Abstract.
We
characterize
the
aerosol
physical
and
optical
properties
of
13Â
transported
biomass
burningÂ
(BB)
events.
BBÂ
events
included
long-range
influence
from
fires
in
Alaskan
Siberian
boreal
forests
to
Mt.Â
Bachelor
Observatory
(MBO)
free
troposphereÂ
(FT)
over
8â14+âd
regional
wildfires
northern
California
southwestern
Oregon
MBO
boundary
layerÂ
(BL)
10âh
3âd.
Intensive
normalized
enhancement
ratios
for
were
derived
measured
light
scattering
coefficientsÂ
(Ïscat),
light-absorbing
class="inline-formula">Ïabs),
fine
particulate
matterÂ
(PM1),
carbon
monoxideÂ
(CO)
measurements
made
July
SeptemberÂ
2019,
with
particle
size
distribution
collected
August
September.
The
observations
showed
that
had
a
lower
Ã
ngström
exponentÂ
(SAE),
higher
mass
efficiencyÂ
(MSE;
),
bimodal
geometric
mean
diameterÂ
class="inline-formula">Dg).
hypothesize
larger
particles
associated
due
transport
dust
alongside
smoke
addition
contributions
condensation
secondary
aerosol,
coagulation
smaller
particles,
aqueous-phase
processing
during
transport.
forest
plumes
long
distances
theÂ
FT
characterized
by
absorption
(AAE)
values
indicative
black
carbonÂ
(BC)
dominance
radiative
budget.
Significantly
elevated
AAE
only
observed
class="inline-formula"><1âd
transport,
which
suggests
strong
production
brown
(BrC)
these
but
limited
forcing
impacts
outside
immediate
region.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(20), P. 14315 - 14325
Published: Oct. 6, 2022
The
lifecycle
of
black
carbon
(BC)-containing
particles
from
biomass
burns
is
examined
using
aircraft
and
surface
observations
the
BC
mixing
state
for
plume
ages
∼15
min
to
10
days.
Because
nonvolatile
chemically
inert,
changes
in
BC-containing
are
driven
solely
by
particle
coating,
which
mainly
secondary
organic
aerosol
(SOA).
coating
mass
initially
increases
rapidly
(kgrowth
=
0.84
h–1),
then
remains
relatively
constant
1–2
days
as
dilution
no
longer
supports
further
growth,
decreases
slowly
until
only
∼30%
maximum
after
(kloss
0.011
h–1).
ratio
coating-to-core
a
with
100
nm
mass-equivalent
diameter
core
reaches
∼20
few
hours
drops
∼5
aging.
initial
increase
can
be
used
determine
SOA
formation
rates.
slow
loss
material,
not
captured
global
models,
comprises
dominant
fraction
these
particles.
Coating-to-core
ratios
stratosphere
much
greater
than
those
free
troposphere
indicating
different
lifecycle.
ACS Earth and Space Chemistry,
Journal Year:
2023,
Volume and Issue:
7(5), P. 1107 - 1119
Published: April 24, 2023
Atmospheric
brown
carbon
(BrC)
can
impact
the
radiative
balance
of
earth
and
form
photooxidants.
However,
light
absorption
photochemical
properties
BrC
from
different
sources
remain
poorly
understood.
To
address
this
gap,
dilute
water
extracts
particulate
matter
(PM)
samples
collected
at
Davis,
CA
over
one
year
were
analyzed
using
high
resolution
aerosol
mass
spectrometry
(HR-AMS)
UV-vis
spectroscopy.
Positive
matrix
factorization
(PMF)
on
combined
AMS
data
resolved
five
water-soluble
organic
(WSOA)
factors
with
distinct
spectra
spectra:
a
fresh
an
aged
biomass
burning
OA
(WSBBOAfresh
WSBBOAaged)
three
oxygenated
(WSOOAs).
WSBBOAfresh
is
most
light-absorbing,
coefficient
(MAC365
nm)
1.1
m2
g-1,
while
WSOOAs
are
least
nm
=
0.01-0.1
g-1).
These
results,
together
abundance
WSBBOAs
(∼52%
WSOA
mass),
indicate
that
activities
such
as
residential
wood
wildfires
important
source
in
northern
California.
The
concentrations
aqueous-phase
photooxidants,
i.e.,
hydroxyl
radical
(·OH),
singlet
molecular
oxygen
(1O2*),
oxidizing
triplet
excited
states
(3C*),
also
measured
PM
during
illumination.
Oxidant
production
potentials
(PPOX)
explored.
photoexcitation
chromophores
BB
emissions
OOAs
significant
1O2*
3C*.
By
applying
our
PPOX
values
to
archived
dozens
sites,
we
found
species
play
role
photooxidant
formation
atmospheric
waters.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(1), P. 1 - 21
Published: Jan. 2, 2024
Abstract.
Fog/cloud
drops
and
aerosol
liquid
water
are
important
sites
for
the
transformations
of
atmospheric
species,
largely
through
reactions
with
photoformed
oxidants
such
as
hydroxyl
radical
(⚫OH),
singlet
molecular
oxygen
(1O2∗),
oxidizing
triplet
excited
states
organic
matter
(3C∗).
Despite
their
importance,
few
studies
have
measured
these
or
seasonal
variations.
To
address
this
gap,
we
collected
ambient
PM2.5
from
Davis,
California,
over
course
a
year
photooxidant
concentrations
light
absorption
in
dilute
aqueous
extracts.
Mass
coefficients
(MACs)
normalized
by
dissolved
carbon
range
0.4–3.8
m2
per
gram
C
at
300
nm.
Concentrations
⚫OH,
1O2∗,
3C∗
extracts
(0.2–4.7)
×
10−15
M,
(0.7–45)
10−13
(0.03–7.9)
respectively,
biomass
burning
brown
playing
major
role
formation
1O2∗
3C∗.
Extrapolating
kinetics
our
particle
to
concentrated
(ALW)
conditions
gives
an
estimated
⚫OH
concentration
7
M
ranges
(0.6–7)
10−12
(0.2–1)
respectively.
Compared
results
Kaur
et
al.
(2019),
ALW
predictions
show
roughly
10
times
higher
up
5
3C,
that
lower
factors
20–100.
These
suggest
dominate
processing
compounds
react
quickly
(e.g.,
phenols
furans,
respectively),
while
is
more
less
reactive
organics.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(1), P. 553 - 576
Published: Jan. 15, 2024
Abstract.
Wildfires
in
Siberia
generate
large
amounts
of
aerosols,
which
may
be
transported
over
long
distances
and
pose
a
threat
to
the
sensitive
ecosystem
Arctic.
Particulate
matter
(PM)
aged
wildfire
plumes
originating
from
Yakutia
August
2021
was
collected
Nadym
on
Bely
Island
(both
northwestern
Siberia).
An
advanced
analysis
chemical
composition
aerosol
particles
conducted
through
multi-wavelength
thermal–optical
carbon
analyzer
(TOCA)
coupled
resonance-enhanced
multiphoton
ionization
time-of-flight
mass
spectrometry
(REMPI-TOFMS)
as
well
ultra-high-resolution
Fourier-transform
ion
cyclotron
resonance
(FT-ICR
MS).
In
Nadym,
concentrations
organic
(OC)
elemental
(EC)
peaked
at
100
40
µg
m−3,
respectively,
associated
with
Angström
absorption
exponents
for
405
808
nm
(AAE405/808)
between
1.5
3.3.
The
weekly
average
8.9
m−3
OC
0.3
EC
AAE405/808
close
unity.
particular,
ambient
had
distinct
biomass
burning
profile
pyrolysis
products
carbohydrates,
such
cellulose
hemicellulose,
lignin
resinoic
acids.
However,
temporarily
higher
five-
six-ring
polycyclic
aromatic
hydrocarbons
(PAHs),
different
PAH
signature
burning,
suggest
contribution
regional
gas
flaring.
FT-ICR
MS
electrospray
(ESI)
revealed
complex
mixture
highly
functionalized
compounds,
containing
up
20
oxygen
atoms,
nitrogen-
sulfur-containing
moieties.
Concentrations
markers
were
substantially
lower
than
flanked
by
appearance
unique
compounds
content,
molecular
weight,
aromaticity.
Back-trajectory
satellite-derived
optical
depth
suggested
long-range
transport
center
Yakutian
plume
periphery
Island.
Owing
its
center,
it
is
demonstrated
how
dilution
affects
during
atmospheric
aging.
Biomass
burning
organic
aerosol
(BBOA),
containing
brown
carbon
chromophores,
plays
a
critical
role
in
atmospheric
chemistry
and
climate
forcing.
However,
the
effects
of
evaporation
on
BBOA
volatility
viscosity
under
different
environmental
conditions
remain
poorly
understood.
This
study
focuses
molecular
characterization
laboratory-generated
proxies
from
wood
pyrolysis
emissions.
The
initial
mixture,
"pyrolysis
oil
(PO
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(2)
Published: Jan. 17, 2025
Abstract
Severe
haze
pollution
has
long
been
an
environmental
problem,
which
is
complicated
and
poorly
understood
in
the
Sichuan
Basin
(SCB).
In
this
study,
a
field
observation
was
carried
out
to
investigate
factors
driving
formation
urban
Chengdu,
typical
megacity
SCB.
It
found
that
accumulation
of
biomass
burning
organic
aerosol
(BBOA)
played
important
role
Chengdu.
The
average
mass
fraction
BBOA
PM
2.5
increased
from
∼1%
during
clear
days
∼10%
severe
episodes.
A
method
combining
backward
trajectory
analysis
with
fire
spot
distribution
used
evaluate
effects
regional
transport
(BB)
emissions.
results
showed
concentration
by
∼3
times
∼54%
when
BB
emissions
were
transported
adjacent
areas
Moreover,
parameter
f
60
(the
ratio
integrated
signal
at
m/z
total
component
spectrum),
indicated
impacts
emissions,
reassessed
be
0.54%
instead
widely
value
0.3%
previously.
Our
uncovered
importance
on
SCB
provided
new
insights
into
pollutant
mitigation
strategies
region.
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:
2023,
Volume and Issue:
23(24), P. 15693 - 15709
Published: Dec. 21, 2023
Abstract.
With
a
few
exceptions,
most
studies
on
tropospheric
ozone
(O3)
variability
during
and
following
the
COrona
VIrus
Disease
(COVID-19)
economic
downturn
focused
high-emission
regions
or
urban
environments.
In
this
work,
we
investigated
impact
of
societal
restriction
measures
COVID-19
pandemic
surface
O3
at
several
high-elevation
sites
across
North
America
western
Europe.
Monthly
anomalies
were
calculated
for
2020
2021,
with
respect
to
baseline
period
2000–2019,
explore
initiated
in
its
recovery
2021.
total,
41
analyzed:
5
rural
mountaintop
stations
Europe,
19
US,
4
US
downwind
highly
polluted
source
regions,
eastern
plus
9
outside
Europe
United
States
provide
“global”
reference.
2020,
European
showed
persistent
negative
spring
(March–May,
i.e.,
MAM)
summer
(June–August,
JJA),
except
April.
The
pattern
was
similar
June.
behavior,
MAM
JJA
(except
August)
2021
seasonal
mean
influenced
by
strong
positive
July
due
large
widespread
wildfires
US.
slight
resulting
anomaly
pronounced
month-to-month
anomalies.
also
characterized
below-mean
both
while
values
exhibited
an
opposite
structure
compared
sites,
which
wildfires.
Concerning
rest
world,
global
picture
could
not
be
drawn,
as
spanning
range
different
environments,
did
show
consistent
anomalies,
experiencing
any
notable
variation.
Moreover,
our
mid-tropospheric
detected
IASI
(Infrared
Atmospheric
Sounding
Interferometer)
satellite
instrument.
Negative
observed
IASI,
published
modeling
studies,
suggesting
that
can
largely
attributed
reduction
precursor
emissions
2020.