygenated
organic
molecules
summertime.
By
contrast,
ice‐covered
region
around
Villum,
we
driven
iodic
but
its
concentration
was
insufficient
grow
nucleated
CCN
sizes.
Our
results
provide
insight
about
sources
precursors
Geophysical Research Letters,
Journal Year:
2014,
Volume and Issue:
41(7), P. 2644 - 2651
Published: March 22, 2014
Primary
and
secondary
aerosol
particles
originating
from
biomass
burning
contribute
significantly
to
the
atmospheric
budget
thereby
both
direct
indirect
radiative
forcing.
Based
on
detailed
measurements
of
a
large
number
plumes
variable
age
in
southern
Africa,
we
show
that
size
distribution,
chemical
composition,
single-scattering
albedo,
hygroscopicity
change
considerably
during
first
2–4
h
their
transport.
These
changes,
driven
by
oxidation
subsequent
formation,
may
reach
factor
6
for
scattering
coefficient
>10
cloud
condensation
nuclei
concentration.
Since
observed
changes
take
place
over
spatial
temporal
scales
are
neither
covered
emission
inventories
nor
captured
large-scale
model
simulations,
findings
reported
here
point
out
significant
gap
our
understanding
climatic
effects
aerosols.
Nature Communications,
Journal Year:
2019,
Volume and Issue:
10(1)
Published: Sept. 30, 2019
Abstract
Particles
formed
in
the
atmosphere
via
nucleation
provide
about
half
number
of
atmospheric
cloud
condensation
nuclei,
but
many
locations,
this
process
is
limited
by
growth
newly
particles.
That
often
organic
vapors.
Identification
these
vapors
and
their
sources
thus
fundamental
for
simulating
changes
to
aerosol-cloud
interactions,
which
are
one
most
uncertain
aspects
anthropogenic
climate
forcing.
Here
we
present
direct
molecular-level
observations
a
distribution
forested
environment
that
can
explain
simultaneously
observed
nanoparticle
from
3
50
nm.
Furthermore,
volatility
sufficient
without
invoking
particle-phase
processes.
The
agreement
between
mass
growth,
predicted
condensing
represents
an
important
step
forward
characterization
particle
growth.
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.