Authorea (Authorea),
Journal Year:
2023,
Volume and Issue:
unknown
Published: Aug. 22, 2023
The
internal
variability
pertains
to
fluctuations
originating
from
processes
inherent
the
climate
component
and
their
mutual
interactions.
On
other
hand,
forced
delineates
influence
of
external
boundary
conditions
on
physical
system.
A
methodology
is
formulated
distinguish
between
within
surface
air
temperature.
noise-to-noise
approach
employed
for
training
a
neural
network,
drawing
an
analogy
image
noise.
large
dataset
compiled
using
temperature
data
spanning
1901
2020,
obtained
ensemble
Atmosphere-Ocean
General
Circulation
Model
(AOGCM)
simulations.
network
utilized
U-Net,
widely
adopted
convolutional
primarily
designed
segmentation.
To
assess
performance,
comparisons
are
made
outputs
two
single-model
initial-condition
ensembles
(SMILEs),
mean,
U-Net’s
predictions.
U-Net
reduces
by
factor
four,
although
notable
discrepancies
observed
at
regional
scale.
While
demonstrating
effective
filtering
El
Niño
Southern
Oscillation,
encounters
challenges
in
areas
dominated
variability,
such
as
Arctic
sea
ice
retreat
region.
This
holds
potential
extension
variables,
facilitating
insights
into
enduring
changes
triggered
forcings
over
long
term.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(20), P. 13369 - 13385
Published: Oct. 24, 2023
Abstract.
Solar
climate
intervention
using
stratospheric
aerosol
injection
(SAI)
has
been
proposed
as
a
method
which
could
offset
some
of
the
adverse
effects
global
warming.
The
Assessing
Responses
and
Impacts
on
Earth
system
with
Stratospheric
Aerosol
Injection
(ARISE-SAI)
set
simulations
is
based
moderate-greenhouse-gas-emission
scenario
employs
sulfur
dioxide
at
four
off-equatorial
locations
control
algorithm
maintains
global-mean
surface
temperature
1.5
K
above
pre-industrial
conditions
(ARISE-SAI-1.5),
well
latitudinal
gradient
inter-hemispheric
difference
in
temperature.
This
first
comparison
between
two
models
(CESM2
UKESM1)
applying
same
multi-target
SAI
strategy.
CESM2
successful
reaching
its
targets,
but
UKESM1
considerable
residual
Arctic
occurs
because
pattern
change
determined
by
both
structure
forcing
(mainly
greenhouse
gases
aerosols)
models'
feedbacks,
latter
favour
strong
amplification
warming
UKESM1.
Therefore,
research
constraining
level
future
would
also
inform
any
hypothetical
deployment
strategy
aims
to
maintain
Equator-to-pole
near-surface
differences.
Furthermore,
despite
broad
agreement
precipitation
response
extratropics,
changes
over
tropical
land
show
important
inter-model
differences,
even
under
gas
only.
In
general,
this
ensemble
step
comparing
policy-relevant
scenarios
will
help
design
an
experimental
protocol
reduces
known
negative
side
simple
enough
encourage
more
participate.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Dec. 15, 2023
Observations
are
increasingly
used
to
detect
critical
slowing
down
(CSD)
measure
stability
changes
in
key
Earth
system
components.
However,
most
datasets
have
non-stationary
missing-data
distributions,
biases
and
uncertainties.
Here
we
show
that,
together
with
the
pre-processing
steps
deal
them,
these
can
bias
CSD
analysis.
We
present
an
uncertainty
quantification
method
address
such
issues.
how
propagate
uncertainties
provided
analysis
develop
conservative,
surrogate-based
significance
tests
on
indicators.
apply
our
three
observational
sea-surface
temperature
salinity
fingerprints
of
Atlantic
Meridional
Overturning
Circulation
derived
from
them.
find
that
properties
especially
specific
gap
filling
procedures
some
cases
indeed
cause
false
indication
CSD.
indicators
North
still
significant
when
accounting
for
dataset
coverage.
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(31)
Published: Aug. 2, 2024
One
way
to
warn
of
forthcoming
critical
transitions
in
Earth
system
components
is
using
observations
detect
declining
stability.
It
has
also
been
suggested
extrapolate
such
stability
changes
into
the
future
and
predict
tipping
times.
Here,
we
argue
that
involved
uncertainties
are
too
high
robustly
We
raise
concerns
regarding
(i)
modeling
assumptions
underlying
any
extrapolation
historical
results
future,
(ii)
representativeness
individual
component
time
series,
(iii)
impact
preprocessing
used
observational
datasets,
with
focus
on
nonstationary
coverage
gap
filling.
explore
these
general
specifically
for
example
Atlantic
Meridional
Overturning
Circulation.
even
under
assumption
a
given
an
approaching
point,
large
reliably
estimate
times
by
extrapolating
information.
Hydrology and earth system sciences,
Journal Year:
2024,
Volume and Issue:
28(9), P. 2123 - 2137
Published: May 15, 2024
Abstract.
Global
responses
of
the
hydrological
cycle
to
climate
change
have
been
widely
studied,
but
uncertainties
still
remain
regarding
water
vapor
lower-tropospheric
temperature.
Here,
we
investigate
trends
in
global
total
precipitable
(TPW)
and
surface
temperature
from
1958
2021
using
ERA5
JRA-55
reanalysis
datasets.
We
further
validate
these
radiosonde
1979
2019
Atmospheric
Infrared
Sounder
(AIRS)
Special
Sensor
Microwave
Imager/Sounder
(SSMIS)
observations
2003
2021.
Our
results
indicate
a
increase
∼
2
%
per
decade
1993–2021.
These
variations
TPW
reflect
interactions
warming
feedback
mechanisms
across
different
spatial
scales.
also
revealed
significant
near-surface
(T2
m)
trend
0.15
K
decade−1
over
period
1958–2021.
The
consistent
at
rate
0.21
after
1993
corresponds
strong
response
9.5
K−1
globally,
with
land
areas
approximately
twice
as
fast
oceans.
relationship
between
T2
m
showed
variation
around
6
K−1–8
15–55°
N
latitude
band,
aligning
theoretical
estimates
Clausius–Clapeyron
equation.
Abstract.
Solar
climate
intervention
using
stratospheric
aerosol
injection
(SAI)
has
been
proposed
as
a
method
which
could
offset
some
of
the
adverse
effects
global
warming.
The
Assessing
Responses
and
Impacts
on
Earth
system
with
Stratospheric
Aerosol
Injection
(ARISE-SAI)
set
simulations
is
based
moderate
greenhouse
gas
emission
scenario
employs
sulphur
dioxide
at
four
off-equatorial
locations
control
algorithm
maintains
global-mean
surface
temperature
1.5
K
above
preindustrial
conditions
(ARISE-SAI-1.5),
well
latitudinal
gradient
inter-hemispheric
difference
in
temperature.
This
first
comparison
between
two
models
(CESM2
UKESM1)
applying
same
multi-target
SAI
strategy.
CESM2
successful
reaching
its
targets,
but
UKESM1
considerable
residual
Arctic
occurs
because
pattern
change
geoengineered
determined
both
by
structure
forcing
(mainly
gases
aerosols)
models’
feedbacks,
latter
favour
strong
amplification
warming
UKESM1.
Therefore,
research
constraining
level
future
would
also
inform
any
hypothetical
deployment
strategy
aims
to
maintain
interhemispheric
equator-to-pole
near-surface
differences.
Furthermore,
despite
broad
agreement
precipitation
response
extratropics,
changes
over
tropical
land
show
important
inter-model
differences,
even
under
only.
In
general,
this
ensemble
step
comparing
policy-relevant
scenarios
SAI,
will
help
design
an
experimental
protocol
reduces
known
negative
side
simple
enough
encourage
more
participate.
Abstract
There
are
large
uncertainties
in
the
projections
of
future
warming
hole,
which
is
defined
as
cooling
trend
subpolar
North
Atlantic
Ocean
despite
global
warming.
Here,
we
found
that
uncertainty
changes
hole
mainly
due
to
model
bias
rather
than
either
natural
variability
or
climate
change
scenario.
Observations
and
results
constrain
intensity
terms
its
relationship
with
present-day
surface
density
Atlantic.
Models
a
low
tend
project
weaker
(i.e.,
stronger
temperature
increase)
suppressed
oceanic
deep
convection
models
high
density.
This
was
robust
across
all
scenarios
used
reduce
by
39%
emissions
Environmental Data Science,
Journal Year:
2025,
Volume and Issue:
4
Published: Jan. 1, 2025
Abstract
Understanding
the
complex
dynamics
of
climate
patterns
under
different
anthropogenic
emissions
scenarios
is
crucial
for
predicting
future
environmental
conditions
and
formulating
sustainable
policies.
Using
Dynamic
Mode
Decomposition
with
control
(DMDc),
we
analyze
surface
air
temperature
from
simulations
to
elucidate
effects
various
climate-forcing
agents.
This
improves
upon
previous
DMD-based
methods
by
including
forcing
information
as
a
variable.
Our
study
identifies
both
common
patterns,
like
North
Atlantic
Oscillation
El
Niño
Southern
Oscillation,
distinct
impacts
aerosol
carbon
emissions.
We
show
that
these
emissions’
vary
scenarios,
particularly
higher
radiative
forcing.
findings
confirm
DMDc’s
utility
in
analysis,
highlighting
its
role
extracting
modes
variability
while
controlling
contributions
exposing
trends
spatial
change.