Frontiers in Earth Science,
Journal Year:
2023,
Volume and Issue:
11
Published: May 19, 2023
There
is
a
growing
debate
regarding
the
influence
of
solar
activity
on
climate
change
as
forcing
signal
decadal/multidecadal
timescales
not
robust
in
long-term
reconstructed
data
or
numerical
simulations.
However,
could
be
amplified
by
ocean–atmosphere
coupling
sensitive
regions,
including
North
Atlantic
Ocean
(N.A.).
This
study
assessed
varied
total
irradiance
(TSI)
due
to
effects
Meridional
Overturning
Circulation
(AMOC)
based
an
Earth
System
model
with
intermediate
complexity
(PLASIM-GENIE).
Three
groups
experiments
different
TSI
series;
i.e.,
constant
(NS),
decadal
(DS),
and
whole
(AS)
for
1610–2000,
were
conducted
AMOC
response
was
investigated.
The
results
showed
that
internal
system
led
quasi-35-year
quasi-65-year
cycles
significant
stable
negative
correlation
between
multidecadal
timescale.
period
significantly
extended
forcing.
declining
trend
occurred
simulations
after
1800.
Thus,
contributed
weakening
at
rate
0.41
Sv
per
century.
variation
main
contributor
this
decline
Geoscientific model development,
Journal Year:
2023,
Volume and Issue:
16(7), P. 1975 - 1995
Published: April 6, 2023
Abstract.
The
Atlantic
meridional
overturning
circulation
(AMOC)
is
an
important
part
of
our
climate
system.
AMOC
predicted
to
weaken
under
change;
however,
theories
suggest
that
it
may
have
a
tipping
point
beyond
which
recovery
difficult,
hence
showing
quasi-irreversibility
(hysteresis).
Although
hysteresis
has
been
seen
in
simple
models,
difficult
demonstrate
comprehensive
global
models.
Here,
we
outline
set
experiments
designed
explore
and
sensitivity
additional
freshwater
input
as
the
North
Hosing
Model
Intercomparison
Project
(NAHosMIP).
These
include
adding
(hosing)
for
fixed
length
time
examine
rate
mechanisms
weakening
whether
subsequently
recovers
once
hosing
stops.
Initial
results
are
shown
from
eight
models
participating
Sixth
Coupled
(CMIP6).
weakens
all
result
freshening,
but
freshening
ceases,
half
other
stays
weakened
state.
difference
model
behaviour
cannot
be
explained
by
ocean
resolution
or
type
nor
details
subgrid-scale
parameterisations.
Likewise,
previously
proposed
properties
mean
state
such
strength
salinity
advection
feedback.
Instead,
determined
reached
when
stops,
with
those
where
weakest
not
experiencing
recovery.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: Jan. 6, 2024
Potential
climate
tipping
points
pose
a
growing
risk
for
societies,
and
policy
is
calling
improved
anticipation
of
them.
Satellite
remote
sensing
can
play
unique
role
in
identifying
anticipating
phenomena
across
scales.
Where
satellite
records
are
too
short
temporal
early
warning
points,
complementary
spatial
indicators
leverage
the
exceptional
spatial-temporal
coverage
remotely
sensed
data
to
detect
changing
resilience
vulnerable
systems.
Combining
Earth
observation
with
system
models
improve
process-based
understanding
their
interactions,
potential
cascades.
Such
fine-resolution
support
point
management
Earth System Dynamics,
Journal Year:
2024,
Volume and Issue:
15(1), P. 41 - 74
Published: Jan. 26, 2024
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
(AMOC),
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
paleoclimate
reconstructions
where
multi-component
spatially
propagating
transitions
were
potentially
at
play.
uncertainties
large,
find
indications
many
destabilizing.
Therefore,
conclude
should
not
only
be
in
isolation,
but
also
more
emphasis
has
put
interactions.
This
means
cascades
cannot
ruled
centennial
millennial
timescales
warming
levels
1.5
2.0
∘C
shorter
if
surpassed
∘C.
At
these
higher
then
fast
AMOC
address
crucial
gaps
element
interactions,
propose
four
strategies
combining
observation-based
approaches,
system
modeling
expertise,
computational
advances,
expert
knowledge.
Climate Dynamics,
Journal Year:
2023,
Volume and Issue:
61(7-8), P. 3397 - 3416
Published: March 16, 2023
Abstract
Given
paleoclimatic
evidence
that
the
Atlantic
Meridional
Overturning
Circulation
(AMOC)
may
affect
global
climate
system,
we
conduct
model
experiments
with
EC-Earth3,
a
state-of-the-art
GCM,
to
specifically
investigate,
for
first
time,
mechanisms
of
precipitation
change
over
Euro-Atlantic
sector
induced
by
weakened
AMOC.
We
artificially
weaken
strength
AMOC
in
through
release
freshwater
anomaly
into
Northern
Hemisphere
high
latitude
ocean,
thereby
obtaining
~
57%
weaker
respect
its
preindustrial
60
years.
Similar
prior
studies,
find
decreases
response
However,
also
frequency
wet
days
increases
some
regions.
By
computing
atmospheric
moisture
budget,
intensified
but
drier
storms
cause
less
land.
Nevertheless,
changes
jet
stream
tend
enhance
northwestern
Europe.
further
investigate
association
anomalies
large-scale
circulations
weather
regimes
clustering
geopotential
height
daily
anomalies.
an
increase
positive
phase
North
Oscillation
(NAO+),
which
is
associated
occurrence
northern
Europe
and
conditions
southern
Since
reduction
within
inter-model
range
projected
declines
end
twenty-first
century,
our
results
have
implications
understanding
role
future
hydrological
changes.
Abstract.
The
Atlantic
meridional
overturning
circulation
(AMOC)
is
an
important
part
of
our
climate
system.
AMOC
predicted
to
weaken
under
change,
however
there
are
theories
that
it
may
have
a
tipping
point
beyond
which
recovery
difficult,
hence
showing
quasi-irreversibility
(hysteresis).
Although
hysteresis
has
been
seen
in
simple
models,
difficult
demonstrate
comprehensive
global
models.
Here
we
outline
set
experiments
designed
explore
and
sensitivity
additional
freshwater
input
as
the
North
hosing
model
intercomparison
project
(NAHosMIP).
These
include
adding
(hosing)
for
fixed
length
time
examine
rate
mechanisms
or
weakening,
whether
subsequently
recovers
once
stops.
Initial
results
shown
from
eight
models
participating
Sixth
Coupled
Model
Intercomparison
Project
(CMIP6).
weakens
all
freshening,
but
freshening
ceases,
half
other
stays
weakened
state.
difference
behaviour
cannot
be
explained
by
ocean
resolution
type,
details
subgridscale
parameterizations.
Nor
can
previously
proposed
properties
mean
state
such
strength
salinity
advection
feedback.
Instead
determined
reached
when
stops,
with
those
where
weakest
not
experiencing
recovery.
Ocean science,
Journal Year:
2023,
Volume and Issue:
19(1), P. 141 - 167
Published: Feb. 20, 2023
Abstract.
Increasing
Greenland
Ice
Sheet
melting
is
anticipated
to
impact
water
mass
transformation
in
the
subpolar
North
Atlantic
and
ultimately
meridional
overturning
circulation.
Complex
ocean
climate
models
are
widely
applied
estimate
magnitude
timing
of
related
impacts
under
global
warming.
We
discuss
role
mean
state,
transformation,
mesoscale
eddies,
atmospheric
coupling
shaping
response
Ocean
enhanced
runoff.
In
a
suite
eight
dedicated
60-
100-year-long
model
experiments
with
without
coupling,
eddy
processes
parameterized
explicitly
simulated
regular
significantly
enlarged
runoff,
we
find
(1)
major
by
interactive
atmosphere
enabling
compensating
temperature
feedback,
(2)
non-negligible
influence
state
biased
towards
greater
stability
coupled
simulations,
both
which
make
circulation
less
susceptible
freshwater
perturbation
applied,
(3)
more
even
spreading
deeper
mixing
runoff
tracer
inter-gyre
exchange
subtropics
strongly
eddying
simulations.
Overall,
our
demonstrate
important
dynamics
feedback
projections
system
hence
underline
necessity
advance
scale-aware
parameterizations
for
next-generation
models.
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.
Environmental Research Letters,
Journal Year:
2023,
Volume and Issue:
18(4), P. 044046 - 044046
Published: March 15, 2023
Abstract
The
North
Atlantic
Oscillation
(NAO)
plays
a
leading
role
in
modulating
wintertime
climate
over
the
and
surrounding
continents
of
Europe
America.
Here
we
show
that
observed
evolution
NAO
displays
larger
multi-decadal
variability
than
simulated
by
nearly
all
CMIP6
models.
To
investigate
as
pacemaker
variability,
analyse
simulations
are
constrained
to
follow
NAO.
We
use
particle
filter
data-assimilation
technique
sub-selects
members
among
an
ensemble
simulations,
well
El
Niño
Southern
Annular
Mode
global
model,
without
nudging
terms.
Since
model
also
contains
external
forcings,
these
can
be
used
compare
forced
response
effect
three
assimilated
modes.
Concentrating
on
28
year
periods
strongest
trends,
leads
large
trends
temperature
precipitation
Northern
Hemisphere
land
sea-ice
concentration.
subpolar
gyre
region
is
particularly
strongly
influenced
NAO,
with
links
found
both
concurrent
atmospheric
Meridional
Overturning
Circulation
(AMOC).
Care
thus
needs
taken
account
for
impacts
when
using
sea
surface
this
proxy
AMOC
strength
decadal
time-scales.
Our
results
have
important
implications
analyses
highlight
need
further
work
understand
causes
variability.
Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences,
Journal Year:
2023,
Volume and Issue:
381(2262)
Published: Oct. 22, 2023
The
Atlantic
Meridional
Overturning
Circulation
(AMOC),
a
crucial
element
of
the
Earth's
climate
system,
is
projected
to
weaken
over
course
twenty-first
century
which
could
have
far
reaching
consequences
for
occurrence
extreme
weather
events,
regional
sea
level
rise,
monsoon
regions
and
marine
ecosystem.
latest
IPCC
report
puts
likelihood
such
weakening
as
'very
likely'.
As
our
confidence
in
future
projections
depends
largely
on
ability
model
past
climate,
we
take
an
in-depth
look
at
difference
twentieth
evolution
AMOC
based
observational
data
(including
direct
observations
various
proxy
data)
from
ensembles.
We
show
that
both
magnitude
trend
different
time
periods
often
even
sign
differs
between
ensemble
mean,
with
becoming
greater
when
looking
CMIP6
compared
CMIP5.
discuss
possible
reasons
this
observation-model
discrepancy
question
what
it
means
higher
than
historical
reproductions.
This
article
part
discussion
meeting
issue
'Atlantic
overturning:
new
challenges'.