Journal of Geophysical Research Atmospheres,
Journal Year:
2024,
Volume and Issue:
129(14)
Published: July 23, 2024
Abstract
In
the
context
of
China's
“dual
carbon”
goal,
emissions
air
pollutants
are
expected
to
significantly
decrease
in
future.
Thus,
direct
climate
effects
black
carbon
(BC)
aerosols
East
Asia
investigated
under
this
goal
using
an
updated
regional
and
chemistry
model.
The
simulated
annual
average
BC
concentration
over
is
approximately
1.29
μg/m
3
last
decade.
Compared
those
2010–2020,
both
column
burden
instantaneous
radiative
forcing
by
more
than
55%
80%,
respectively,
peak
year
(2030s)
neutrality
(2060s).
Conversely,
effective
(ERF)
responses
exhibit
substantial
nonlinearity
emission
reduction,
possibly
resulting
from
different
adjustments
thermal‐dynamic
fields
clouds
BC‐radiation
interactions.
mean
ERF
at
tropopause
+1.11
W/m
2
2010–2020
while
negative
2060s.
interactions
present‐day
impose
a
significant
cooling
−0.2
−0.5
K
central
China
but
warming
+0.3
Tibetan
Plateau.
As
decline,
surface
temperature
show
mixed
picture
compared
with
eastern
Tibet
−0.3
2030s,
Indian
might
play
important
role
Asian
reduction
China.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(16), P. 10787 - 10800
Published: Aug. 27, 2019
Abstract.
The
high
aerosol
concentration
(AC)
over
eastern
China
has
attracted
attention
from
both
science
and
society.
Based
on
the
simulations
of
a
chemical
transport
model
using
fixed
emissions
level,
possible
impact
previous
autumn
North
Atlantic
Oscillation
(NAO)
combined
with
simultaneous
El
Niño–Southern
(ENSO)
boreal
winter
AC
is
investigated.
We
find
that
NAO
only
manifests
its
negative
impacts
during
phase
central
China,
significant
positive
influence
distribution
observed
south
warm
events
ENSO.
occurs
via
an
anomalous
sea
surface
temperature
tripole
pattern
by
which
teleconnection
wave
train
induced
results
in
convergence
China.
In
contrast,
occurrence
ENSO
may
induce
shift
western
Pacific
subtropical
result
southwesterlies
circulations
associated
Niño
are
not
favorable
for
correspond
to
worsening
air
conditions
highlight
fact
effects
tropical
extratropical
systems
play
considerable
role
affecting
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(8), P. 4999 - 5017
Published: April 28, 2020
Abstract.
Recent
studies
suggested
significant
impacts
of
boreal
cryosphere
changes
on
wintertime
air
stagnation
and
haze
pollution
extremes
in
China.
However,
the
underlying
mechanisms
such
a
teleconnection
relationship
remains
unclear.
Here
we
use
Whole
Atmosphere
Community
Climate
Model
(WACCM)
to
investigate
dynamic
processes
leading
atmospheric
circulation
responses
Arctic
sea
ice
changes.
We
conduct
four
climate
sensitivity
experiments
by
perturbing
concentrations
(SIC)
corresponding
surface
temperature
(SST)
autumn
early
winter
over
whole
three
subregions
model.
The
results
indicate
distinct
patterns
regional
ventilation
region-specific
changes,
with
largest
increase
both
probability
(by
132
%)
intensity
30
monthly
being
found
experiment
driven
SIC
SST
Pacific
sector
(the
East
Siberian
Chukchi
seas).
increased
are
mainly
an
amplified
planetary-scale
pattern
that
resembles
negative
phase
Eurasian
(EU)
pattern.
Dynamical
diagnostics
suggest
convergence
transient
eddy
forcing
vicinity
Scandinavia
is
largely
responsible
for
amplification
Transient
vorticity
fluxes
dominate
produce
barotropic
anticyclonic
anomaly
near
wave
train
propagation
across
Eurasia
downstream
regions
Asia.
piecewise
potential
inversion
analysis
reveals
this
long-range
origin
takes
place
primarily
via
middle
upper
troposphere.
anomalous
ridge
Asia
troposphere
worsens
conditions
weakening
monsoon
northwesterlies
enhancing
inversions
surface,
more
stronger
eastern
China
winter.
Ensemble
projections
based
state-of-the-art
models
Coupled
Intercomparison
Project
Phase
6
(CMIP6)
corroborate
between
high-latitude
environmental
midlatitude
weather
extremes,
though
tendency
magnitude
vary
considerably
among
each
participating
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(2)
Published: Jan. 18, 2025
Abstract
Pollutant
emissions
in
China
have
significantly
decreased
over
the
past
decade
and
are
expected
to
continue
declining
future.
Aerosols,
as
important
pollutants
short‐lived
climate
forcing
agents,
significant
but
currently
unclear
impacts
East
Asia
their
concentrations
decrease
until
mid‐century.
Here,
we
employ
a
well‐developed
regional
model
RegCM4
combined
with
future
pollutant
emission
inventories,
which
more
representative
of
investigate
changes
effects
major
anthropogenic
aerosols
under
six
different
reduction
scenarios
(1.5°C
goals,
Neutral‐goals,
2°C
‐goals,
NDC‐goals,
Current‐goals,
Baseline).
By
2060s,
aerosol
surface
these
projected
by
89%,
87%,
84%,
73%,
65%,
21%,
respectively,
compared
those
2010–2020.
Aerosol
effect
associated
its
loadings
not
linear
manner.
The
average
effective
radiative
at
induced
aerosol‐radiation‐cloud
interactions
will
diminish
24%
±
13%
2030s
35%
2060s.
These
alternations
caused
reductions
lead
increases
near‐surface
temperatures
precipitations.
Specifically,
aerosol‐induced
temperature
precipitation
responses
estimated
change
−78%
−20%
−69%
77%,
goals
2060s
Therefore,
resulting
from
substantial
need
be
fully
considered
pathway
toward
carbon
neutrality.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(11), P. 7759 - 7774
Published: June 12, 2019
Abstract.
Aerosols
can
not
only
participate
in
fog
formation
by
acting
as
condensation
nuclei
of
droplets
but
also
modify
the
meteorological
conditions
such
air
temperature
and
moisture,
planetary
boundary
layer
height
(PBLH)
regional
circulation
during
haze
events.
The
impact
aerosols
on
formation,
yet
to
be
revealed,
critical
understanding
predicting
fog–haze
In
this
study,
we
used
Weather
Research
Forecasting
model
coupled
with
Chemistry
(WRF-Chem)
investigate
a
heavy
event
multiday
intense
pollution
episode
early
December
2013
Yangtze
River
Delta
(YRD)
region
eastern
China.
Using
WRF-Chem
model,
conducted
four
parallel
numerical
experiments
evaluate
roles
aerosol–radiation
interaction
(ARI),
aerosol–cloud
(ACI),
black
carbon
(BC)
non-BC
maintenance
event.
We
find
that
when
aerosols'
feedback
processes
are
considered
capture
well.
And
effects
ARI
played
dominant
role,
while
ACI
were
negligible.
Furthermore,
our
analyses
show
BC
was
more
important
inducing
YRD
7
than
aerosols.
dome
effect
leads
an
increase
moisture
over
sea
reducing
PBLH
weakening
vertical
mixing,
thereby
confining
water
vapor
near-surface
layer.
strengthened
daytime
onshore
flow
cyclonic
wind
anomaly,
induced
contrast
perturbation
land
sea,
transported
moister
region,
where
suppressed
weakened
mixing
maintained
high
level.
Then
formed
due
surface
cooling
at
night.
This
study
highlights
importance
anthropogenic
emissions
advection–radiation
polluted
coastal
areas.
Journal of Geophysical Research Atmospheres,
Journal Year:
2019,
Volume and Issue:
124(8), P. 4567 - 4583
Published: April 9, 2019
Abstract
High‐impact
poor
air
quality
events,
such
as
Beijing's
so‐called
“Airpocalypse”
in
January
2013,
demonstrate
that
short‐lived
events
can
have
significant
effects
on
health
and
economic
vitality.
Poor
result
from
the
combination
of
emission
pollutants
meteorological
conditions
favorable
to
their
accumulation,
which
include
limited
scavenging,
dispersion,
ventilation.
The
unprecedented
nature
2013
Airpocalypse,
conjunction
with
our
nonstationary
climate,
motivate
an
assessment
whether
climate
change
has
altered
conducive
winter
Beijing.
Using
three
indices
designed
quantify
support
drawing
attribution
methods
Diffenbaugh
et
al.
(2017,
https://doi.org/10.1073/pnas.1618082114
),
we
assess
(
i
)
contribution
observed
trends
magnitude
ii
probability
iii
return
interval
observational
record,
preindustrial
model‐simulated
historical
iv
trend
climates,
v
relative
influences
anthropogenic
forcing
natural
variability
trend.
We
find
influence
had
a
small
effect
event
all
but
increased
long‐term
positive
two
out
indices.
This
work
provides
framework
for
both
further
understanding
role
expanding
scope
attribution.