Atmospheric chemistry and physics,
Journal Year:
2010,
Volume and Issue:
10(2), P. 525 - 546
Published: Jan. 20, 2010
Abstract.
New
primary
and
secondary
organic
aerosol
modules
have
been
added
to
PMCAMx,
a
three
dimensional
chemical
transport
model
(CTM),
for
use
with
the
SAPRC99
chemistry
mechanism
based
on
recent
smog
chamber
studies.
The
new
modelling
framework
is
volatility
basis-set
approach:
both
components
are
assumed
be
semivolatile
photochemically
reactive
distributed
in
logarithmically
spaced
bins.
This
of
basis
parameters
low-NOx
high-NOx
conditions
tends
predict
4–6
times
higher
anthropogenic
SOA
concentrations
than
those
predicted
older
generation
models.
resulting
PMCAMx-2008
was
applied
Mexico
City
Metropolitan
Area
(MCMA)
approximately
week
during
April
2003
period
very
low
regional
biomass
burning
impact.
emission
inventory,
which
uses
as
starting
point
MCMA
2004
official
modified
(POA)
emissions
by
dilution
experiments.
(OA)
peak
center
City,
reaching
values
above
40
μg
m−3.
predictions
compared
results
Positive
Matrix
Factorization
(PMF)
analysis
Aerosol
Mass
Spectrometry
(AMS)
observations.
reproduces
Hydrocarbon-like
Organic
(HOA)
Oxygenated
(OOA)
diurnal
profiles.
small
OA
underprediction
rush-hour
periods
overprediction
afternoon
suggest
potential
improvements
description
fresh
formation
oxygenated
aerosols,
respectively,
although
they
may
also
due
errors
simulation
dispersion
vertical
mixing.
However,
AMS
OOA
data
not
specific
enough
prove
that
observations
right
reasons.
Other
combinations
contributions
production
rates
lead
similar
results.
strongly
that,
simulated
period,
from
outside
city
significant
contributor
observed
levels.
Future
simulations
should
larger
domain
order
test
whether
can
current
parameterizations.
Sensitivity
tests
indicate
concentration
especially
sensitive
distribution
lower
Atmospheric chemistry and physics,
Journal Year:
2014,
Volume and Issue:
14(19), P. 10845 - 10895
Published: Oct. 15, 2014
Abstract.
This
paper
evaluates
the
current
status
of
global
modeling
organic
aerosol
(OA)
in
troposphere
and
analyzes
differences
between
models
as
well
observations.
Thirty-one
chemistry
transport
(CTMs)
general
circulation
(GCMs)
have
participated
this
intercomparison,
framework
AeroCom
phase
II.
The
simulation
OA
varies
greatly
terms
magnitude
primary
emissions,
secondary
(SOA)
formation,
number
species
used
(2
to
62),
complexity
parameterizations
(gas-particle
partitioning,
chemical
aging,
multiphase
chemistry,
microphysics),
physical,
optical
properties.
diversity
results
has
increased
since
earlier
experiments,
mainly
due
increasing
SOA
parameterization
models,
implementation
new,
highly
uncertain,
sources.
Diversity
over
one
order
exists
modeled
vertical
distribution
concentrations
that
deserves
a
dedicated
future
study.
Furthermore,
although
/
OC
ratio
depends
on
sources
atmospheric
processing,
is
important
for
model
evaluation
against
observations,
it
resolved
only
by
few
models.
median
(POA)
source
strength
56
Tg
a−1
(range
34–144
a−1)
(natural
anthropogenic)
19
13–121
a−1).
Among
take
into
account
semi-volatile
nature,
calculated
be
51
16–121
a−1),
much
larger
than
value
calculate
more
simplistic
way
(19
a−1;
range
13–20
a−1,
with
at
37
burden
1.4
(24
0.6–2.0
4
2.0
3.8
Tg),
lifetime
5.4
days
3.8–9.6
days).
In
reported
both
sulfate
burdens,
OA/sulfate
0.77;
13
lower
1,
9
higher
1.
For
26
deposition
fluxes,
wet
removal
70
28–209
which
average
85%
total
deposition.
Fine
carbon
(OC)
observations
from
continuous
monitoring
networks
individual
field
campaigns
been
evaluation.
At
urban
locations,
model–observation
comparison
indicates
missing
knowledge
anthropogenic
sources,
seasonality.
combined
model–measurements
analysis
suggests
existence
levels
during
summer
biogenic
formation
large
areas
USA
can
same
POA,
even
contribute
measured
seasonal
pattern.
Global
are
able
simulate
high
character
observed
atmosphere
result
POA
amount
present
remains
largely
underestimated,
mean
normalized
bias
(MNB)
equal
−0.62
(−0.51)
based
data
all
surface,
−0.15
(+0.51)
when
compared
remote
measurements,
−0.30
marine
locations
data.
temporal
correlations
across
stations
low
measurements:
0.47
(0.52)
stations,
0.39
(0.37)
0.25
combination
(negative)
MNB
correlation
sites
about
processes
govern
removal,
top
their
stations.
There
no
clear
change
skill
regard
or
mass
concentration.
However,
needed
distinguish
natural
climate
mitigation,
impact
accurately.
Journal of Geophysical Research Atmospheres,
Journal Year:
2009,
Volume and Issue:
114(D19)
Published: Oct. 13, 2009
We
characterized
the
gas‐
and
speciated
aerosol‐phase
emissions
from
open
combustion
of
33
different
plant
species
during
a
series
255
controlled
laboratory
burns
Fire
Laboratory
at
Missoula
Experiments
(FLAME).
The
we
tested
were
chosen
to
improve
existing
database
for
U.S.
domestic
fuels:
laboratory‐based
emission
factors
have
not
previously
been
reported
many
commonly
burned
that
are
frequently
consumed
by
fires
near
populated
regions
protected
scenic
areas.
plants
included
chaparral
chamise,
manzanita,
ceanothus,
common
southeastern
United
States
(common
reed,
hickory,
kudzu,
needlegrass
rush,
rhododendron,
cord
grass,
sawgrass,
titi,
wax
myrtle).
Fire‐integrated
gas‐phase
CO
2
,
CO,
CH
4
C
2–4
hydrocarbons,
NH
3
SO
NO,
NO
HNO
particle‐phase
organic
carbon
(OC),
elemental
(EC),
2−
−
Cl
Na
+
K
generally
varied
with
both
fuel
type
fire‐integrated
modified
efficiency
(MCE),
measure
relative
importance
flaming‐
smoldering‐phase
total
burn.
Chaparral
fuels
tended
emit
less
particulate
OC
per
unit
mass
dry
than
did
other
types,
whereas
had
some
largest
observed
fine
matter.
Our
measurements
spanned
larger
range
MCE
prior
studies,
thus
help
estimates
variation
conditions
individual
fuels.
Environmental Science & Technology,
Journal Year:
2010,
Volume and Issue:
44(22), P. 8553 - 8560
Published: Sept. 30, 2010
Numerous
scientific
upgrades
to
the
representation
of
secondary
organic
aerosol
(SOA)
are
incorporated
into
Community
Multiscale
Air
Quality
(CMAQ)
modeling
system.
Additions
include
several
recently
identified
SOA
precursors:
benzene,
isoprene,
and
sesquiterpenes;
pathways:
in-cloud
oxidation
glyoxal
methylglyoxal,
particle-phase
oligomerization,
acid
enhancement
isoprene
SOA.
NOx-dependent
aromatic
yields
also
added
along
with
new
empirical
measurements
enthalpies
vaporization
mass-to-carbon
ratios.
For
first
time,
these
precursors,
pathways
parameters
included
simultaneously
in
an
air
quality
model
for
annual
simulation
spanning
continental
U.S.
Comparisons
CMAQ-modeled
carbon
(OCsec)
semiempirical
estimates
screened
from
165
routine
monitoring
sites
across
indicate
module
substantially
improves
performance.
The
most
notable
improvement
occurs
central
southeastern
where
regionally
averaged
temporal
correlations
(r)
between
modeled
OCsec
increase
−0.5
0.8
−0.3
0.8,
respectively,
when
is
employed.
Wintertime
results
improve
all
regions
seasonal
regional
patterns
biogenic
better
represented.
Proceedings of the National Academy of Sciences,
Journal Year:
2011,
Volume and Issue:
108(6), P. 2190 - 2195
Published: Jan. 24, 2011
Field
measurements
of
secondary
organic
aerosol
(SOA)
find
significantly
higher
mass
loads
than
predicted
by
models,
sparking
intense
effort
focused
on
finding
additional
SOA
sources
but
leaving
the
fundamental
assumptions
used
models
unchallenged.
Current
air-quality
use
absorptive
partitioning
theory
assuming
particles
are
liquid
droplets,
forming
instantaneous
reversible
equilibrium
with
gas
phase.
Further,
they
ignore
effects
adsorption
spectator
species
during
formation
properties
and
fate.
Using
accurate
highly
sensitive
experimental
approach
for
studying
evaporation
kinetics
size-selected
single
particles,
we
characterized
room-temperature
laboratory-generated
α-pinene
ambient
atmospheric
SOA.
We
found
that
even
when
phase
organics
removed,
it
takes
∼24
h
pure
to
evaporate
75%
their
mass,
which
is
in
sharp
contrast
∼10
min
time
scale
current
kinetic
models.
Adsorption
“spectator”
vapors
formation,
aging
these
coated
dramatically
reduced
rate,
some
cases
nearly
stopped
it.
Ambient
was
exhibit
behavior
very
similar
aged
For
all
studied
this
work,
size-independent
does
not
follow
model
assumptions.
The
findings
about
phase,
rates,
importance
gases
indicate
there
need
reformulate
way
treated
Atmospheric chemistry and physics,
Journal Year:
2010,
Volume and Issue:
10(18), P. 8697 - 8760
Published: Sept. 16, 2010
Abstract.
MILAGRO
(Megacity
Initiative:
Local
And
Global
Research
Observations)
is
an
international
collaborative
project
to
examine
the
behavior
and
export
of
atmospheric
emissions
from
a
megacity.
The
Mexico
City
Metropolitan
Area
(MCMA)
–
one
world's
largest
megacities
North
America's
most
populous
city
was
selected
as
case
study
characterize
sources,
concentrations,
transport,
transformation
processes
gases
fine
particles
emitted
MCMA
atmosphere
evaluate
regional
global
impacts
these
emissions.
findings
this
are
relevant
evolution
pollution
many
other
megacities.
measurement
phase
consisted
month-long
series
carefully
coordinated
observations
chemistry
physics
in
near
during
March
2006,
using
wide
range
instruments
at
ground
sites,
on
aircraft
satellites,
enlisting
over
450
scientists
150
institutions
30
countries.
Three
supersites
were
set
up
primary
particles.
Additional
platforms
or
included
mobile
vans
containing
scientific
laboratories
stationary
upward-looking
lidars.
Seven
instrumented
research
provided
information
about
large
region
various
altitudes.
Satellite-based
peered
down
into
atmosphere,
providing
even
larger
geographical
coverage.
overall
campaign
complemented
by
meteorological
forecasting
numerical
simulations,
satellite
surface
networks.
Together,
have
comprehensive
characterization
MCMA's
urban
composition
that
will
take
years
analyze
fully.
In
paper
we
review
120
papers
resulting
MILAGRO/INTEX-B
Campaign
been
published
submitted,
well
earlier
MCMA-2003
Campaign,
with
aim
road
map
for
community
interested
understanding
megacity
such
their
air
quality
climate.
This
describes
measurements
performed
results
obtained
meteorology
dynamics,
particles,
sources
concentrations
volatile
organic
compounds,
photochemistry,
ambient
particulate
matter,
aerosol
radiative
properties,
plume
characterization,
health
studies.
A
summary
key
field
presented.
Journal of Geophysical Research Atmospheres,
Journal Year:
2016,
Volume and Issue:
121(4), P. 1955 - 1977
Published: Jan. 23, 2016
Abstract
To
investigate
the
seasonal
characteristics
of
submicron
aerosol
(PM
1
)
in
Beijing
urban
areas,
a
high‐resolution
time‐of‐flight
aerosol‐mass‐spectrometer
(HR‐ToF‐AMS)
was
utilized
at
an
site
summer
(August
to
September
2011)
and
winter
(November
December
2010),
coupled
with
multiple
state
art
online
instruments.
The
average
mass
concentrations
PM
(60–84
µg
m
−3
its
chemical
compositions
different
campaigns
were
relatively
consistent
recent
years.
In
summer,
daily
variations
stable
repeatable.
Eighty‐two
percent
concentration
on
composed
secondary
species,
where
62%
is
inorganic
20%
organic
(SOA).
winter,
changed
dramatically
because
meteorological
conditions.
high
fraction
(58%)
primary
species
including
(POA),
black
carbon,
chloride
indicates
emissions
usually
played
more
important
role
winter.
However,
aqueous
chemistry
resulting
efficient
formation
during
occasional
periods
relative
humidity
may
also
contribute
substantially
haze
Results
past
OA
source
apportionment
studies
show
45–67%
22–50%
can
be
SOA.
Based
results,
we
found
45%
POA
61%
are
from
nonfossil
sources,
contributed
by
cooking
both
seasons
biomass
burning
(BBOA)
Cooking
OA,
accounting
for
13–24%
carbon
all
years
should
not
neglected.
fossil
sources
include
hydrocarbon‐like
vehicle
coal
combustion
(CCOA)
CCOA
BBOA
two
main
contributors
(57%
OA)
highest
(>100
POA/ΔCO
ratios
11
16
ppm
−1
,
respectively,
similar
western
cities.
Higher
OOA/O
x
(=
NO
2
+
O
3
ratio
(0.49
ppb
study
than
these
cities
(0.03–0.16
observed,
which
due
reaction
or
extra
SOA
semivolatile
compounds
various
(e.g.,
CCOA)
Beijing.
evolution
oxygen
(O/C)
photochemical
age
allows
estimate
equivalent
rate
constant
aging
as
k
OH
~
4.1
×
10
−12
cm
molecule
s
same
order
obtained
other
anthropogenic
influenced
areas
useful
modeling.
Atmospheric chemistry and physics,
Journal Year:
2014,
Volume and Issue:
14(12), P. 6159 - 6176
Published: June 23, 2014
Abstract.
Organic
aerosols
(OA)
represent
one
of
the
major
constituents
submicron
particulate
matter
(PM1)
and
comprise
a
huge
variety
compounds
emitted
by
different
sources.
Three
intensive
measurement
field
campaigns
to
investigate
aerosol
chemical
composition
all
over
Europe
were
carried
out
within
framework
European
Integrated
Project
on
Aerosol
Cloud
Climate
Air
Quality
Interactions
(EUCAARI)
Monitoring
Evaluation
Programme
(EMEP)
during
2008
(May–June
September–October)
2009
(February–March).
In
this
paper
we
focus
identification
main
organic
sources
define
standardized
methodology
perform
source
apportionment
using
positive
matrix
factorization
(PMF)
with
multilinear
engine
(ME-2)
Aerodyne
mass
spectrometer
(AMS)
data.
Our
procedure
is
tested
applied
25
data
sets
accounting
for
two
urban,
several
rural
remote
high
altitude
sites;
therefore
it
likely
suitable
treatment
AMS-related
ambient
sets.
For
most
sites,
four
components
are
retrieved,
improving
significantly
previous
results
where
only
separation
in
primary
secondary
OA
was
possible.
Generally,
our
solutions
include
sources,
i.e.
hydrocarbon-like
(HOA)
biomass
burning
(BBOA)
components,
semi-volatile
oxygenated
(SV-OOA)
low-volatility
(LV-OOA).
specific
sites
cooking-related
(COA)
marine-related
(MSA)
also
separated.
Finally,
work
provides
large
overview
an
interesting
set
highly
time
resolved
modeling
purposes.