Journal of Geophysical Research Atmospheres,
Год журнала:
2024,
Номер
129(2)
Опубликована: Янв. 13, 2024
Abstract
Arctic
clouds
are
sensitive
to
atmospheric
particles
since
these
sometimes
in
such
low
concentrations
that
cannot
always
form
under
supersaturated
water
vapor
conditions.
This
is
especially
true
the
late
summer,
when
aerosol
generally
very
high
Arctic.
The
environment
changes
rapidly
around
freeze‐up
as
open
waters
close
and
snow
starts
accumulating
on
ice.
We
investigated
droplet
formation
during
eight
significant
fog
events
central
Ocean,
north
of
80°,
from
August
12
19
September
2018
Ocean
expedition
onboard
icebreaker
Oden
.
Calculated
hygroscopicity
parameters
(
κ
)
for
entire
study
were
(up
=
0.85
±
0.13),
notably
after
freeze‐up,
suggesting
cloud
condensation
nuclei
(CCN)‐active.
At
least
one
showed
surface
able
persist
at
a
couple
hours
less
than
10
cm
−3
,
which
was
previously
suggested
be
minimum
formation.
Among
considered
limited
CCN,
effective
radii
larger
CCN
cases.
In
some
events,
residuals
did
not
reactivate
supersaturations
up
0.95%,
either
in‐droplet
reactions
decreased
hygroscopicity,
or
an
ambient
supersaturation
above
1%.
These
results
provide
insight
into
clean
late‐summer
fall
with
influence
continental
sources.
Atmospheric chemistry and physics,
Год журнала:
2025,
Номер
25(2), С. 1063 - 1104
Опубликована: Янв. 28, 2025
Abstract.
Lagrangian
tracer
simulations
are
deployed
to
investigate
processes
influencing
vertical
and
horizontal
dispersion
of
anthropogenic
pollution
in
Fairbanks,
Alaska,
during
the
Alaskan
Layered
Pollution
Chemical
Analysis
(ALPACA)
2022
field
campaign.
Simulated
concentrations
carbon
monoxide
(CO),
sulfur
dioxide
(SO2),
nitrogen
oxides
(NOx),
including
surface
elevated
sources,
highest
at
under
very
cold
stable
conditions.
enhancements
above
(50–300
m)
mainly
attributed
power
plant
emissions.
Both
sources
contribute
Fairbanks'
regional
that
is
transported
downwind,
primarily
south-west,
may
wintertime
Arctic
haze.
Inclusion
a
novel
plume
rise
treatment
considers
presence
temperature
inversion
layers
leads
improved
agreement
with
observed
CO
NOx
plumes,
discrepancies
to,
for
example,
displacement
plumes
by
modelled
winds.
At
surface,
model
results
show
variability
largely
driven
meteorology
and,
lesser
extent,
emissions,
although
simulated
tracers
sensitive
dispersion.
Modelled
underestimation
polluted
conditions
considerably
following
inclusion
substantial
increases
diesel
vehicle
emissions
temperatures
(e.g.
factor
6
−30
°C).
In
contrast,
overestimation
SO2
deficiencies
(5–18
space
heating
This
study
highlights
need
improvements
local
simulation
boundary
layers.
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Сен. 8, 2022
Abstract
Frequency
and
intensity
of
warm
moist
air-mass
intrusions
into
the
Arctic
have
increased
over
past
decades
been
related
to
sea
ice
melt.
During
our
year-long
expedition
in
remote
central
Ocean,
a
record-breaking
increase
temperature,
moisture
downwelling-longwave
radiation
was
observed
mid-April
2020,
during
an
intrusion
carrying
air
pollutants
from
northern
Eurasia.
The
two-day
intrusion,
caused
drastic
changes
aerosol
size
distribution,
chemical
composition
particle
hygroscopicity.
Here
we
show
how
transformed
low-particle
environment
area
comparable
central-European
urban
setting.
Additionally,
resulted
explosive
cloud
condensation
nuclei,
which
can
direct
effects
on
clouds’
radiation,
their
precipitation
patterns,
lifetime.
Thus,
unless
prompt
actions
significantly
reduce
emissions
source
regions
are
taken,
such
events
expected
continue
affect
climate.
Nature Geoscience,
Год журнала:
2023,
Номер
16(9), С. 768 - 774
Опубликована: Сен. 1, 2023
Abstract
The
Arctic
warms
nearly
four
times
faster
than
the
global
average,
and
aerosols
play
an
increasingly
important
role
in
climate
change.
In
Arctic,
sea
salt
is
a
major
aerosol
component
terms
of
mass
concentration
during
winter
spring.
However,
mechanisms
production
remain
unclear.
Sea
are
typically
thought
to
be
relatively
large
size
but
low
number
concentration,
implying
that
their
influence
on
cloud
condensation
nuclei
population
properties
generally
minor.
Here
we
present
observational
evidence
abundant
from
blowing
snow
central
Arctic.
Blowing
was
observed
more
20%
time
November
April.
sublimation
generates
high
concentrations
fine-mode
(diameter
below
300
nm),
enhancing
up
tenfold
above
background
levels.
Using
chemical
transport
model,
estimate
April
north
70°
N,
produced
accounts
for
about
27.6%
total
particle
number,
increases
longwave
emissivity
clouds,
leading
calculated
surface
warming
+2.30
W
m
−2
under
cloudy
sky
conditions.
Atmospheric chemistry and physics,
Год журнала:
2023,
Номер
23(1), С. 389 - 415
Опубликована: Янв. 11, 2023
Abstract.
The
Arctic
environment
is
rapidly
changing
due
to
accelerated
warming
in
the
region.
trend
driving
a
decline
sea
ice
extent,
which
thereby
enhances
feedback
loops
surface
energy
budget
Arctic.
aerosols
play
an
important
role
radiative
balance
and
hence
climate
response
region,
yet
direct
observations
of
over
Ocean
are
limited.
In
this
study,
we
investigate
annual
cycle
aerosol
particle
number
size
distribution
(PNSD),
concentration
(PNC),
black
carbon
(BC)
mass
central
during
Multidisciplinary
drifting
Observatory
for
Study
Climate
(MOSAiC)
expedition.
This
first
continuous,
year-long
data
set
PNSD
ever
collected
Ocean.
We
use
k-means
cluster
analysis,
FLEXPART
simulations,
inverse
modeling
evaluate
seasonal
patterns
influence
different
source
regions
on
population.
Furthermore,
compare
land-based
sites
across
Arctic,
using
both
long-term
measurements
year
MOSAiC
expedition
(2019–2020),
interannual
variability
give
context
characteristics
from
within
Our
analysis
identifies
that,
overall,
exhibits
typical
aerosols,
including
anthropogenic
haze
winter
secondary
processes
summer.
pattern
corresponds
global
radiation,
air
temperature,
timing
melting/freezing,
drive
changes
transport
processes.
winter,
Norilsk
region
Russia/Siberia
was
dominant
signals
BC
observations,
contributed
higher
accumulation-mode
PNC
concentrations
than
at
observatories.
also
show
that
wintertime
Oscillation
(AO)
phenomenon,
reported
achieve
record-breaking
positive
phase
January–March
2020,
explains
unusual
magnitude
compared
longer-term
observations.
summer,
PNCs
nucleation
Aitken
modes
enhanced;
however,
were
notably
lower
pack
further
south.
presented
herein
provides
current
snapshot
characterized
by
rapid
changes,
will
be
crucial
improving
model
predictions,
understanding
linkages
between
environmental
processes,
investigating
impacts
change
future
studies.
Atmospheric chemistry and physics,
Год журнала:
2025,
Номер
25(4), С. 2207 - 2241
Опубликована: Фев. 19, 2025
Abstract.
Aerosols
play
a
critical
role
in
the
Arctic's
radiative
balance,
influencing
solar
radiation
and
cloud
formation.
Limited
observations
central
Arctic
leave
gaps
understanding
aerosol
dynamics
year-round,
affecting
model
predictions
of
climate-relevant
properties.
Here,
we
present
first
annual
high-time-resolution
submicron
chemical
composition
during
Ocean
2018
(AO2018)
2019–2020
Multidisciplinary
drifting
Observatory
for
Study
Climate
(MOSAiC)
expeditions.
Seasonal
variations
mass
concentrations
were
found
to
be
driven
by
typical
seasonal
regimes
resemble
those
pan-Arctic
land-based
stations.
Organic
aerosols
dominated
pristine
summer,
while
anthropogenic
sulfate
prevailed
autumn
spring
under
haze
conditions.
Ammonium,
which
impacts
acidity,
was
consistently
less
abundant,
relative
sulfate,
compared
lower
latitudes
Arctic.
Cyclonic
(storm)
activity
have
significant
influence
on
variability
enhancing
emissions
from
local
sources
transport
remote
aerosol.
Local
wind-generated
particles
contributed
up
80
%
(20
%)
condensation
nuclei
population
(spring).
While
analysis
presented
herein
provides
current
baseline,
will
serve
improve
climate
region,
it
also
underscores
importance
integrating
short-timescale
processes,
such
as
wind-driven
blowing
snow
open
leads/ocean
simulations.
This
is
particularly
important,
given
decline
mid-latitude
increase
ones.
Atmospheric chemistry and physics,
Год журнала:
2022,
Номер
22(15), С. 9915 - 9947
Опубликована: Авг. 3, 2022
Abstract.
We
present
an
Arctic
aerosol
optical
depth
(AOD)
climatology
and
trend
analysis
for
2003–2019
spring
summertime
periods
derived
from
a
combination
of
multi-agency
reanalyses,
remote-sensing
retrievals,
ground
observations.
This
includes
the
U.S.
Navy
Aerosol
Analysis
Prediction
System
ReAnalysis
version
1
(NAAPS-RA
v1),
NASA
Modern-Era
Retrospective
Research
Applications,
2
(MERRA-2),
Copernicus
Atmosphere
Monitoring
Service
(CAMSRA).
Spaceborne
retrievals
AOD
are
considered
Moderate
Resolution
Imaging
Spectroradiometer
(MODIS),
Multi-angle
SpectroRadiometer
(MISR),
Cloud-Aerosol
Lidar
with
Orthogonal
Polarization
(CALIOP).
Ground-based
data
include
sun
photometer
AErosol
RObotic
NETwork
(AERONET)
sites
oceanic
Maritime
Network
(MAN)
measurements.
reanalysis
AODs
spaceborne
show
consistent
climatological
spatial
patterns
trends
both
summer
seasons
over
lower
(60–70∘
N).
Consistent
also
found
high
(north
70∘
N)
reanalyses.
The
reanalyses
yield
more
results
than
climate
models,
can
be
verified
well
AERONET,
corroborate
complementary
analysis.
Speciated
variable
total
among
three
little
so
March–May
(MAM)
June–August
(JJA).
Black
carbon
(BC)
in
comes
predominantly
biomass
burning
(BB)
sources
MAM
JJA,
BB
overwhelms
anthropogenic
JJA
study
period.
exhibits
multi-year
negative
positive
during
2003–2019,
due
to
overall
decrease
sulfate/anthropogenic
pollution
significant
increase
smoke.
Interannual
variability
is
significantly
large,
driven
by
fine-mode
and,
specifically,
smoke,
smoke
contribution
interannual
variation
larger
MAM.
It
recommended
that
models
should
account
emissions
variabilities
change
studies.
Communications Earth & Environment,
Год журнала:
2022,
Номер
3(1)
Опубликована: Сен. 19, 2022
Abstract
Summertime
wildfire
activity
is
increasing
in
boreal
forest
and
tundra
ecosystems
the
Northern
Hemisphere.
However,
impact
of
long
range
transport
deposition
aerosols
on
biogeochemical
cycles
Arctic
Ocean
unknown.
Here,
we
use
satellite-based
ocean
color
data,
atmospheric
modeling
back
trajectory
analysis
to
investigate
fate
emitted
from
Siberian
wildfires
summer
2014
their
potential
phytoplankton
dynamics
Ocean.
We
detect
large
blooms
near
North
Pole
(up
82°N
eastern
Eurasian
Basin).
Our
indicates
that
these
were
induced
by
northward
plume
nutrient-bearing
aerosols.
estimate
highly
stratified
surface
waters
received
amounts
wildfire-derived
nitrogen,
which
alleviated
nutrient
stress
community
triggered
an
unusually
bloom
event.
findings
suggest
changes
may
strongly
influence
summertime
productivity
Atmospheric chemistry and physics,
Год журнала:
2022,
Номер
22(9), С. 5775 - 5828
Опубликована: Май 4, 2022
Abstract.
While
carbon
dioxide
is
the
main
cause
for
global
warming,
modeling
short-lived
climate
forcers
(SLCFs)
such
as
methane,
ozone,
and
particles
in
Arctic
allows
us
to
simulate
near-term
health
impacts
a
sensitive,
pristine
region
that
warming
at
3
times
rate.
Atmospheric
critical
understanding
long-range
transport
of
pollutants
Arctic,
well
abundance
distribution
SLCFs
throughout
atmosphere.
Modeling
also
used
tool
determine
SLCF
on
present
future
emissions
scenarios.
In
this
study,
we
evaluate
18
state-of-the-art
atmospheric
Earth
system
models
by
assessing
their
representation
Northern
Hemisphere
distributions,
considering
wide
range
different
chemical
species
(methane,
tropospheric
ozone
its
precursors,
black
carbon,
sulfate,
organic
aerosol,
particulate
matter)
multiple
observational
datasets.
Model
simulations
over
4
years
(2008–2009
2014–2015)
conducted
2022
Monitoring
Assessment
Programme
(AMAP)
assessment
report
are
thoroughly
evaluated
against
satellite,
ground,
ship,
aircraft-based
observations.
The
annual
means,
seasonal
cycles,
3-D
distributions
were
using
several
metrics,
absolute
percent
model
biases
correlation
coefficients.
results
show
large
performance,
with
no
one
particular
or
type
performing
all
regions
species.
multi-model
mean
(mmm)
was
able
represent
general
features
had
best
overall
performance.
For
greatest
radiative
impact
(CH4,
O3,
BC,
SO42-),
mmm
within
±25
%
measurements
across
Hemisphere.
Therefore,
recommend
ensemble
be
simulating
SLCFs.
Of
our
smallest
CH4
OA.
most
SLCFs,
skewed
from
positive
negative
increasing
latitude.
Our
analysis
suggests
vertical
mixing,
transport,
deposition,
wildfires
remain
highly
uncertain
processes.
These
processes
need
better
improve
simulation
environment.
As
development
proceeds
these
areas,
evaluated,
information
improving
models.
npj Climate and Atmospheric Science,
Год журнала:
2022,
Номер
5(1)
Опубликована: Авг. 1, 2022
Abstract
The
Arctic
environment
has
changed
profoundly
in
recent
decades.
Aerosol
particles
are
involved
numerous
feedback
mechanisms
the
Arctic,
e.g.,
aerosol-cloud/radiation
interactions,
which
have
important
climatic
implications.
To
understand
changes
different
aerosol
types
and
number
concentrations,
we
performed
a
trend
analysis
of
particle
size
distributions,
their
properties,
associated
air
mass
history
at
Villum
Research
Station,
northeastern
Greenland,
from
2010
to
2018.
We
found
that,
during
spring,
total/ultrafine
mode
concentration
time
masses
spent
over
open
ocean
is
significantly
increasing,
can
be
ascribed
transport
patterns
changing
more
frequent
arrival
ice-free
Greenland
Sea.
summer,
concentration,
occurrence
Nucleation
cluster
(i.e.
newly
formed
gas
conversion),
increasing.
This
also
attributed
patterns,
here
with
arriving
frequently
Baffin
Bay.
Finally,
autumn,
ultrafine
Pristine
clean,
natural
background
conditions)
likely
due
increasing
amounts
accumulated
precipitation
along
trajectory
path
decreasing
above
mixed
layer,
respectively.
Our
results
demonstrate
that
circulation
factors
predominantly
affecting
trends
concentrations
Greenland.
Atmospheric chemistry and physics,
Год журнала:
2023,
Номер
23(8), С. 4741 - 4761
Опубликована: Апрель 20, 2023
Abstract.
Ice-nucleating
particles
(INPs)
can
initiate
ice
formation
in
clouds
at
temperatures
above
−38
∘C
through
heterogeneous
nucleation.
As
a
result,
INPs
affect
cloud
microphysical
and
radiative
properties,
lifetime,
precipitation
behavior
thereby
ultimately
the
Earth's
climate.
Yet,
little
is
known
regarding
sources,
abundance
properties
of
INPs,
especially
remote
regions
such
as
Arctic.
In
this
study,
2-year-long
INP
measurements
(from
July
2018
to
September
2020)
Villum
Research
Station
northern
Greenland
are
presented.
A
low-volume
filter
sampler
was
deployed
collect
samples
for
offline
analysis.
An
annual
cycle
concentration
(NINP)
observed,
fraction
heat-labile
found
be
higher
months
with
low
no
snow
cover
lower
when
surface
well
covered
(>
0.8
m).
Samples
were
categorized
into
three
different
types
based
only
on
slope
their
spectra,
namely
summer,
winter
mix
type.
For
each
temperature-dependent
parameterization
derived,
clearly
depending
time
year.
Winter
summer
occurred
during
respective
seasons
seen
60
%
time.
The
mixed
type
remaining
40
throughout
April,
May
November
transition
months.
case
study
comparing
April
2019
2020
performed.
month
selected
because
significant
difference
NINP
observed
these
two
periods,
2020.
parallel
differences
NINP,
also
cloud-ice
satellite
data
2020,
compared
2019.
period
revealed
clear
dependency
either
meteorological
parameters
or
which
passed
by
collected
air
masses.
Overall,
results
suggest
that
coastal
main
sources
most
likely
including
both
local
terrestrial
marine
sources.