Nature Communications,
Journal Year:
2017,
Volume and Issue:
8(1)
Published: April 21, 2017
Secondary
organic
aerosols
(SOA)
are
a
large
source
of
uncertainty
in
our
current
understanding
climate
change
and
air
pollution.
The
phase
state
SOA
is
important
for
quantifying
their
effects
on
quality,
but
its
global
distribution
poorly
characterized.
We
developed
method
to
estimate
glass
transition
temperatures
based
the
molar
mass
molecular
O:C
ratio
components,
we
used
chemistry
model
EMAC
with
aerosol
module
ORACLE
predict
atmospheric
SOA.
For
planetary
boundary
layer,
simulations
indicate
that
mostly
liquid
tropical
polar
high
relative
humidity,
semi-solid
mid-latitudes
solid
over
dry
lands.
find
middle
upper
troposphere
should
be
glassy
state.
Thus,
slow
diffusion
water,
oxidants
molecules
could
kinetically
limit
gas-particle
interactions
free
troposphere,
promote
ice
nucleation
facilitate
long-range
transport
reactive
toxic
pollutants
embedded
Biogeosciences,
Journal Year:
2015,
Volume and Issue:
12(23), P. 7129 - 7167
Published: Dec. 8, 2015
Abstract.
The
Arctic
is
a
water-rich
region,
with
freshwater
systems
covering
about
16
%
of
the
northern
permafrost
landscape.
Permafrost
thaw
creates
new
ecosystems,
while
at
same
time
modifying
existing
lakes,
streams,
and
rivers
that
are
impacted
by
thaw.
Here,
we
describe
current
state
knowledge
regarding
how
affects
lentic
(still)
lotic
(moving)
systems,
exploring
effects
both
thermokarst
(thawing
collapse
ice-rich
permafrost)
deepening
active
layer
(the
surface
soil
thaws
refreezes
each
year).
Within
thermokarst,
further
differentiate
between
in
lowland
areas
vs.
on
hillslopes.
For
almost
all
processes
explore,
vary
regionally,
lake
stream
systems.
Much
this
regional
variation
caused
differences
ground
ice
content,
topography,
type,
coverage.
Together,
these
factors
determine
(i)
degree
to
which
manifests
as
(ii)
whether
leads
slumping
or
formation
(iii)
manner
constituent
delivery
altered
Differences
thaw-enabled
can
be
considerable,
determining,
for
example,
balance
particulate
dissolved
constituents,
inorganic
organic
materials.
Changes
composition
thaw-impacted
waters,
coupled
changes
morphology,
strongly
affect
physical
optical
properties
lakes.
ecology
lakes
streams
also
likely
change;
have
unique
microbiological
communities,
show
respiration,
primary
production,
food
web
structure
largely
driven
sediment,
matter,
nutrient
delivery.
enables
matter
morphology
stratification
characteristics
recipient
will
play
an
important
role
determining
release
greenhouse
gases
(CO2
CH4),
its
burial
sediments,
loss
downstream.
magnitude
impacts
aquatic
ecosystems
increasing,
prevalence
streams.
There
therefore
urgent
need
quantify
affecting
across
diverse
landscapes,
implications
change
climate
warming.
Atmospheric chemistry and physics,
Journal Year:
2017,
Volume and Issue:
17(3), P. 2103 - 2162
Published: Feb. 13, 2017
Oxidation
of
biogenic
volatile
organic
compounds
(BVOC)
by
the
nitrate
radical
(NO3)
represents
one
important
interactions
between
anthropogenic
emissions
related
to
combustion
and
natural
from
biosphere.
This
interaction
has
been
recognized
for
more
than
3
decades,
during
which
time
a
large
body
research
emerged
laboratory,
field,
modeling
studies.
NO3-BVOC
reactions
influence
air
quality,
climate
visibility
through
regional
global
budgets
reactive
nitrogen
(particularly
nitrates),
ozone,
aerosol.
Despite
its
long
history
significance
this
topic
in
atmospheric
chemistry,
number
uncertainties
remain.
These
include
an
incomplete
understanding
rates,
mechanisms,
aerosol
yields
reactions,
lack
constraints
on
role
heterogeneous
oxidative
processes
associated
with
NO3
radical,
difficulty
characterizing
spatial
distributions
BVOC
within
poorly
mixed
nocturnal
atmosphere,
challenge
constructing
appropriate
boundary
layer
schemes
non-photochemical
mechanisms
use
state-of-the-art
chemical
transport
chemistry-climate
models.
review
is
result
workshop
same
title
held
at
Georgia
Institute
Technology
June
2015.
The
first
half
summarizes
current
literature
particular
focus
recent
advances
instrumentation
models,
secondary
(SOA)
formation
chemistry.
Building
understanding,
second
outlines
impacts
chemistry
quality
climate,
suggests
critical
needs
better
constrain
improve
predictive
capabilities
Environmental Science & Technology,
Journal Year:
2016,
Volume and Issue:
51(3), P. 1074 - 1093
Published: Dec. 21, 2016
Secondary
organic
aerosol
(SOA)
is
formed
from
the
atmospheric
oxidation
of
gas-phase
compounds
leading
to
formation
particle
mass.
Gasoline-
and
diesel-powered
motor
vehicles,
both
on/off-road,
are
important
sources
SOA
precursors.
They
emit
complex
mixtures
that
vary
in
volatility
molecular
structure—factors
influence
their
contributions
urban
SOA.
However,
relative
importance
each
vehicle
type
with
respect
remains
unclear
due
conflicting
evidence
recent
laboratory,
field,
modeling
studies.
Both
likely
important,
evolving
location
over
short
time
scales.
This
review
summarizes
evidence,
research
needs,
discrepancies
between
top-down
bottom-up
approaches
used
estimate
focusing
on
inconsistencies
molecular-level
understanding
regional
observations.
The
effect
emission
controls
(e.g.,
exhaust
aftertreatment
technologies,
fuel
formulation)
precursor
emissions
needs
comprehensive
evaluation,
especially
international
perspective
given
heterogeneity
regulations
technology
penetration.
Novel
studies
needed
identify
quantify
"missing"
appear
contribute
substantially
production,
gasoline
vehicles
most
advanced
aftertreatment.
Initial
suggests
catalyzed
diesel
particulate
filters
greatly
reduce
precursors
along
primary
aerosol.
Nature Communications,
Journal Year:
2017,
Volume and Issue:
8(1)
Published: April 21, 2017
Secondary
organic
aerosols
(SOA)
are
a
large
source
of
uncertainty
in
our
current
understanding
climate
change
and
air
pollution.
The
phase
state
SOA
is
important
for
quantifying
their
effects
on
quality,
but
its
global
distribution
poorly
characterized.
We
developed
method
to
estimate
glass
transition
temperatures
based
the
molar
mass
molecular
O:C
ratio
components,
we
used
chemistry
model
EMAC
with
aerosol
module
ORACLE
predict
atmospheric
SOA.
For
planetary
boundary
layer,
simulations
indicate
that
mostly
liquid
tropical
polar
high
relative
humidity,
semi-solid
mid-latitudes
solid
over
dry
lands.
find
middle
upper
troposphere
should
be
glassy
state.
Thus,
slow
diffusion
water,
oxidants
molecules
could
kinetically
limit
gas-particle
interactions
free
troposphere,
promote
ice
nucleation
facilitate
long-range
transport
reactive
toxic
pollutants
embedded