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
Abstract
Climate
science
is
expected
to
provide
usable
information
policy‐makers,
support
the
resolution
of
climate
change.
The
complex,
multiply
connected
nature
change
as
a
social
problem
reviewed
and
contrasted
with
current
modular
discipline‐bounded
approaches
in
science.
We
argue
that
retains
much
its
initial
“physics‐first”
orientation,
it
adheres
problematic
notion
objectivity
freedom
from
value
judgments.
Together,
these
undermine
ability
information.
develop
usability
using
work
literature
on
adaptation,
but
our
argument
applies
all
illustrate
tension
between
objective,
physics‐first
orientation
an
example
about
model
development
practices
For
solutions,
we
draw
two
frameworks
for
which
responds
societal
challenges:
post‐normal
mandated
generate
five
recommendations
adapting
practice
science,
produce
more
thereby
respond
directly
challenge
These
are:
(1)
integrated
cross‐disciplinarity,
(2)
wider
involvement
stakeholders
throughout
lifecycle
study,
(3)
new
framing
role
values
(4)
uncertainty
management,
(5)
communication.
This
article
categorized
under:
Models
Modeling
>
Knowledge
Generation
Social
Status
Change
Sociology/Anthropology
Perceptions,
Behavior,
Communication
npj Climate and Atmospheric Science,
Journal Year:
2024,
Volume and Issue:
7(1)
Published: Feb. 2, 2024
Abstract
Assessing
changes
in
the
distribution
of
biological
communities
that
share
a
climate
(biomes)
is
essential
for
estimating
their
vulnerability
to
change.
We
use
CMIP6
models
calculate
biome
as
featuring
classifications
such
Holdridge’s
Life
Zones
(climate
envelopes).
found
transitional
zones
between
biomes
(known
ecotones)
are
expected
decline
under
all
change
scenarios,
but
also
model
consensus
remains
low.
Accurate
assessments
diversity
loss
limited
certain
areas
globe,
while
still
poor
half
planet.
identify
where
there
robust
estimates
and
ecotones,
lacking.
argue
caution
should
be
exercised
measuring
biodiversity
latter,
greater
confidence
can
placed
former.
find
shortcomings
life
zone
classification
related
inter-model
variability,
which
ultimately
depends
on
larger
problem,
namely
accurate
estimation
precipitation
compared
CRU.
Application
methodology
other
confirms
findings.
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