Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(12), P. 7253 - 7260
Published: June 25, 2024
Abstract.
Cloud
albedo
susceptibility
to
droplet
number
perturbation
remains
a
source
of
uncertainty
in
understanding
aerosol–cloud
interactions
and
thus
both
past
present
climate
states.
Through
the
Energy
Exascale
Earth
System
Model
(E3SM)
v2
experiments,
we
probe
effects
competing
processes
on
cloud
low-lying
marine
stratocumulus
northeast
Pacific.
In
present-day
conditions,
find
that
increasing
precipitation
suppression
by
aerosols
increases
susceptibility,
whereas
sedimentation
decreases
it.
By
constructing
hypothetical
model
configuration
exhibiting
negative
under
all
conclude
change
due
aerosol
cannot
be
predicted
co-variabilities
E3SM
v2.
As
such,
our
null
result
herein
challenges
assumption
observations
are
sufficient
constrain
states,
at
least
context
changes
perturbation.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(18), P. 12221 - 12239
Published: Sept. 21, 2022
Abstract.
Anthropogenic
aerosols
exert
a
cooling
influence
that
offsets
part
of
the
greenhouse
gas
warming.
Due
to
their
short
tropospheric
lifetime
only
several
days,
aerosol
forcing
responds
quickly
emissions.
Here,
we
present
and
discuss
evolution
since
2000.
There
are
multiple
lines
evidence
allow
us
robustly
conclude
anthropogenic
effective
radiative
(ERF)
–
both
aerosol–radiation
interactions
(ERFari)
aerosol–cloud
(ERFaci)
has
become
less
negative
globally,
i.e.
trend
in
changed
sign
from
positive.
Bottom-up
inventories
show
primary
precursor
emissions
declined
most
regions
world;
observations
related
burden
declining
trends,
particular
fine-mode
particles
make
up
aerosols;
satellite
retrievals
cloud
droplet
numbers
trends
with
declines
consistent
these
sign,
as
do
top-of-atmosphere
radiation.
Climate
model
results,
including
revised
set
is
constrained
by
ocean
heat
content
magnitude
for
positive
relative
year
2000
due
reduced
effects.
This
reduction
leads
an
acceleration
climate
change,
increase
0.1
0.3
W
m−2,
12
%
total
2019
compared
1750
according
Intergovernmental
Panel
on
Change
(IPCC).
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(12)
Published: March 20, 2024
Marine
cloud
brightening
(MCB)
is
the
deliberate
injection
of
aerosol
particles
into
shallow
marine
clouds
to
increase
their
reflection
solar
radiation
and
reduce
amount
energy
absorbed
by
climate
system.
From
physical
science
perspective,
consensus
a
broad
international
group
scientists
that
viability
MCB
will
ultimately
depend
on
whether
observations
models
can
robustly
assess
scale-up
local-to-global
in
today's
identify
strategies
ensure
an
equitable
geographical
distribution
benefits
risks
associated
with
projected
regional
changes
temperature
precipitation.
To
address
knowledge
gaps
required
societal
implications
MCB,
we
propose
substantial
targeted
program
research-field
laboratory
experiments,
monitoring,
numerical
modeling
across
range
scales.
Annual Review of Earth and Planetary Sciences,
Journal Year:
2023,
Volume and Issue:
51(1), P. 447 - 470
Published: Feb. 8, 2023
As
atmospheric
carbon
dioxide
concentrations
rise
and
climate
change
becomes
more
destructive,
geoengineering
has
become
a
subject
of
serious
consideration.
By
reflecting
fraction
incoming
sunlight,
solar
could
cool
the
planet
quickly,
but
with
uncertain
effects
on
regional
climatology,
particularly
hydrological
patterns.
Here,
we
review
recent
work
projected
hydrologic
outcomes
geoengineering,
in
context
robust
literature
responses
to
change.
While
most
approaches
are
expected
weaken
global
cycle,
will
vary
based
implementation
method
strategy.
The
impacts
demonstrates
that
its
implications
for
human
welfare
depend
assumptions
about
underlying
social
conditions
objectives
intervention
as
well
lens
through
which
interpreted.
We
conclude
suggestions
reduce
decision-relevant
uncertainties
this
novel
field
Earth
science
inquiry.
▪The
reducing
insolation
among
consequential
(SG).▪Theoretical
frameworks
from
broader
can
help
explain
SG's
precipitation,
relative
humidity,
other
aspects
hydroclimate.▪The
state
knowledge
SG
is
unevenly
concentrated
regions.▪Projected
scenario
dependent
difficult
characterize
either
harmful
or
beneficial.
Abstract
Reduction
in
aerosol
cooling
unmasks
greenhouse
gas
warming,
exacerbating
the
rate
of
future
warming.
The
strict
sulfur
regulation
on
shipping
fuel
implemented
2020
(IMO2020)
presents
an
opportunity
to
assess
potential
impacts
such
emission
regulations
and
detectability
deliberate
perturbations
for
climate
intervention.
Here
we
employ
machine
learning
capture
cloud
natural
variability
estimate
a
radiative
forcing
+0.074
±0.005
W
m
−2
related
IMO2020
associated
with
changes
shortwave
effect
over
three
low-cloud
regions
where
routes
prevail.
We
find
low
this
event,
attributed
strong
albedo
cover.
Regionally,
is
higher
southeastern
Atlantic
stratocumulus
deck.
These
results
raise
concerns
that
reductions
emissions
will
accelerate
warming
proposed
as
marine
brightening
need
be
substantial
order
overcome
detectability.
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(4)
Published: Feb. 12, 2025
Abstract
This
study
estimates
the
meteorological
covariations
of
aerosol
and
marine
boundary
layer
(MBL)
cloud
properties
in
eastern
North
Atlantic
(ENA)
region,
characterized
by
diverse
synoptic
conditions.
Using
a
deep‐learning‐based
clustering
model
with
mid‐level
surface
daily
data,
we
identify
seven
distinct
regimes
during
summer
from
2016
to
2021.
Our
analysis,
incorporating
reanalysis
data
satellite
retrievals,
shows
that
aerosols
MBL
clouds
exhibit
clear
regime‐dependent
characteristics,
whereas
lower
tropospheric
do
not.
discrepancy
likely
arises
determined
large‐scale
conditions,
which
may
overlook
air
mass
histories
predominantly
dictate
Focusing
on
three
dominated
northerly
winds,
analyze
Atmospheric
Radiation
Measurement
Program
(ARM)
ENA
observations
Graciosa
Island
Azores.
In
subtropical
anticyclone
regime,
fewer
cumulus
more
single‐layer
stratocumulus
light
drizzle
are
observed,
along
highest
droplet
number
concentration
(Nd),
condensation
nuclei
(CCN)
levels.
The
post‐trough
regime
features
broken
or
multi‐layer
slightly
higher
rain
rate,
Nd
CCN
weak
trough
is
deepest
clouds,
primarily
strongest
rate
lowest
Nd,
levels,
indicating
strong
wet
scavenging.
These
findings
highlight
importance
considering
covariation
driven
when
assessing
indirect
effects
using
observations.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(13), P. 9129 - 9160
Published: July 14, 2022
Abstract.
The
effective
radiative
forcing
of
anthropogenic
aerosols
(ERFaer)
is
an
important
measure
the
aerosol
effects
simulated
by
a
global
climate
model.
Here
we
analyze
ERFaer
E3SM
version
1
(E3SMv1)
atmospheric
model
using
both
century-long
free-running
atmosphere–land
simulations
and
short
nudged
simulations.
We
relate
to
characteristics
composition
optical
properties,
evaluate
relationships
between
key
cloud
properties.
In
terms
historical
changes
from
year
1870
2014,
our
results
show
that
mean
burden
depth
increase
during
simulation
period
as
expected,
but
regional
averages
large
differences
in
temporal
evolution.
largest
are
found
emission-induced
evolution
sulfate
aerosol:
strong
decreasing
trend
seen
Northern
Hemisphere
high-latitude
region
after
around
1970,
while
continued
tropics.
properties
(relative
pre-industrial
present-day
conditions)
also
evident
diverging
linear
exhibited
for
1870–1969.
addition
relationships,
reduced
sensitivity
droplet
number
other
perturbations
when
perturbation
large.
Consequently,
annual
magnitude
does
not
1970.
E3SMv1
relatively
compared
recently
published
multi-model
estimates;
primary
reason
indirect
effect
(i.e.,
through
aerosol–cloud
interactions).
Compared
models,
features
relative
radius
response
perturbations.
Large
liquid
depth,
which
determined
water
path.
Aerosol-induced
ice
have
correlation,
affects
formation
homogeneous
nucleation
cirrus
clouds
(that
causes
on
longwave
ERFaer).
As
suggested
previous
study,
appears
be
one
reasons
why
cannot
reproduce
observed
temperature
second
half
20th
century.
Sensitivity
performed
understand
parameterization
and/or
parameter
impact
ERFaer.
estimates
shortwave
components
sensitive
processes.
When
processes
modified,
top-of-model
largely
offset
each
other,
so
net
negligible.
This
suggests
that,
reduce
ERFaer,
it
would
more
or
mixed-phase
clouds.
Geophysical Research Letters,
Journal Year:
2023,
Volume and Issue:
50(2)
Published: Jan. 18, 2023
Abstract
A
supervised
neural
network
algorithm
is
used
to
categorize
near‐global
satellite
retrievals
into
three
mesoscale
cellular
convective
(MCC)
cloud
morphology
patterns.
At
constant
amount,
patterns
differ
in
brightness
associated
with
the
amount
of
optically
thin
features.
Environmentally
driven
transitions
from
closed
MCC
other
patterns,
typically
accompanied
by
more
features,
are
as
a
framework
quantify
contribution
optical
depth
component
shortwave
feedback.
marine
heat
wave
an
out‐of‐sample
test
occurrence
predictions.
Morphology
shifts
between
65°S
and
65°N
under
projected
environmental
changes
(i.e.,
abrupt
quadrupling
CO
2
)
assuming
cover
contributes
0.04
0.07
W
m
−2
K
−1
(aggregate
0.06)
global
mean
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(2), P. 1073 - 1090
Published: Jan. 20, 2023
Abstract.
Marine
stratocumuli
cool
the
Earth
effectively
due
to
their
high
reflectance
of
incoming
solar
radiation
and
persistent
occurrence.
The
susceptibility
cloud
albedo
droplet
number
concentration
perturbations
depends
strongly
on
large-scale
meteorological
conditions.
Studies
focused
dependence
adjustments
often
overlook
covariability
among
factors
geographical
temporal
variability.
We
use
8
years
satellite
observations
sorted
by
day
location
show
global
distribution
marine
low-cloud
susceptibility.
find
an
overall
brightening
potential
for
most
warm
clouds,
which
is
more
pronounced
over
subtropical
coastal
regions.
A
weak
darkening
in
annual
mean
evident
remote
SE
Pacific
Atlantic.
that
fields
from
ERA5
reanalysis
data,
including
lower-tropospheric
stability,
free-tropospheric
relative
humidity,
sea
surface
temperature,
boundary
layer
depth,
have
distinct
covariabilities
each
eastern
ocean
basins
where
prevail.
This
leads
a
markedly
different
cycle
basin.
Moreover,
we
basin-specific
regional
relationships
between
key
susceptibilities
are
absent
analysis.
Our
results
stress
importance
considering
distinctiveness
when
scaling
up
local-to-global
response
aerosol
perturbations.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(2), P. 1345 - 1368
Published: Jan. 25, 2023
Abstract.
Ship
tracks
in
subtropical
marine
low
clouds
are
simulated
and
investigated
using
large-eddy
simulations.
Five
variants
of
a
shallow
stratocumulus-topped
boundary
layer
(MBL)
chosen
to
span
range
background
aerosol
concentrations
variations
free-tropospheric
moisture.
Idealized
time-invariant
meteorological
forcings
approximately
steady-state
constitute
the
conditions.
We
investigate
processes
controlling
cloud
microphysical,
macrophysical,
radiative
responses
injections.
For
analysis,
we
use
novel
methods
decompose
liquid
water
path
(LWP)
adjustment
into
changes
boundary-layer
properties
effect
(CRE)
contributions
from
macro-
microphysics.
The
key
results
that
(a)
cloud-top
entrainment
rate
increases
all
cases,
with
stronger
for
thicker
than
thinner
clouds;
(b)
drying
warming
induced
by
increased
is
offset
differing
degrees
corresponding
surface
fluxes,
precipitation,
radiation;
(c)
MBL
turbulence
responds
caused
perturbation,
this
significantly
affects
macrophysics;
(d)
across
2
d
simulation,
were
brightened
cases.
In
pristine
MBL,
significant
drizzle
suppression
injections
not
only
greater
retention
but
also
intensification,
leading
increase
amount.
case,
Twomey
brightening
strongly
augmented
an
thickness
cover.
addition,
reduction
loss
through
coalescence
scavenging
more
offsets
dilution.
This
interplay
precludes
estimation
lifetime
perturbation.
combined
microphysics
lead
10–100
times
effective
these
cases
relative
those
non-precipitating
moderate
polluted
MBLs,
enhancement
makes
drier,
warmer,
stratified,
decrease
thickness.
LWP
response
greatest
fraction
moderately
moist
free
troposphere.
finding
differs
previous
studies
found
larger
drier
troposphere,
it
initially
clouds,
so
offsetting
effects
weaker.
injected
MBLs
estimated
be
2–3
d,
which
much
longer
estimates
typical
ship
track
lifetimes
satellite
images.