Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(15), P. 10173 - 10194
Published: Aug. 9, 2022
Abstract.
Peat
fires
in
Southeast
Asia
are
a
major
source
of
trace
gases
and
particles
to
the
regional-global
atmosphere
that
influence
atmospheric
chemistry,
climate,
air
quality.
During
November
2015
record-high
Ocean
Niño
Index
(ONI,
2.6)
our
mobile
smoke
sampling
team
made
first,
or
rare,
field
measurements
numerous
gases,
aerosol
optical
properties,
chemistry
mass
emissions
for
burning
only
peat
Indonesian
province
Central
Kalimantan
(on
island
Borneo).
The
used
Fourier
transform
infrared
spectroscopy
(FTIR),
whole
(WAS),
photoacoustic
extinctiometers
(PAX,
401
870
nm),
detailed
off-line
analyses
particulate
matter
(PM)
collected
on
filters.
In
September–November
2019
we
measured
fire
gas
again,
using
WAS
only,
under
El
Niño–Southern
Oscillation
(ENSO)-neutral
conditions
0.3)
more
remote
areas
also
provinces
Riau,
Jambi,
South
Sumatra,
all
Sumatra.
significantly
expanded
geographic
range
climate
sampled.
This
paper
presents
results
synthesizes
them
with
previous
fieldwork
converge
robust
regional
average
emission
factors
(EFs;
grams
compound
per
kilogram
biomass
burned)
authentic
fires.
addition,
samples
imported
from
Indonesia
were
burned
US
laboratories,
EFs
properties
characterized
detail
than
by
larger
suite
instrumentation.
We
use
improved
knowledge
based
select
most
representative
lab
data
compute
synthesized,
“chemically
complete”
set
tropical
modified
combustion
efficiency
(MCE)
values
sampled
within
MCEs
2015,
but
lower
(0.718±0.021,
0.687–0.736)
(0.772±0.035,
0.693–0.835).
Averaging
new
older
together
suggests
an
updated
MCE
∼0.76.
Despite
difference
MCE,
study-average
methane
(EF
CH4)
remarkably
similar
across
2
years
probing
different
regions:
9.42±2.51
g
kg−1
9.51±4.74
2015.
When
parsing
province,
non-methane
organic
(NMOGs)
about
3
times
higher
Sumatra
Jambi
overall
study
was
∼15
%
average.
emitted
amounts
carbonyl
dimethyl
sulfide,
suggesting
volcanic
marine
effects
agricultural
chemicals.
taken
provide
230
including
CO2
(1544
kg−1),
CO
(315
CH4
(9.8
kg−1).
These
significant
adjustments
IPCC-recommended
EFs,
−9
%,
+50
−53
respectively.
report
NMOGs,
46
N-containing
compounds,
14
sulfur-
halogen-containing
species.
high-resolution
spectrometry
allowed
measurement
82
NMOG
field.
Gravimetrically
EF
PM2.5
(17.3±5.8
kg−1)
∼20
studies
(22.4±10.4
perhaps
due
temperatures.
Taken
show
single-scattering
albedo
(SSA)
largely
independent
wavelength
visible
(∼0.998),
at
low
405
nm
value
0.958
MCE.
absorption
Ångström
exponent
(AAE)
5.7.
By
far
largest
PM
component
weakly
absorbing
insoluble
carbon.
Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
128(2)
Published: Dec. 30, 2022
Abstract
The
NOAA/NASA
Fire
Influence
on
Regional
to
Global
Environments
and
Air
Quality
(FIREX‐AQ)
experiment
was
a
multi‐agency,
inter‐disciplinary
research
effort
to:
(a)
obtain
detailed
measurements
of
trace
gas
aerosol
emissions
from
wildfires
prescribed
fires
using
aircraft,
satellites
ground‐based
instruments,
(b)
make
extensive
suborbital
remote
sensing
fire
dynamics,
(c)
assess
local,
regional,
global
modeling
fires,
(d)
strengthen
connections
observables
the
ground
such
as
fuels
fuel
consumption
satellite
products
burned
area
radiative
power.
From
Boise,
ID
western
were
studied
with
NASA
DC‐8
two
NOAA
Twin
Otter
aircraft.
high‐altitude
ER‐2
deployed
Palmdale,
CA
observe
some
these
in
conjunction
overpasses
other
Further
conducted
three
mobile
laboratories
sites,
17
different
forecast
analyses
for
fire,
air
quality
climate
implications.
Salina,
KS
investigated
87
smaller
Southeast
in‐situ
data
collection.
Sampling
by
all
platforms
designed
measure
gases
aerosols
multiple
transects
capture
chemical
transformation
perform
observations
smoke
plumes
under
day
night
conditions.
linked
consumed
power
orbital
collected
during
overflights
sampling
fuels.
Journal of Geophysical Research Atmospheres,
Journal Year:
2020,
Volume and Issue:
126(4)
Published: Dec. 23, 2020
Abstract
The
Western
Wildfire
Experiment
for
Cloud
Chemistry,
Aerosol
Absorption,
and
Nitrogen
(WE‐CAN)
deployed
the
NSF/NCAR
C‐130
aircraft
in
summer
2018
across
western
U.S.
to
sample
wildfire
smoke
during
its
first
days
of
atmospheric
evolution.
We
present
a
summary
subset
reactive
oxidized
nitrogen
species
(NO
y
)
plumes
sampled
pseudo‐Lagrangian
fashion.
Emissions
oxides
x
=
NO
+
2
nitrous
acid
(HONO)
are
rapidly
converted
more
forms.
Within
4
h,
∼86%
ΣNO
is
form
peroxy
acyl
nitrates
(PANs)
(∼37%),
particulate
nitrate
(
p
3
(∼27%),
gas‐phase
organic
(Org
N
(g)
(∼23%).
average
e
‐folding
time
distance
∼90
min
∼40
km,
respectively.
Nearly
no
enhancements
nitric
(HNO
were
observed
fashion,
implying
HNO
‐limited
ammonium
(NH
formation,
with
one
notable
exception
that
we
highlight
as
case
study.
also
summarize
partitioning
all
samples
intercepted
WE‐CAN.
In
above
km
sea
level
(ASL),
contributions
PANs
increase
altitude.
WE‐CAN
from
multiple
fires
mixed
anthropogenic
emissions
over
California
Central
Valley.
distinguish
where
appear
lead
an
abundances
by
factor
four
contribute
additional
PAN
formation.
Atmospheric measurement techniques,
Journal Year:
2021,
Volume and Issue:
14(6), P. 4517 - 4542
Published: June 18, 2021
Abstract.
We
evaluate
the
sensitivity
of
size
calibrations
two
commercially
available,
high-resolution
optical
particle
sizers
to
changes
in
aerosol
composition
and
complex
refractive
index
(RI).
The
Droplet
Measurement
Technologies
Ultra-High
Sensitivity
Aerosol
Spectrometer
(UHSAS)
TSI,
Inc.
Laser
(LAS)
are
commonly
used
instruments
for
measuring
portion
distribution
with
diameters
larger
than
nominally
60–90
nm.
Both
illuminate
particles
a
laser
relate
single-particle
light
scattering
intensity
count
rate
measured
over
wide
range
angles
size-dependent
concentration.
While
block
geometry
flow
system
similar
each
instrument,
significant
difference
between
models
is
wavelength
(1054
nm
UHSAS
633
LAS)
(about
100
times
higher
UHSAS),
which
may
affect
way
instrument
sizes
non-spherical
or
absorbing
aerosols.
Here,
we
challenge
LAS
laboratory-generated,
mobility-size-classified
aerosols
known
chemical
quantify
response
relative
that
ammonium
sulfate
(RI
1.52+0i
at
532
nm)
NIST-traceable
polystyrene
latex
spheres
(PSLs
RI
1.59+0i
589
nm).
inorganic
salt
species
chosen
cover
real
1.32
1.78,
while
light-absorbing
carbonaceous
include
fullerene
soot,
nigrosine
dye,
humic
acid,
fulvic
acid
standards.
generally
good
agreement
electrical
mobility
diameter.
However,
large
undersizing
deviations
observed
low-refractive-index
fluoride
salts
strongly
dye
soot
particles.
Polydisperse
distributions
both
fresh
aged
wildfire
smoke
from
recent
Fire
Influence
on
Regional
Global
Environments
Experiment
Air
Quality
(FIREX-AQ)
Cloud,
Aerosol,
Monsoon
Processes
Philippines
(CAMP2Ex)
airborne
campaigns
show
contemporaneous
sizing
time-of-flight
mass
spectrometric
measurements.
assess
uncertainties
by
interpolating
laboratory
curves
using
previously
reported
RIs
multiple
type
classifications.
These
results
suggest
that,
underperform
compounds
tailpipe
emissions
measurements,
sampling
within
atmospherically
relevant
indices
likely
be
sized
better
±10
%–20
%
uncertainty
submicron
when
calibrated
sulfate.
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.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(12), P. 8009 - 8036
Published: June 21, 2022
Abstract.
Brown
carbon
(BrC)
associated
with
aerosol
particles
in
western
United
States
wildfires
was
measured
between
July
and
August
2019
aboard
the
NASA
DC-8
research
aircraft
during
Fire
Influence
on
Regional
to
Global
Environments
Air
Quality
(FIREX-AQ)
study.
Two
BrC
measurement
methods
are
investigated,
highly
spectrally
resolved
light
absorption
solvent
(water
methanol)
extracts
of
collected
filters
situ
bulk
particle
at
three
wavelengths
(405,
532
664
nm)
a
photoacoustic
spectrometer
(PAS).
A
light-absorption
closure
analysis
for
300
700
nm
performed.
The
combined
pure
black
material,
including
enhancements
due
internally
mixed
materials,
plus
soluble
Mie-predicted
factor
conversion
BrC,
compared
spectra
from
power
law
fit
PAS
wavelengths.
For
various
parameters
used,
wavelength
roughly
400
they
agreed,
lower
individual
component-predicted
significantly
exceeded
higher
consistently
but
more
variable.
Limitations
extrapolation
data
below
405
missing
species
low
solubility
that
strongly
absorb
may
account
differences.
Based
measurements
closest
fires,
emission
ratio
PAS-measured
relative
monoxide
(CO)
average
0.13
Mm−1
ppbv−1;
ratios
also
provided.
As
smoke
moved
away
burning
regions,
evolution
over
time
observed
be
complex;
enhancement,
depletion
or
constant
levels
age
were
all
first
8
h
after
different
plumes.
Within
following
emissions,
4-nitrocatechol,
well-characterized
chromophore
commonly
found
particles,
largely
depleted
BrC.
In
descending
plume
where
temperature
increased
by
15
K,
4-nitrocatechol
dropped,
possibly
temperature-driven
evaporation,
remained
unchanged.
Evidence
reactions
ozone,
related
species,
as
pathway
secondary
formation
under
both
high
oxides
nitrogen
(NOx)
conditions,
while
bleached
regions
ozone
NOx,
consistent
complex
behaviors
laboratory
studies.
Although
hours
is
variable,
limited
number
aged
(15
30
h)
indicate
net
loss
It
yet
determined
how
near-field
affects
characteristics
longer
timescales
spatial
scales,
its
environmental
impacts
likely
greater.
Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
127(2)
Published: Jan. 10, 2022
Abstract
Biomass
burning
(BB)
events
are
occurring
globally
with
increasing
frequency,
and
their
emissions
having
more
impacts
on
human
health
climate.
Large
ash
particles
recognized
as
a
BB
product
major
influences
soil
water
environments.
However,
fine‐ash
particles,
which
have
diameters
smaller
than
several
microns
characteristic
morphologies
compositions
(mainly
Ca
Mg
carbonates),
not
yet
been
explicitly
considered
aerosol
component
either
in
field
observations
or
climate
models.
This
study
measured
samples
using
transmission
electron
microscopy
(TEM)
ion
chromatography
during
the
Fire
Influence
Regional
to
Global
Environments
Air
Quality
(FIREX‐AQ)
campaign.
We
show
that
significant
amounts
of
fine
ash‐bearing
transported
>100
km
from
fire
sources.
Our
environmental
chamber
experiments
suggest
they
can
act
cloud
condensation
ice
nuclei.
also
found
considerable
TEM
collected
previous
campaigns
(Biomass
Burning
Observation
Project
Megacity
Initiative:
Local
Research
Observations).
These
commonly
mixed
organic
matter
make
up
∼8%
5%
smoke
by
number
mass,
respectively,
FIREX‐AQ
The
ash‐mass
concentrations
approximately
five
times
six
greater
those
black
carbon
potassium,
scaling
an
estimated
global
emission
11.6
Tg
yr
−1
range
8.8–16.3
.
Better
characterization
constraints
these
will
improve
measurements
strengthen
assessments
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(8), P. 5399 - 5414
Published: April 25, 2022
Abstract.
This
article
presents
a
study
of
long-range
transported
biomass
burning
aerosols
(BBA)
originated
from
the
North
American
wildfires
in
September
2020.
The
BBA
plumes
presented
this
were
troposphere
and
underwent
1–2
weeks
aging
before
arriving
at
lidar
station
ATOLL
(ATmospheric
Observatory
LiLle)
northern
France.
A
novel
lidar-derived
dataset,
2α+3β+3δ+ϕ
(α:
extinction
coefficient;
β:
backscatter
δ:
particle
linear
depolarization
ratio,
i.e.,
PLDR;
ϕ:
fluorescence
capacity),
is
provided
for
characterization
BBA.
capacity
an
intensive
aerosol
parameter
describing
ability
producing
when
exposed
to
UV
excitation.
In
our
observations,
obvious
variations
parameters,
reflecting
variability
properties,
detected.
PLDRs
varied
less
than
0.03
all
wavelengths
0.15–0.22
0.12–0.16,
respectively,
355
532
nm.
related
Angström
exponent
was
within
range
−0.3
1.0
×
10−4–4.0
10−4.
Lidar
ratio
as
low
24
±
4
sr
(50
8
sr)
observed
(532)
nm
on
17–18
September,
which
lower
most
previously
aged
BBAs.
These
are
likely
correlated
with
combustion
process,
lifting
conditions
(temperature,
humidities,
etc.)
process.
addition,
results
indicate
could
act
ice
nucleating
particles
tropospheric
conditions.
channel
proves
be
important
added
value
aerosol–cloud
interactions
studies,
due
its
high
sensitivity.
With
increase
wildfire
occurrence
intensity,
BBAs
become
more
atmospheric
component.
context,
we
show
potential
dataset
particles'
understanding
their
role
cloud
processes.
Reviews of Geophysics,
Journal Year:
2023,
Volume and Issue:
61(2)
Published: May 4, 2023
Abstract
Aerosol
forcing
uncertainty
represents
the
largest
climate
overall.
Its
magnitude
has
remained
virtually
undiminished
over
past
20
years
despite
considerable
advances
in
understanding
most
of
key
contributing
elements.
Recent
work
produced
modest
increases
only
confidence
estimate
itself.
This
review
summarizes
contributions
toward
reducing
aerosol
made
by
satellite
observations,
measurements
taken
within
atmosphere,
as
well
modeling
and
data
assimilation.
We
adopt
a
more
measurement‐oriented
perspective
than
reviews
subject
assessing
strengths
limitations
each;
gaps
possible
ways
to
fill
them
are
considered.
Currently
planned
programs
supporting
advanced,
global‐scale
surface‐based
aerosol,
cloud,
precursor
gas
modeling,
intensive
field
campaigns
aimed
at
characterizing
underlying
physical
chemical
processes
involved,
all
essential.
But
addition,
new
efforts
needed:
(a)
obtain
systematic
aircraft
situ
capturing
multi‐variate
probability
distribution
functions
particle
optical,
microphysical,
properties
(and
associated
estimates),
co‐variability
with
meteorology,
for
major
airmass
types;
(b)
conceive,
develop,
implement
suborbital
(aircraft
plus
surface‐based)
program
systematically
quantifying
cloud‐scale
microphysics,
cloud
optical
properties,
cloud‐related
vertical
velocities
aerosol‐cloud
interactions;
(c)
focus
much
research
on
integrating
unique
measurements,
reduce
persistent
forcing.
Atmospheric chemistry and physics,
Journal Year:
2021,
Volume and Issue:
21(9), P. 6839 - 6855
Published: May 5, 2021
Abstract.
Biomass
burning
emits
vapors
and
aerosols
into
the
atmosphere
that
can
rapidly
evolve
as
smoke
plumes
travel
downwind
dilute,
affecting
climate-
health-relevant
properties
of
smoke.
To
date,
theory
has
been
unable
to
explain
observed
variability
in
evolution.
Here,
we
use
observational
data
from
Burning
Observation
Project
(BBOP)
field
campaign
show
initial
organic
aerosol
mass
concentrations
help
predict
changes
aging
markers,
number
concentration,
mean
diameter
between
40–262
nm.
Because
measurements
are
generally
>10
min
downwind,
smaller
will
have
already
undergone
substantial
dilution
relative
larger
lower
species
at
these
observations
closest
fire.
The
extent
which
occurred
prior
first
observation
is
not
a
directly
measurable
quantity.
We
plume
serve
rough
indicator
measurement,
impacts
photochemistry,
evaporation,
coagulation.
Cores
higher
than
edges.
By
segregating
cores
edges,
find
evidence
particle
aging,
coagulation
before
measurement.
further
on
more
oxygenated,
while
marker
for
primary
biomass
emissions
decreased
abundance
compared
cores.
Finally,
attempt
decouple
roles
physical
age
since
emission
by
performing
multivariate
linear
regression
various
(composition,
size)
two
factors.
Atmospheric chemistry and physics,
Journal Year:
2021,
Volume and Issue:
21(12), P. 9417 - 9440
Published: June 21, 2021
Abstract.
Seasonal
biomass
burning
(BB)
over
West
Africa
is
a
globally
significant
source
of
carbonaceous
particles
in
the
atmosphere,
which
have
important
climate
impacts
but
are
poorly
constrained.
Here,
evolution
smoke
aerosols
emitted
from
flaming-controlled
agricultural
waste
and
wooded
savannah
Senegal
region
was
characterized
timescale
half-day
advection
during
MOYA-2017
(Methane
Observation
Yearly
Assessment-2017)
aircraft
campaign.
Plumes
such
fire
types
rich
black
carbon
(BC)
emissions.
Concurrent
measurements
chemical
composition,
organic
aerosol
(OA)
oxidation
state,
bulk
size
BC
mixing
state
reveal
that
BB
submicron
changed
dramatically
with
time.
Various
optical
properties
(e.g.
absorption
Ångström
exponent
–
AAE
mass
coefficients
MACs)
also
evolved
ageing.
In
this
study,
brown
(BrC)
minor
fractional
component
freshly
(<
0.5
h),
increasing
particle
age
indicates
BrC
formation
dominated
any
loss
process
first
∼
12
h
plume
transport.
Using
different
methods,
contribution
to
total
showed
an
trend
time
18
%–31
%
at
wavelength
405
nm
after
The
generated
found
be
positively
correlated
oxygenated
low-volatility
OA,
likely
evaporated
primary
OA
secondary
formation.
We
compared
previous
field
studies
mainly
focused
on
emissions
smouldering
fires,
shown
high
net
upon
This
study
suggests
initial
stage
enhancement
smoke.
Secondary
processing
dominant
contributor
production
region,
contrast
emission
previously
reported
other
studies.
normalized
(MACmeas-BC)
enhanced
ageing
due
lensing
effect
increasingly
thick
coatings
by
BrC.
absorption,
represented
(EAbs-MAC),
estimated
timescales
hours.
provides
novel
results.
comparisons
between
imply
absorbing
(BC
BrC)
varies
combustion
conditions.
Different
treatments
fires
their
downwind
should
considered
when
modelling
regional
radiative
forcing.
These
observational
results
will
very
for
predicting
effects
regions
controlled
flaming
savannah-like
fuels.