Earth system science data,
Journal Year:
2023,
Volume and Issue:
15(8), P. 3747 - 3760
Published: Aug. 22, 2023
Abstract.
We
present
a
global
multiyear
height-resolved
data
set
of
aerosol-type-specific
cloud
condensation
nuclei
concentrations
(nCCN)
estimated
from
the
spaceborne
lidar
aboard
Cloud-Aerosol
Lidar
and
Infrared
Pathfinder
Satellite
Observation
(CALIPSO)
satellite.
For
estimating
nCCN,
we
apply
recently
introduced
Optical
Modelling
CALIPSO
Aerosol
Microphysics
(OMCAM)
algorithm
to
Level
2
Profile
product.
The
nCCN
are
then
gridded
into
uniform
latitude–longitude
grid
2∘×5∘,
vertical
resolution
60
m
surface
an
altitude
8
km,
temporal
1
month.
span
total
186
months,
June
2006
December
2021.
In
addition,
provide
3D
climatology
produced
using
complete
time
series.
further
highlight
some
potential
applications
in
context
aerosol–cloud
interactions.
can
be
accessed
at
https://doi.org/10.1594/PANGAEA.956215
(Choudhury
Tesche,
2023).
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).
The Innovation,
Journal Year:
2024,
Volume and Issue:
5(5), P. 100691 - 100691
Published: Aug. 23, 2024
Public
summary•What
does
AI
bring
to
geoscience?
has
been
accelerating
and
deepening
our
understanding
of
Earth
Systems
in
an
unprecedented
way,
including
the
atmosphere,
lithosphere,
hydrosphere,
cryosphere,
biosphere,
anthroposphere
interactions
between
spheres.•What
are
noteworthy
challenges
As
we
embrace
huge
potential
geoscience,
several
arise
reliability
interpretability,
ethical
issues,
data
security,
high
demand
cost.•What
is
future
The
synergy
traditional
principles
modern
AI-driven
techniques
holds
immense
promise
will
shape
trajectory
geoscience
upcoming
years.AbstractThis
paper
explores
evolution
geoscientific
inquiry,
tracing
progression
from
physics-based
models
data-driven
approaches
facilitated
by
significant
advancements
artificial
intelligence
(AI)
collection
techniques.
Traditional
models,
which
grounded
physical
numerical
frameworks,
provide
robust
explanations
explicitly
reconstructing
underlying
processes.
However,
their
limitations
comprehensively
capturing
Earth's
complexities
uncertainties
pose
optimization
real-world
applicability.
In
contrast,
contemporary
particularly
those
utilizing
machine
learning
(ML)
deep
(DL),
leverage
extensive
glean
insights
without
requiring
exhaustive
theoretical
knowledge.
ML
have
shown
addressing
science-related
questions.
Nevertheless,
such
as
scarcity,
computational
demands,
privacy
concerns,
"black-box"
nature
hinder
seamless
integration
into
geoscience.
methodologies
hybrid
presents
alternative
paradigm.
These
incorporate
domain
knowledge
guide
methodologies,
demonstrate
enhanced
efficiency
performance
with
reduced
training
requirements.
This
review
provides
a
comprehensive
overview
research
paradigms,
emphasizing
untapped
opportunities
at
intersection
advanced
It
examines
major
showcases
advances
large-scale
discusses
prospects
that
landscape
outlines
dynamic
field
ripe
possibilities,
poised
unlock
new
understandings
further
advance
exploration.Graphical
abstract
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.
Nature Geoscience,
Journal Year:
2024,
Volume and Issue:
17(5), P. 404 - 410
Published: April 11, 2024
Abstract
With
global
warming
currently
standing
at
approximately
+1.2
°C
since
pre-industrial
times,
climate
change
is
a
pressing
issue.
Marine
cloud
brightening
one
proposed
method
to
tackle
through
injecting
aerosols
into
marine
clouds
enhance
their
reflectivity
and
thereby
planetary
albedo.
However,
because
it
unclear
how
influence
clouds,
especially
cover,
both
projections
the
effectiveness
of
remain
uncertain.
Here
we
use
satellite
observations
volcanic
eruptions
in
Hawaii
quantify
aerosol
fingerprint
on
tropical
clouds.
We
observe
large
enhancement
reflected
sunlight,
mainly
due
an
aerosol-induced
increase
cover.
This
observed
strong
negative
forcing
suggests
that
current
level
driven
by
weaker
net
radiative
than
previously
thought,
arising
from
competing
effects
greenhouse
gases
aerosols.
implies
greater
sensitivity
Earth’s
therefore
larger
response
rising
gas
concentrations
reductions
atmospheric
air
quality
measures.
our
findings
also
indicate
mitigation
via
plausible
most
effective
humid
stable
conditions
tropics
where
solar
radiation
strong.
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(46)
Published: Nov. 7, 2022
How
clouds
respond
to
anthropogenic
sulfate
aerosols
is
one
of
the
largest
sources
uncertainty
in
radiative
forcing
climate
over
industrial
era.
This
limits
our
ability
predict
equilibrium
sensitivity
(ECS)-the
global
warming
following
a
doubling
atmospheric
CO2.
Here,
we
use
satellite
observations
quantify
relationships
between
and
low-level
while
carefully
controlling
for
meteorology.
We
then
combine
with
estimates
change
concentration
since
about
1850
constrain
associated
forcing.
estimate
that
cloud-mediated
from
[Formula:
see
text]
W
m-2
ocean
(95%
confidence).
constraint
implies
ECS
likely
2.9
4.5
K
(66%
Our
results
indicate
aerosol
less
uncertain
probably
larger
than
ranges
proposed
by
recent
assessments.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Nov. 8, 2023
Abstract
In
the
latter
half
of
twentieth
century,
a
significant
climate
phenomenon
“diurnal
asymmetric
warming”
emerged,
wherein
global
land
surface
temperatures
increased
more
rapidly
during
night
than
day.
However,
recent
episodes
brightening
and
regional
droughts
heatwaves
have
brought
notable
alterations
to
this
warming
trend.
Here,
we
re-evaluate
sub-diurnal
temperature
patterns,
revealing
substantial
increase
in
rates
daily
maximum
(T
max
),
while
minimum
remained
relatively
stable.
This
shift
has
resulted
reversal
diurnal
trend,
expanding
range
over
decades.
The
intensified
T
is
attributed
widespread
reduction
cloud
cover,
which
led
solar
irradiance
at
surface.
Our
findings
underscore
urgent
need
for
enhanced
scrutiny
trends
their
implications
wider
earth
system.
Science Advances,
Journal Year:
2023,
Volume and Issue:
9(45)
Published: Nov. 8, 2023
Aerosols
cool
Earth's
climate
indirectly
by
increasing
low
cloud
brightness
and
their
coverage
(Cf),
constituting
the
aerosol
indirect
forcing
(AIF).
The
partially
offsets
greenhouse
warming
positively
correlates
with
sensitivity.
However,
it
remains
highly
uncertain.
Here,
we
show
direct
observational
evidence
for
strong
from
Cf
adjustment
to
increased
aerosols
weak
liquid
water
path
adjustment.
We
estimate
that
drives
between
52%
300%
of
additional
Twomey
effect
over
ocean
a
total
AIF
-1.1
±
0.8
W
m-2.
follows
power
law
as
function
background
droplet
number
concentration,
Nd.
It
thus
depends
on
time
location
is
stronger
when
Nd
low.
only
increases
substantially
clouds
start
drizzle,
suggesting
role
aerosol-precipitation
interactions.
Our
findings
highlight
key
process
reducing
uncertainty
future
projections.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(24), P. 15305 - 15324
Published: Dec. 14, 2023
Abstract.
The
difficulties
in
using
conventional
mitigation
techniques
to
maintain
global-mean
temperatures
well
below
2
∘C
compared
with
pre-industrial
levels
have
been
documented,
leading
so-called
“climate
intervention”
or
“geoengineering”
research
whereby
the
planetary
albedo
is
increased
counterbalance
global
warming
and
ameliorate
some
impacts
of
climate
change.
In
scientific
literature,
most
prominent
intervention
proposal
that
stratospheric
aerosol
injection
(SAI),
although
proposals
for
marine
cloud
brightening
(MCB)
also
received
considerable
attention.
this
study,
we
design
a
new
MCB
experiment
(G6MCB)
UKESM1
Earth-system
model
which
follows
same
baseline
cooling
scenarios
as
well-documented
G6sulfur
SAI
scenario
developed
by
Geoengineering
Model
Intercomparison
Project
(GeoMIP),
compare
results
from
G6MCB
those
G6sulfur.
deployment
strategy
used
injects
sea-salt
into
four
cloudy
areas
eastern
Pacific.
This
appears
capable
delivering
radiative
forcing
up
−1
W
m−2
MCB,
but
at
higher
rates,
much
effect
found
derive
direct
interaction
injected
aerosols
solar
radiation,
i.e.
sky
(MSB).
show
while
can
achieve
its
target
terms
reducing
high-end
moderate
levels,
there
are
several
side
effects.
Some
common
SAI,
including
overcooling
tropics
residual
middle
high
latitudes.
Other
effects
specific
choice
targeted
regions
include
changes
monsoon
precipitation,
year-round
increases
precipitation
over
Australia
maritime
continent,
sea-level
rise
around
western
continent;
these
all
consistent
permanent
very
strong
La
Niña-like
response
being
induced
G6MCB.
emphasize
attention
needs
be
given
oceanic
feedbacks
spatially
inhomogeneous
forcings.
It
should
stressed
extremely
dependent
upon
chosen
deployment.
As
demonstrated
development
strategies
multiple
temperature
targets
change,
further
work
required
models
obtain
robust
understanding
practical
scope,
limitations,
pitfalls
any
proposed
Quaternary Science Reviews,
Journal Year:
2023,
Volume and Issue:
301, P. 107936 - 107936
Published: Jan. 10, 2023
Polar
ice
cores
provide
long,
continuous
and
well-dated
records
of
past
volcanism
have
contributed
significantly
to
our
understanding
volcanic
impacts
on
climate
society.
Sulphate
aerosols
deposited
in
the
are
essential
for
determining
effective
radiative
forcing
potential
eruptions,
but
calculations
improved
with
knowledge
eruption
source
parameters.
Only
co-deposition
ash
can
presently
confirm
eruption.
Here
we
review
current
state
regarding
representation
Common
Era
from
Greenland
consider
what
tephras
reveal
about
ice.
We
augment
published
record
a
large
dataset
previously
unreported
tephras,
result
programme
targeted
sampling
guided
by
microparticle
that
allow
us
home
tephra
layers
variable
temporal
relationships
sulphate
aerosol
deposition.
In
addition
revealing
extensive
region
disperses
Greenland,
explores
first
time
some
insights
provided
such
as
magma
type
style.
characteristics
eruptions
associated
varying
degrees
responses
find
strongest
tends
be
those
producing
mafic
intermediate
tephra,
phreatomagmatic
processes
commonly
involved.
The
frequent
occurrence
multiple
these
instances
may
also
play
role
accentuating
response.
note
consistencies
timing
particulate
fallout
Icelandic
(synchronous)
Alaskan
(ash
before
sulphates)
regions,
greater
delays
(one
or
more
years)
stratospheric
transport
tropical
eruptions.
outline
remaining
avenues
research
ice-core
promise
throw
light
processes,
including
volatile
release
transport,
well
frequency
impact
small-to-moderate
advocate
integration
wide-ranging
towards
better
volcano-climate
relationships.
npj Climate and Atmospheric Science,
Journal Year:
2023,
Volume and Issue:
6(1)
Published: Aug. 29, 2023
Abstract
A
large
fraction
of
the
uncertainty
around
future
global
warming
is
due
to
cooling
effect
aerosol-liquid
cloud
interactions,
and
in
particular
elusive
sign
liquid
water
path
(LWP)
adjustments
aerosol
perturbations.
To
quantify
this
adjustment,
we
propose
a
causal
approach
that
combines
physical
knowledge
form
graph
with
geostationary
satellite
observations
stratocumulus
clouds.
This
allows
us
remove
confounding
influences
from
large-scale
meteorology
disentangle
counteracting
processes
(cloud-top
entrainment
enhancement
precipitation
suppression
perturbations)
on
different
timescales.
results
weak
LWP
are
time-dependent
(first
positive
then
negative)
meteorological
regime-dependent.
More
importantly,
reveals
failing
account
for
covariations
droplet
sizes
depth,
which
are,
respectively,
mediator
confounder
influences,
leads
an
overly
negative
aerosol-induced
response.
would
result
underestimation
influence
aerosol-cloud
interactions.