ACS Earth and Space Chemistry,
Journal Year:
2021,
Volume and Issue:
5(11), P. 3268 - 3278
Published: Nov. 4, 2021
Information
on
the
diffusion
rates
of
organic
molecules
within
secondary
aerosol
(SOA)
and
biomass
burning
(BBOA)
is
needed
to
predict
impact
these
aerosols
atmospheric
chemistry,
air
quality,
climate.
Nevertheless,
no
studies
have
measured
organics
SOA
generated
from
β-caryophyllene
or
BBOA.
Here,
we
in
laboratory-generated
BBOA
as
a
function
water
activity
(aw)
using
fluorescence
recovery
after
photobleaching.
The
was
by
ozonolysis
β-caryophyllene,
pyrolysis
pine
wood.
Only
water-soluble
component
studied.
coefficients
range
1.1
×
10–16
1.3
10–14
m2
s–1
for
aw
values
ranging
0.23
0.86.
For
BBOA,
7.3
10–17
6.6
0.43.
Based
values,
mixing
times
200
nm
are
less
than
1
min
>0.23.
Since
often
greater
planetary
boundary
layer
temperatures
5
K
our
experimental
temperatures,
likely
short
that
part
atmosphere
types
studied
here.
SOA,
compared
with
predictions
based
Stokes–Einstein
relation
fractional
relation.
both
relations,
agree
predicted
coefficients.
This
work
illustrates
when
radius
diffusing
average
matrix
molecules,
equation
able
reasonable
accuracy.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(10), P. 6275 - 6304
Published: May 29, 2024
Abstract.
Brown
carbon
(BrC)
is
an
absorbing
organic
aerosol
(OA),
primarily
emitted
through
biomass
burning
(BB),
which
exhibits
light
absorption
unique
to
both
black
(BC)
and
other
aerosols.
Despite
many
field
laboratory
studies
seeking
constrain
BrC
properties,
the
radiative
forcing
(RF)
of
still
highly
uncertain.
To
better
understand
its
climate
impact,
we
introduced
One-Moment
Aerosol
(OMA)
module
GISS
ModelE
Earth
system
model
(ESM).
We
assessed
sensitivity
primary
processed
a
novel
chemical
aging
scheme
secondary
formed
from
biogenic
volatile
compounds
(BVOCs).
Initial
results
show
that
typically
contributes
top-of-the-atmosphere
(TOA)
effect
0.04
W
m−2.
Sensitivity
tests
indicate
explicitly
simulating
(separating
it
OAs),
including
BrC,
bleaching
contribute
distinguishable
effects
should
be
accounted
for
in
schemes.
This
addition
prognostic
allows
greater
physical
complexity
OA
representation
with
no
apparent
trade-off
performance,
as
evaluation
optical
depth
against
Robotic
Network
(AERONET)
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS)
retrieval
data,
without
scheme,
reveals
similar
skill
cases.
Thus,
simulated
allow
more
physically
based
composition,
crucial
detailed
like
comparisons
situ
measurement
campaigns.
include
summary
best
practices
within
at
end
this
paper.
npj Climate and Atmospheric Science,
Journal Year:
2024,
Volume and Issue:
7(1)
Published: June 12, 2024
Abstract
This
study
investigates
long-term
changes
in
the
shortwave
direct
aerosol
radiative
effect
(DARE)
at
top
of
atmosphere
(TOA)
induced
by
biomass
burning
(BBA)
transported
from
southern
Africa
to
south-eastern
Atlantic
(SEA)
stratocumulus
region
during
extended
fire
seasons.
The
evolution
since
2002
aerosol,
cloud
properties,
and
TOA
outgoing
radiation
advanced
passive
satellite
sensors
are
presented,
as
well
observational
trend
clear-sky
DARE
clr
retrieval
all-sky
all
.
Supplemented
chemical
transport
model
simulations,
we
estimate
that
has
become
more
negative
(−0.09
±
0.06
W
m
−2
yr
−1
)
due
increased
presence
SEA.
Meanwhile,
positive
(
+
0.04
0.15
aerosols
cloudy
sky
regions.
reveals
capabilities
capturing
complex
BBA-cloud-solar
interactions
for
accurate
forcing
estimates
projections.
Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(33), P. 14753 - 14763
Published: July 10, 2024
The
global
increase
in
wildfires,
primarily
driven
by
climate
change,
significantly
affects
air
quality
and
health.
Wildfire-emitted
particulate
matter
(WFPM)
is
linked
to
adverse
health
effects,
yet
the
toxicological
mechanisms
are
not
fully
understood
given
its
physicochemical
complexity
lack
of
spatiotemporal
exposure
data.
This
study
focuses
on
characterization
WFPM
from
a
Canadian
wildfire
June
2023,
which
affected
over
100
million
people
US
Northeast,
particularly
around
New
Jersey/New
York.
Aerosol
systems
were
deployed
characterize
during
3
day
event,
revealing
unprecedented
mass
concentrations
mainly
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(4), P. 2087 - 2121
Published: Feb. 19, 2025
Abstract.
The
Aerosol
Cloud
meTeorology
Interactions
oVer
the
western
ATlantic
Experiment
(ACTIVATE)
is
a
NASA
mission
to
characterize
aerosol–cloud
interactions
over
North
Atlantic
Ocean
(WNAO).
Such
characterization
requires
understanding
of
life
cycle,
composition,
transport
pathways,
and
distribution
aerosols
WNAO.
This
study
uses
GEOS-Chem
model
simulate
aerosol
distributions
properties
that
are
evaluated
against
aircraft,
ground-based,
satellite
observations
during
winter
summer
field
deployments
in
2020
ACTIVATE.
Transport
boundary
layer
(BL)
behind
cold
fronts
was
major
mechanism
for
American
continental
outflow
pollution
WNAO
winter.
Turbulent
mixing
main
driver
upward
sea
salt
within
ventilation
out
BL
composition
dominated
by
salt,
which
increased
summer,
followed
organics
sulfate.
Aircraft
situ
measurements
provided
useful
constraints
on
wet
scavenging
GEOS-Chem.
generally
captured
observed
features
such
as
outflow,
land–ocean
gradient,
anthropogenic
with
salt.
Model
sensitivity
experiments
elevated
smoke
injection
heights
mid-troposphere
(versus
BL)
better
reproduced
from
US
wildfires
summer.
analysis
suggests
strong
hygroscopic
growth
particles
their
seeding
marine
clouds
(<
35°
N).
Future
modeling
efforts
should
focus
improving
parameterizations
scavenging,
implementing
realistic
heights,
applying
high-resolution
models
resolve
vertical
transport.
Wildfire
particulate
matter
from
Canadian
forest
fires
significantly
impacted
the
air
quality
in
northeastern
United
States
during
summer
of
2023.
Here,
we
used
real-time
and
time-integrated
instrumentation
to
characterize
physicochemical
properties
radiative
effects
wildfire
reaching
metropolitan
areas
New
Jersey/
York
this
extreme
incident.
The
forcing
-352.4
W/m2
derived
here
based
on
measured
optical
explains,
some
extent,
ground
level
temperature
reduction
about
3
°C
observed
City
Such
negative
densely
populated
megacities
may
limit
natural
ventilation,
increase
residence
time
background
pollutants,
exacerbating
public
health
risks.
This
study
highlights
importance
their
potential
implications
for
climate,
health.
The Journal of Physical Chemistry A,
Journal Year:
2022,
Volume and Issue:
126(17), P. 2619 - 2631
Published: April 25, 2022
New
approaches
for
the
sensitive
and
accurate
quantification
of
aerosol
optical
properties
are
needed
to
improve
current
understanding
unique
physical
chemistry
airborne
particles
explore
their
roles
in
fields
as
diverse
chemical
manufacturing,
healthcare,
atmospheric
science.
We
have
pioneered
use
cavity
ring-down
spectroscopy
(CRDS),
with
concurrent
angularly
resolved
elastic
light
scattering
measurements,
interrogate
single
levitated
electrodynamic
traps.
This
approach
enables
robust
such
extinction
cross
sections
individual
known
size.
Our
measurements
can
now
distinguish
absorption
contributions
overall
extinction,
from
which
real
imaginary
components
complex
refractive
indices
be
retrieved
linked
composition.
In
this
Feature
Article,
we
show
that
innovative
measurement
platform
precise
spherical
nonspherical
particles,
whether
nonabsorbing
or
absorbing
at
CRDS
probe
wavelength.
discuss
limitations
our
key
challenges
addressed
by
controlled
environments.
ACS Earth and Space Chemistry,
Journal Year:
2023,
Volume and Issue:
7(3), P. 632 - 641
Published: Feb. 24, 2023
Nitrophenols
are
a
major
component
of
light-absorbing
atmospheric
organic
aerosols,
commonly
referred
to
as
brown
carbon
(BrC).
Most
nitrophenol
formation
pathways
involve
reactions
phenolic
compounds
with
OH,
NO3,
and
NO2
in
the
gas
phase.
In
this
study,
an
aqueous
production
pathway
is
investigated
that
can
proceed
dark
without
apparent
OH
radical
formation.
Using
high-performance
liquid
chromatography–mass
spectrometry,
we
demonstrate
catechol
reacts
acidic
solutions
dissolved
nitrite
form
nitrocatechol.
The
rate
nitration
increases
significantly
from
pH
4.4
3.4
such
nitrocatechol
susceptible
second-generation
under
most
conditions
producing
chromophores
absorb
visible
region
(peak
at
425
nm).
Increases
N:C
ratio
reaction
solution,
detected
by
aerosol
mass
enhanced
absorption
300
500
nm
wood
peat
smoke
extracts
exposed
suggest
general
pathway.
which
BrC
process
may
occur
discussed.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(8), P. 4775 - 4799
Published: April 24, 2023
Abstract.
Aerosol
over
the
remote
southeastern
Atlantic
is
some
of
most
sunlight-absorbing
aerosol
on
planet:
in
situ
free-tropospheric
single-scattering
albedo
at
530
nm
wavelength
(SSA530
nm)
ranges
from
0.83
to
0.89
within
ORACLES
(ObseRvations
Aerosols
above
CLouds
and
their
intEractionS)
aircraft
flights
late
August–September.
Here
we
seek
explain
low
SSA.
The
SSA
depends
strongly
black
carbon
(BC)
number
fraction,
which
0.15
0.4.
Low
organic
(OA)-to-BC
mass
ratios
8–14
modified
combustion
efficiency
values
>0.975
point
indirectly
dry,
flame-efficient
primarily
grass
fuels,
with
back
trajectories
ending
miombo
woodlands
Angola.
youngest
aerosol,
aged
4–5
d
since
emission,
occupied
top
half
a
5
km
thick
plume
sampled
directly
west
Angola
vertically
consistent
BC:ΔCO
(carbon
monoxide)
ratio,
indicating
homogenization
source
emissions.
younger
transported
more
quickly
off
continent
by
stronger
winds,
overlaid
older,
slower-moving
larger
mean
particle
size
fraction
BC-containing
particles.
This
ongoing
gas
condensation
coagulation
smaller
non-BC
particles
upon
volumes
OA:BC
older
were
smaller,
attributed
evaporation
following
fragmentation,
instead
dilution
or
thermodynamics.
CLARIFY
(CLoud–Aerosol–Radiation
Interaction
Forcing:
Year
2017)
campaign
aerosols
that
had
traveled
further
reach
Ascension
Island.
reported
higher
BC
fractions,
lower
ratios,
yet
absorption
coefficients
compared
this
study's.
Values
one
2017
flight,
held
midway
Island,
are
intermediate,
confirming
long-range
changes.
Overall
data
continuing
oxidation
through
fragmentation
releasing
subsequently
enter
phase,
reducing
OA
mass,
rather
than
support
best
fit:
SSA530nm=0.801+0055⋅(OA:BC)
(r=0.84).
fires
southern
Africa
emit
approximately
one-third
world's
carbon;
emitted
distinct
other
regional
smoke
emissions,
composition
needs
be
represented
appropriately
realistically
depict
radiative
effects.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(4), P. 2333 - 2363
Published: Feb. 21, 2025
Abstract.
African
biomass-burning
aerosol
(BBA)
in
the
southeast
Atlantic
Ocean
(SEA)
marine
boundary
layer
(MBL)
is
an
important
contributor
to
Earth's
radiation
budget,
yet
its
representation
remains
poorly
constrained
regional
and
global
climate
models.
Data
from
Layered
Smoke
Interactions
with
Clouds
(LASIC)
field
campaign
on
Ascension
Island
(7.95°
S,
14.36°
W)
provide
insight
into
how
burning
conditions,
fuel
type,
transport
pathways,
atmospheric
processing
affect
chemical,
microphysical,
optical
properties
of
BBA
between
June
September
2017.
A
total
10
individual
plume
events
characterize
seasonal
evolution
properties.
Early-season
inefficient
fires,
determined
by
low
refractory
black
carbon
above-background
monoxide
mixing
ratios
(rBC
:
ΔCO),
led
enhanced
concentrations
organic-
sulfate-rich
aerosols.
Mid-season
efficient
higher
rBC
ΔCO
values,
rBC-enriched
BBA.
mix
fires
later
season
resulted
conflicting
Prolonged
(∼
d)
through
MBL
lower
free
troposphere
(FT)
facilitated
chemical
aqueous-phase
processing,
which
a
reduction
organic
mass
concentrations.
This
(OA)
(OA
rBC)
(2–5)
compared
values
(5–15)
nearby
FT.
These
cloud
oxidation
processes
yield
more
light-absorbing
explain
notably
single-scattering
albedo
at
530
nm
(SSA530)
(<
0.80)
observed
MBL.
study
establishes
robust
correlation
SSA530
OA
across
FT,
underscoring
dependency
composition.