Environmental Science & Technology Letters,
Год журнала:
2022,
Номер
9(10), С. 869 - 876
Опубликована: Авг. 29, 2022
The
record-setting
wildfires
that
ravaged
the
western
United
States
throughout
2020
released
high
concentrations
of
organic
carbon
(C)
into
environment,
including
adjacent
Pacific
Ocean.
Yet
little
is
known
about
fate
marine
wildfire-derived
C,
solubilized
as
dissolved
matter
(DOM),
despite
growing
observations
ash
deposition
in
such
systems.
We
sought
to
quantify
and
characterize
DOM
inputs
surface
waters
spanning
California
coastline
from
August
1
October
31,
2020.
Across
over
290
field
samples,
C
peaked
2-
4-fold
higher
after
eruption
fire
systems
than
immediate
pre-wildfire
levels.
were
well
correlated
with
atmospheric
pyrogenic
proxies
PM2.5
ozone,
supporting
sourcing.
Molecular
characterization
by
ultrahigh-resolution
FTICR-MS
revealed
both
a
diversity
formulas,
consensus
heterogeneity,
temporal
shifts
conserved
across
sites.
An
initial
increase
highly
aromatic,
oxygen-containing
compounds
aligned
concentrations,
burn
extent,
deposition.
Over
time,
transformation
increasingly
aliphatic
occurred.
latter
hypothesized
be
result
complex
interplay
between
biotic
abiotic
processes,
warranting
further
study.
Our
suggest
are
substantial
yet
dynamic
source
C.
Journal of Advances in Modeling Earth Systems,
Год журнала:
2024,
Номер
16(4)
Опубликована: Апрель 1, 2024
Abstract
We
present
a
variable‐resolution
global
chemistry‐climate
model
(AM4VR)
developed
at
NOAA's
Geophysical
Fluid
Dynamics
Laboratory
(GFDL)
for
research
the
nexus
of
US
climate
and
air
quality
extremes.
AM4VR
has
horizontal
resolution
13
km
over
US,
allowing
it
to
resolve
urban‐to‐rural
chemical
regimes,
mesoscale
convective
systems,
land‐surface
heterogeneity.
With
gradually
reducing
100
Indian
Ocean,
we
achieve
multi‐decadal
simulations
driven
by
observed
sea
surface
temperatures
50%
computational
cost
25‐km
uniform‐resolution
grid.
In
contrast
with
GFDL's
AM4.1
contributing
sixth
Coupled
Model
Intercomparison
Project
resolution,
features
much
improved
mean
patterns
variability.
particular,
shows
representation
of:
precipitation
seasonal‐to‐diurnal
cycles
extremes,
notably
central
dry‐and‐warm
bias;
western
snowpack
summer
drought,
implications
wildfires;
North
American
monsoon,
affecting
dust
storms.
exhibits
excellent
winter
precipitation,
pollution
meteorology
in
California
complex
terrain,
enabling
skillful
prediction
both
extreme
ozone
haze
events
Central
Valley.
also
provides
vast
improvements
process‐level
representations
biogenic
volatile
organic
compound
emissions,
interactive
emissions
from
land,
removal
pollutants
terrestrial
ecosystems.
highlight
value
increased
representing
climate–air
interactions
through
land‐biosphere
feedbacks.
offers
novel
opportunity
study
dimensions
quality,
especially
role
Earth
system
feedbacks
changing
climate.
Geophysical Research Letters,
Год журнала:
2024,
Номер
51(15)
Опубликована: Авг. 6, 2024
Abstract
Quantifying
the
variable
impacts
of
wildfire
smoke
on
ozone
air
quality
is
challenging.
Here
we
use
airborne
measurements
from
2018
Western
Wildfire
Experiment
for
Cloud
Chemistry,
Aerosol
Absorption,
and
Nitrogen
(WE‐CAN)
to
parameterize
emissions
reactive
nitrogen
(NO
y
)
wildfires
into
peroxyacetyl
nitrate
(PAN;
37%),
NO
3
−
(27%),
(36%)
in
a
global
chemistry‐climate
model
with
13
km
spatial
resolution
over
contiguous
US.
The
partitioning,
compared
emitting
all
as
NO,
reduces
bias
near‐fire
plumes
sampled
by
aircraft
enhances
downwind
5–10
ppbv
when
Canadian
travel
Washington,
Utah,
Colorado,
Texas.
Using
multi‐platform
observations,
identify
smoke‐influenced
days
daily
maximum
8‐hr
average
(MDA8)
70–88
Kennewick,
Salt
Lake
City,
Denver
Dallas.
On
these
days,
enhanced
MDA8
5–25
ppbv,
through
produced
remotely
during
plume
transport
locally
via
interactions
urban
emissions.
Environmental Science & Technology,
Год журнала:
2022,
Номер
56(3), С. 1557 - 1567
Опубликована: Янв. 17, 2022
In
the
western
United
States,
number
and
severity
of
large
wildfires
have
been
growing
for
decades.
Biomass
burning
(BB)
is
a
major
source
volatile
organic
compounds
(VOCs)
to
atmosphere
both
globally
regionally.
Following
emission,
BB
VOCs
are
oxidized
while
being
transported
downwind,
producing
ozone,
secondary
aerosols,
hazardous
VOCs.
this
research,
we
measured
using
proton
transfer
reaction
time-of-flight
mass
spectrometry
(PTR-ToF-MS)
in
an
urban
area
55–65
km
downwind
October
2017
Northern
California
wildfires.
Nonaromatic
oxygenated
were
dominant
component
measured.
smoke
plumes,
account
70–75%
total
observed
carbon,
with
remainder
particulate
matter
(with
diameter
<2.5
μm,
PM2.5).
We
show
that
correlation
furan
(primary
VOC)
maleic
anhydride
(secondary
can
indicate
origin
This
was
further
confirmed
by
diurnal
variations
their
concentration-weighted
trajectories.
Oxidation
during
transport
consumed
highly
reactive
including
benzenoids,
furanoids,
terpenoids
produced
more
Furthermore,
wildfire
altered
ozone
formation
regime
raised
O3
levels
San
Francisco
Bay
Area.
Environmental Science & Technology Letters,
Год журнала:
2022,
Номер
9(10), С. 869 - 876
Опубликована: Авг. 29, 2022
The
record-setting
wildfires
that
ravaged
the
western
United
States
throughout
2020
released
high
concentrations
of
organic
carbon
(C)
into
environment,
including
adjacent
Pacific
Ocean.
Yet
little
is
known
about
fate
marine
wildfire-derived
C,
solubilized
as
dissolved
matter
(DOM),
despite
growing
observations
ash
deposition
in
such
systems.
We
sought
to
quantify
and
characterize
DOM
inputs
surface
waters
spanning
California
coastline
from
August
1
October
31,
2020.
Across
over
290
field
samples,
C
peaked
2-
4-fold
higher
after
eruption
fire
systems
than
immediate
pre-wildfire
levels.
were
well
correlated
with
atmospheric
pyrogenic
proxies
PM2.5
ozone,
supporting
sourcing.
Molecular
characterization
by
ultrahigh-resolution
FTICR-MS
revealed
both
a
diversity
formulas,
consensus
heterogeneity,
temporal
shifts
conserved
across
sites.
An
initial
increase
highly
aromatic,
oxygen-containing
compounds
aligned
concentrations,
burn
extent,
deposition.
Over
time,
transformation
increasingly
aliphatic
occurred.
latter
hypothesized
be
result
complex
interplay
between
biotic
abiotic
processes,
warranting
further
study.
Our
suggest
are
substantial
yet
dynamic
source
C.