Abstract.
It
is
now
established
that
the
increase
in
atmospheric
CO2
likely
to
cause
a
weakening,
or
perhaps
collapse
of
Atlantic
Meridional
Overturning
Circulation
(AMOC).
To
investigate
mechanisms
this
response
CMIP5
models,
Levang
and
Schmitt
(2020)
have
estimated
offline
geostrophic
streamfunction
these
models
decomposed
simulated
changes
into
contribution
caused
by
variations
temperature
salinity.
They
concluded
under
warming
scenario,
for
most
weakening
AMOC
fundamentally
driven
anomalies
while
freshwater
forcing
actually
acts
stabilize
it.
However,
given
both
3-D
fields
ocean
salinity
are
expected
respond
at
surface,
it
unclear
what
extent
diagnostic
informative
about
nature
forcing.
clarify
question,
we
used
Earth
system
Model
Intermediate
Complexity
(EMIC)
cGENIE,
which
equipped
with
C-GOLDSTEIN
friction-geostrophic
model.
First,
reproduced
experiments
simulating
RCP8.5
scenario
observed
cGENIE
behaves
similarly
majority
considered
(2020),
dominated
thermal
structure
ocean.
Next,
hysteresis
associated
(1)
water
hosing
(2)
decrease.
In
all
experiments,
initial
appear
be
primarily
distribution,
distribution
compensating
only
partly
contribution.
These
also
reveal
limited
sensitivity
ocean's
inventory.
That
diagnostics
behave
scenarios
suggests
output
proposed
mainly
determined
internal
circulation,
rather
than
applied
Our
results
illustrate
difficulty
inferring
any
information
from
wind
raise
questions
feasibility
designing
experiment
could
identify
aspect
(thermal
haline)
driving
AMOC.
npj Climate and Atmospheric Science,
Год журнала:
2024,
Номер
7(1)
Опубликована: Янв. 29, 2024
Abstract
This
study
investigates
the
possibility
of
Atlantic
Meridional
Overturning
Circulation
(AMOC)
noise-induced
tipping
solely
driven
by
internal
climate
variability
without
applying
external
forcing
that
alter
radiative
or
North
freshwater
budget.
We
address
this
hypothesis
a
rare
event
algorithm
to
ensemble
simulations
present-day
with
an
intermediate
complexity
model.
The
successfully
identifies
trajectories
leading
abrupt
AMOC
slowdowns,
which
are
unprecedented
in
2000-year
control
run.
Part
these
weakened
states
lead
collapsed
state
evidence
recovery
on
multi-centennial
time
scales.
temperature
and
Northern
Hemisphere
jet
stream
responses
internally-induced
slowdowns
show
strong
similarities
those
found
externally
forced
state-of-the-art
models.
slowdown
seems
be
initially
Ekman
transport
due
westerly
wind
stress
anomalies
subsequently
sustained
complete
collapse
oceanic
convection
Labrador
Sea.
These
results
demonstrate
transitions
purely
model
simulation
but
theoretically
possible.
Additionally,
algorithms
tool
valuable
general
interest
points
since
they
introduce
collecting
large
number
events
cannot
sampled
using
traditional
approaches.
opens
identifying
mechanisms
driving
complex
systems
little
a-priori
knowledge
is
available.
Nonlinear processes in geophysics,
Год журнала:
2023,
Номер
30(4), С. 481 - 502
Опубликована: Ноя. 3, 2023
Abstract.
The
climate
system
as
well
ecosystems
might
undergo
relatively
sudden
qualitative
changes
in
the
dynamics
when
environmental
parameters
or
external
forcings
vary
due
to
anthropogenic
influences.
study
of
these
changes,
called
tipping
phenomena,
requires
development
new
methodological
approaches
that
allow
phenomena
observed
nature
be
modeled,
analyzed
and
predicted,
especially
concerning
crisis
its
consequences.
Here
we
briefly
review
mechanisms
classical
investigate
rate-dependent
which
occur
non-autonomous
systems
characterized
by
multiple
timescales
more
detail.
We
focus
on
mechanism
rate-induced
caused
basin
boundary
crossings.
unravel
this
transition
analyze,
particular,
role
such
crossings
a
parameter
drift
induces
saddle-node
bifurcation
attractors
saddle
points
emerge,
including
their
basins
attraction.
Furthermore,
detectability
those
bifurcations
monitoring
single
trajectories
state
space
find
depending
rate
drift,
masked
hidden,
they
can
only
detected
if
critical
is
crossed.
This
analysis
reveals
unstable
states
type
are
organizing
centers
global
multistable
need
much
attention
future
studies.
Paleoclimate
proxy
records
from
the
North
Atlantic
region
reveal
substantially
greater
multicentennial
temperature
variability
during
Last
Glacial
Maximum
(LGM)
compared
to
current
interglacial.
As
there
was
no
obvious
change
in
external
forcing,
causes
for
increased
remain
unknown.
Exploiting
LGM
simulations
with
a
comprehensive
coupled
climate
model
along
high-resolution
records,
we
introduce
an
oscillatory
mode
of
variability,
which
is
associated
moderate
variations
meridional
overturning
circulation
and
depends
on
large-scale
salinity
distribution.
This
self-sustained
amplified
by
sea-ice
feedbacks
induces
maximum
surface
subpolar
region.
Characterized
distinct
climatic
imprint
different
dynamics,
oscillation
has
be
distinguished
Dansgaard-Oeschger
emerges
only
under
full
forcing.
The
potential
modes
emerge
or
disappear
response
changing
forcing
may
have
implications
future
change.
Climate Dynamics,
Год журнала:
2024,
Номер
62(6), С. 5219 - 5237
Опубликована: Апрель 4, 2024
Abstract
Various
studies
identified
possible
drivers
of
extremes
Arctic
sea
ice
reduction,
such
as
observed
in
the
summers
2007
and
2012,
including
preconditioning,
local
feedback
mechanisms,
oceanic
heat
transport
synoptic-
large-scale
atmospheric
circulations.
However,
a
robust
quantitative
statistical
analysis
reduction
is
hindered
by
small
number
events
that
can
be
sampled
observations
numerical
simulations
with
computationally
expensive
climate
models.
Recent
tackled
problem
sampling
using
rare
event
algorithms,
i.e.,
computational
techniques
developed
physics
to
reduce
cost
required
sample
simulations.
Here
we
apply
algorithm
ensemble
intermediate
complexity
coupled
model
PlaSim-LSG
investigate
extreme
negative
summer
pan-Arctic
area
anomalies
under
pre-industrial
greenhouse
gas
conditions.
Owing
algorithm,
estimate
return
times
orders
magnitude
larger
than
feasible
direct
sampling,
compute
statistically
significant
composite
maps
dynamical
quantities
conditional
on
occurrence
these
extremes.
We
find
extremely
low
are
associated
preconditioning
through
winter
ice-ocean
state,
enhanced
downward
longwave
radiation
due
an
anomalously
moist
warm
spring
atmosphere
sensible
fluxes
during
spring-summer
transition.
As
consequence
three
processes,
ice-albedo
becomes
active
leads
amplification
pre-existing
summer.
Abstract.
The
climate
system
as
well
ecosystems
might
undergo
relatively
sudden
qualitative
changes
in
the
dynamics
when
environmental
parameters
or
external
forcings
vary
due
to
anthropogenic
influences.
study
of
these
changes,
called
tipping
phenomena,
requires
development
new
methodological
approaches
that
allow
modeling,
analyzing,
and
predicting
observed
phenomena
nature,
especially
concerning
crisis
its
consequences.
Here
we
briefly
review
mechanisms
classical
investigate
more
detail
rate-dependent
which
occur
non-autonomous
systems
characterized
by
multiple
timescales.
We
focus
on
mechanism
rate-induced
caused
basin
boundary
crossings.
unravel
this
transition
analyze,
particular,
role
such
crossings
a
parameter
drift
induces
saddle-node
bifurcation
attractors
saddle
points
emerge,
including
their
basins
attraction.
Furthermore,
detectability
those
bifurcations
monitoring
single
trajectories
state
space
find
depending
rate
drift,
be
masked
hidden
they
can
detected
only
if
critical
is
crossed.
This
analysis
reveals
quasi-stationary
multistable
are
organizing
centers
global
need
much
attention
future
studies.
Geophysical Research Letters,
Год журнала:
2025,
Номер
52(3)
Опубликована: Фев. 9, 2025
Abstract
Understanding
internal
variability
of
the
climate
system
is
critical
when
isolating
and
anthropogenically
forced
signals.
Here,
we
investigate
modes
Atlantic
Meridional
Overturning
Circulation
(
AMOC
)
using
perturbation
experiments
with
Institut
Pierre‐Simon
Laplace's
(IPSL)
coupled
model
compare
them
to
Coupled
Model
Intercomparison
Project
Phase
6
(CMIP6)
pre‐industrial
control
simulations.
We
identify
two
characteristic
variability—decadal‐to‐multidecadal
DMD
var
centennial
CEN
).
The
former
driven
largely
by
temperature
anomalies
in
subpolar
North
Atlantic,
while
latter
salinity
western
Atlantic.
amplitude
each
mode
scales
linearly
mean
strength
IPSL
experiments.
correlates
well
across
CMIP6
models,
does
not.
These
findings
suggest
that
depends
robustly
on
state,
may
be
model‐dependent.
Chaos An Interdisciplinary Journal of Nonlinear Science,
Год журнала:
2025,
Номер
35(2)
Опубликована: Фев. 1, 2025
A
non-autonomous
system
can
undergo
a
rapid
change
of
state
in
response
to
small
or
slow
forcing,
due
the
presence
nonlinear
processes
that
give
rise
critical
transitions
tipping
points.
Such
are
thought
possible
various
subsystems
(tipping
elements)
Earth’s
climate
system.
The
Atlantic
Meridional
Overturning
Circulation
(AMOC)
is
considered
particular
element
where
models
varying
complexity
have
shown
potential
for
bi-stability
and
tipping.
We
consider
both
transient
stochastic
forcing
simple
but
data-adapted
model
AMOC.
propose
test
geometric
early
warning
signal
predict
whether
will
occur
large
based
on
dynamics
near
an
edge
state.
For
we
quantify
mean
times
between
noise-induced
using
Ordered
Line
Integral
Method
Cameron
(2017)
estimate
quasipotential.
calculate
minimum
action
paths
stable
states
scenarios.
Finally,
discuss
problem
finding
warnings
forcing.
Chaos An Interdisciplinary Journal of Nonlinear Science,
Год журнала:
2025,
Номер
35(2)
Опубликована: Фев. 1, 2025
The
Atlantic
Meridional
Overturning
Circulation
(AMOC)
stability
landscape
is
commonly
investigated
with
single-realization
hysteresis
diagrams
driven
by
freshwater
input
in
the
North
Ocean.
However,
effect
of
CO2
forcing
on
one
side
and
role
internal
climate
variability
timing
tipping
AMOC
other
remain
less
explored.
Here,
we
address
this
gap
running
three
independent
simulations,
consisting
a
slow
ramp-up
plus
ramp-down
concentration
(0.2
ppm/year)
within
PlaSim-Large-Scale
Geostrophic
(LSG)
intermediate
complexity
model.
We
show
that
realizations
CO2-driven
cycle,
particularly,
recovery,
are
remarkably
affected
variability.
In
even
observe
reversed
where
recovers
at
higher
level
than
collapse
point.
While
statistical
Early
Warning
Signals
(EWSs)
some
success
detecting
points,
also
find
EWS
considerably
reduces
predictability
leads
to
false
positives
an
approaching
tipping.
suggest
presence
may
have
characteristics
deviate
substantially
from
behavior
seen
simple
models
caution
needed
when
interpreting
results
single-experiment
realization.
Our
findings
highlight
need
for
probabilistic
approach
defining
“safe
operating
space”
stability,
since
it
might
not
be
possible
define
single
critical
threshold
prevent
collapse.
Physica D Nonlinear Phenomena,
Год журнала:
2023,
Номер
459, С. 134043 - 134043
Опубликована: Дек. 23, 2023
Anticipating
critical
transitions
in
the
Earth
system
is
of
great
societal
relevance,
yet
there
may
be
intrinsic
limitations
to
their
predictability.
For
instance,
from
theory
dynamical
systems
possessing
multiple
chaotic
attractors,
it
known
that
asymptotic
state
depends
sensitively
on
initial
condition
proximity
a
fractal
basin
boundary.
Here,
we
approach
problem
final-state
sensitivity
Atlantic
Meridional
Overturning
Circulation
(AMOC)
using
conceptual
climate
model,
composed
slow
bistable
ocean
coupled
fast
atmosphere.
First,
explore
occurrence
long
transients
monostable
regime,
which
can
mask
loss
stability
near
bifurcations.
In
explicitly
construct
saddle
edge
tracking
technique.
Quantifying
through
maximum
Lyapunov
exponent
and
lifetime
saddle,
find
exhibits
boundary
with
almost
full
phase
space
dimension,
implying
vanishing
predictability
second
kind
Our
results
demonstrate
usefulness
studying
non-attracting
sets
context
predicting
climatic
tipping
points,
provide
guidance
for
interpretation
higher-dimensional
models
such
as
general
circulation
models.