Surveys in Geophysics,
Journal Year:
2024,
Volume and Issue:
unknown
Published: May 31, 2024
Abstract
This
paper
is
concerned
with
how
the
diabatically-forced
overturning
circulations
of
atmosphere,
established
by
deep
convection
within
tropical
trough
zone
(TTZ),
first
introduced
Riehl
and
(Malkus)
Simpson,
in
Contr
Atmos
Phys
52:287–305
(1979),
fundamentally
shape
distributions
subtropical
cloudiness
changes
to
as
Earth
warms.
The
study
draws
on
an
analysis
a
range
observations
understand
connections
between
energetics
TTZ,
clouds.
These
reveal
tight
coupling
two
main
components
diabatic
heating,
cloud
component
radiative
shaped
mostly
high
clouds
formed
convection,
latent
heating
associated
precipitation.
Interannual
variability
TTZ
reveals
marked
variation
that
connects
depth
troposphere,
thickness
TOA
imbalance.
examines
this
convective
further
afield
context
CMIP6
model
experiments
climate
warming.
warming
realized
SSP5-8.5
scenario
multi-model
experiments,
for
example,
produces
enhanced
Hadley
circulation
increased
cooling
subsidence
regions.
impacts
low
turn
response
through
feedbacks.
pattern
produced
models,
also
influenced
region,
has
profound
influence
projected
global
npj Climate and Atmospheric Science,
Journal Year:
2023,
Volume and Issue:
6(1)
Published: June 17, 2023
Abstract
Benchmarking
climate
model
simulations
against
observations
of
the
is
core
to
process
building
realistic
models
and
developing
accurate
future
projections.
However,
in
many
cases,
do
not
match
historical
observations,
particularly
on
regional
scales.
If
there
a
mismatch
between
modeled
observed
features,
should
we
necessarily
conclude
that
our
are
deficient?
Using
several
illustrative
examples,
emphasize
internal
variability
can
easily
lead
marked
differences
basic
features
climate,
even
when
decades
data
available.
This
appear
as
an
apparent
failure
capture
trends
or
changes
global
teleconnections,
simulation
extreme
events.
Despite
large
body
literature
impact
this
acknowledgment
has
yet
penetrated
evaluation
activities,
for
climate.
We
using
single
small
ensemble
error
premature
conclusions
fidelity.
A
multidecadal
therefore
needed
properly
sample
order
robustly
identify
deficiencies
convincingly
demonstrate
progress
generations
models.
Annual Review of Public Health,
Journal Year:
2023,
Volume and Issue:
44(1), P. 255 - 277
Published: Jan. 10, 2023
Climate
change
is
a
threat
multiplier,
exacerbating
underlying
vulnerabilities,
worsening
human
health,
and
disrupting
health
systems'
abilities
to
deliver
high-quality
continuous
care.
This
review
synthesizes
the
evidence
of
what
care
sector
can
do
adapt
changing
climate
while
reducing
its
own
impact,
identifies
barriers
change,
makes
recommendations
achieve
sustainable,
resilient
systems.
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.
Journal of Advances in Modeling Earth Systems,
Journal Year:
2024,
Volume and Issue:
16(2)
Published: Feb. 1, 2024
Abstract
Toward
the
achievement
of
reliable
global
kilometer‐scale
(k‐scale)
climate
simulations,
we
improve
Nonhydrostatic
ICosahedral
Atmospheric
Model
(NICAM)
by
focusing
on
moist
physical
processes.
A
goal
model
improvement
is
to
establish
a
configuration
that
can
simulate
realistic
fields
seamlessly
from
daily‐scale
variability
climatological
statistics.
Referring
two
representative
configurations
present
NICAM,
each
which
has
been
used
for
climate‐scale
and
sub‐seasonal‐scale
experiments,
try
find
appropriate
partitioning
fast/local
slow/global‐scale
circulations.
In
series
sensitivity
experiments
at
14‐km
horizontal
resolution,
test
(a)
tuning
terminal
velocities
rain,
snow,
cloud
ice,
(b)
implementation
turbulent
diffusion
Leonard
term,
(c)
enhanced
vertical
resolution.
These
tests
yield
reasonable
convection
triggering
convection‐induced
tropospheric
moistening,
result
in
better
performance
than
previous
NICAM
simulations.
mean
state,
double
Intertropical
Convergence
Zone
bias
disappears,
zonal
contrast
equatorial
precipitation,
top‐of‐atmosphere
radiation
balance,
temperature
profile,
position/strength
subtropical
jet
are
reproduced
dramatically
better.
Variability
such
as
waves
Madden–Julian
oscillation
(MJO)
spontaneously
realized
with
spectral
power
Asian
summer
monsoon,
boreal‐summer
MJO,
tropical
cyclone
(TC)
activities
more
realistically
simulated
especially
around
western
Pacific.
Meanwhile,
biases
still
exist
representation
low‐cloud
fraction,
TC
intensity,
precipitation
diurnal
cycle,
suggesting
both
higher
spatial
resolutions
further
development
warranted.
Annals of the New York Academy of Sciences,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 24, 2025
Abstract
Vegetation
is
often
viewed
as
a
consequence
of
long‐term
climate
conditions.
However,
vegetation
itself
plays
fundamental
role
in
shaping
Earth's
by
regulating
the
energy,
water,
and
biogeochemical
cycles
across
terrestrial
landscapes.
It
exerts
influence
consuming
water
resources
through
transpiration
interception,
lowering
atmospheric
CO
2
concentration,
altering
surface
roughness,
controlling
net
radiation
its
partitioning
into
sensible
latent
heat
fluxes.
This
propagates
atmosphere,
from
microclimate
scales
to
entire
boundary
layer,
subsequently
impacting
large‐scale
circulation
global
transport
moisture.
Understanding
feedbacks
between
atmosphere
multiple
crucial
for
predicting
land
use
cover
changes,
accurately
representing
these
processes
models.
review
discusses
biophysical
mechanisms
which
modulates
spatial
temporal
scales.
Particularly,
we
evaluate
on
patterns,
precipitation,
temperature,
considering
both
trends
extreme
events,
such
droughts
heatwaves.
Our
goal
highlight
state
science
recent
studies
that
may
help
advance
our
collective
understanding
they
play
climate.
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(47)
Published: Nov. 14, 2022
Traditional
general
circulation
models,
or
GCMs-that
is,
three-dimensional
dynamical
models
with
unresolved
terms
represented
in
equations
tunable
parameters-have
been
a
mainstay
of
climate
research
for
several
decades,
and
some
the
pioneering
studies
have
recently
recognized
by
Nobel
prize
Physics.
Yet,
there
is
considerable
debate
around
their
continuing
role
future.
Frequently
mentioned
as
limitations
GCMs
are
structural
error
uncertainty
across
different
representations
scales
fact
that
tuned
to
reproduce
certain
aspects
observed
Earth.
We
consider
these
shortcomings
context
future
generation
may
address
issues
through
substantially
higher
resolution
detail,
use
machine
learning
techniques
match
them
better
observations,
theory,
process
models.
It
our
contention
calibration,
far
from
being
weakness
an
essential
element
simulation
complex
systems,
contributes
understanding
inner
workings.
Models
can
be
calibrated
reveal
both
fine-scale
detail
global
response
external
perturbations.
New
methods
enable
us
articulate
improve
connections
between
levels
abstract
representation
processes,
resides
entire
hierarchy
where
will
continue
play
central
foreseeable