Cambridge Prisms Water,
Год журнала:
2024,
Номер
3
Опубликована: Дек. 27, 2024
Abstract
The
current
generation
of
climate
models
has
proven
very
helpful
in
understanding
and
projecting
anthropogenic
change
but
also
shown
to
be
insufficient
for
studying
the
interactions
tipping
elements
their
impact
on
overall
stability.
As
a
consequence,
are
mostly
absent
from
projections
that
commonly
used
by
drinking
water
industry
test
resilience
systems.
There
is,
however,
mounting
evidence
existence
potential
(possibly
even
imminent)
activation
some
these
elements.
sector
necessity,
slow-moving
as
its
infrastructure
is
meant
operate
many
decades
practice
often
does
so
longer.
time
scales
possible
changes
associated
with
element
activations
may,
much
shorter.
We
provide
review
present
simple
model
investigates
magnitudes
rapid
activations.
study
consequences
supply
systems,
focusing
Europe,
argue
given
deep
uncertainty
far-reaching
consequences,
it
essential
include
scenarios
decision-making
processes
sector.
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.
Abstract.
Climate
tipping
elements
are
large-scale
subsystems
of
the
Earth
that
may
transgress
critical
thresholds
(tipping
points)
under
ongoing
global
warming,
with
substantial
impacts
on
biosphere
and
human
societies.
Frequently
studied
examples
such
include
Greenland
Ice
Sheet,
Atlantic
Meridional
Overturning
Circulation,
permafrost,
monsoon
systems,
Amazon
rainforest.
While
recent
scientific
efforts
have
improved
our
knowledge
about
individual
elements,
interactions
between
them
less
well
understood.
Also,
potential
events
to
induce
additional
elsewhere,
or
stabilize
other
is
largely
unknown.
Here,
we
map
out
current
state
literature
climate
review
influences
them.
To
do
so,
gathered
evidence
from
model
simulations,
observations
conceptual
understanding,
as
archetypal
paleoclimate
reconstructions
where
multi-component
spatially
propagating
transitions
were
potentially
at
play.
Lastly,
identify
crucial
gaps
in
element
outline
how
future
research
could
address
those
gaps.
Geophysical Research Letters,
Год журнала:
2024,
Номер
51(10)
Опубликована: Май 13, 2024
Abstract
All
climate
models
project
a
weakening
of
the
Atlantic
Meridional
Overturning
Circulation
(AMOC)
strength
in
response
to
greenhouse
gas
forcing.
However,
impacts
AMOC
decline
alone
cannot
be
isolated
from
other
drivers
change
using
existing
Coupled
Model
Intercomparison
Project
simulations.
To
address
this
issue,
we
conduct
idealized
experiments
EC‐Earth3
model.
We
compare
an
abrupt
4×CO
2
simulation
with
same
experiment,
except
artificially
fix
at
preindustrial
levels.
With
design,
can
formally
attribute
differences
between
these
two
decline.
In
addition,
quantify
state‐dependence
by
comparing
aforementioned
which
reduce
strength.
Our
findings
demonstrate
that
are
state‐dependent,
thus
understanding
on
future
requires
targeted
model
experiments.
Surveys in Geophysics,
Год журнала:
2024,
Номер
46(2), С. 443 - 502
Опубликована: Ноя. 6, 2024
Abstract
As
climate
change
continues,
the
likelihood
of
passing
critical
thresholds
or
tipping
points
increases.
Hence,
there
is
a
need
to
advance
science
for
detecting
such
thresholds.
In
this
paper,
we
assess
needs
and
opportunities
Earth
Observation
(EO,
here
understood
refer
satellite
observations)
inform
society
in
responding
risks
associated
with
ten
potential
large-scale
ocean
elements:
Atlantic
Meridional
Overturning
Circulation;
Subpolar
Gyre;
Beaufort
Arctic
halocline;
Kuroshio
Large
Meander;
deoxygenation;
phytoplankton;
zooplankton;
higher
level
ecosystems
(including
fisheries);
marine
biodiversity.
We
review
current
scientific
understanding
identify
specific
EO
related
modelling
each
these
elements.
draw
out
some
generic
that
apply
across
several
These
common
include
importance
maintaining
long-term,
consistent
time
series;
combine
data
consistently
situ
types
subsurface),
example
through
assimilation;
reduce
work
mismatches
resolution
(in
both
directions)
between
models
datasets.
Our
analysis
shows
developing
EO,
prediction
systems
together,
strengths
limitations
each,
provides
many
promising
paths
towards
monitoring
early
warning
tipping,
development
next
generation
models.
Abstract
As
exceeding
the
1.5°C
level
of
global
warming
is
likely
to
happen
in
near
future,
understanding
response
ocean‐climate
system
temporarily
overshooting
this
critical
importance.
Here,
we
apply
Adaptive
Emissions
Reduction
Approach
Earth
System
Model
GFDL‐ESM2M
conduct
novel
overshoot
scenarios
that
reach
2.0,
2.5
and
3.0°C
before
returning
over
time
period
1861–2500.
We
also
perform
a
complementary
scenario
stabilizes
temperature
at
1.5°C,
allowing
isolate
impacts
caused
by
overshoots
alone,
both
during
their
peaks
after
reversals.
The
simulations
indicate
substantial
residual
ocean
surface
persists
high
latitudes
overshoots,
with
most
notable
regional
anomalies
occurring
North
Atlantic
(up
+3.1°C
3°C
compared
stabilization
scenario)
Southern
Ocean
(+1.2°C).
primarily
driven
recoveries
meridional
overturning
circulation
associated
increases
heat
transport.
Excess
subsurface
storage
low
mid‐latitudes
prevents
steric
sea
rise
(SLR)
from
reverting
levels
any
scenario,
remaining
up
32%
higher
on
centennial
scales.
Both
peak
persistent
changes
reversal
bear
significant
implications
for
future
assessments
coastlines,
climates,
marine
ecosystems,
ice
sheets.
Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences,
Год журнала:
2023,
Номер
381(2262)
Опубликована: Окт. 22, 2023
Atlantic
multidecadal
variability
(AMV)
has
long
been
thought
to
be
an
expression
of
low-frequency
in
the
Meridional
Overturning
Circulation
(AMOC).
However,
alternative
hypotheses
have
forwarded,
including
that
AMV
is
primarily
externally
forced.
Here,
we
review
current
state
play
by
assessing
historical
simulations
made
for
sixth
coupled
model
intercomparison
project
(CMIP6).
Overall,
importance
external
forcing
sensitive
type
index
used,
due
globally
coherent
forced
signals
models.
There
are
also
significant
contrasts
between
processes
drive
internally
and
AMV,
but
these
can
isolated
exploring
multivariate
AMV.
Specifically,
internal
CMIP6
models
consistent
with
important
role
ocean
circulation
AMOC
largely
a
surface-flux
mechanism
little
ocean.
fingerprint
similar
observed,
appears
inconsistent
observations.
Therefore,
climate
still
suggest
key
dynamics,
specifically
AMOC,
observed
Nevertheless,
remain
deficient
number
areas,
stronger
dynamical
changes
cannot
ruled
out.
This
article
part
discussion
meeting
issue
'Atlantic
overturning:
new
observations
challenges'.
Climate of the past,
Год журнала:
2025,
Номер
21(1), С. 115 - 132
Опубликована: Янв. 16, 2025
Abstract.
This
study
introduces
a
novel
dynamical
systems
model
designed
to
capture
the
highly
non-periodic
nature
of
Dansgaard–Oeschger
(DO)
events.
Such
events
are
difficult
adequately
due
their
variable
durations
(some
lasting
around
1
century,
while
others
span
multiple
millennia)
and
occurrence
short
precursor
that
precede
longer
DO
despite
similar
boundary
climate
conditions.
Utilising
simplified
two-equation
framework
derived
from
Stommel
model,
our
approach
integrates
an
internal
control
parameter
which
acts
as
feedback
on
Antarctic
Bottom
Water
(AABW)
formation.
Through
both
analytical
numerical
methods,
we
establish
suitable
domain
within
newly
adjusted
models
can
accurately
replicate
palaeoclimatic
records
described
by
summary
statistics
ice-core
data.
The
analysis
also
shows
that,
without
parameter,
does
not
have
in
it
reproduce
wide
range
event
characteristics
seen
record.
provides
new
insights
into
underlying
mechanisms
driving
these
significant
phenomena
necessary
timescale
they
forced
allowing
model's
parameters
vary
through
time.
allows
achieve
unprecedented
precision
capturing
realistic
sequence
with
timing
matching
those
observational
refined
only
enhances
understanding
cycles
but
demonstrates
potential
simple
simulate
complex
interactions.
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.
Environmental Research Letters,
Год журнала:
2023,
Номер
19(1), С. 014054 - 014054
Опубликована: Дек. 12, 2023
Abstract
There
is
a
consensus
that
weakened
Atlantic
Meridional
Overturning
Circulation
(AMOC)
decreases
mean
surface
temperature
in
the
Northern
Hemisphere,
both
over
ocean
and
continents.
However,
impacts
of
reduced
AMOC
on
cold
extreme
events
have
not
yet
been
examined.
We
analyse
strength
Europe
using
targeted
sensitivity
experiments
with
EC-Earth3
climate
model.
Starting
from
fully
coupled
ocean-atmosphere
simulation
which
was
artificially
reduced,
set
atmosphere-only
integrations
prescribed
sea
sea-ice
cover
conducted
to
evaluate
effects
weakly
strongly
strength.
Despite
overall
cooling,
leads
fewer
winter
spells
Europe.
find
intensifies
near-surface
meridional
gradient
North
Europe,
thus
providing
energy
boost
jet
stream.
A
stronger
stream
less
atmospheric
blocking,
reducing
frequency
Although
limited
output
one
model,
our
results
indicate
may
play
role
shaping
future
change
by
modulating
blocking.