Climate Dynamics,
Год журнала:
2024,
Номер
62(6), С. 4673 - 4696
Опубликована: Май 11, 2024
Abstract
Meteorological
processes
over
islands
with
complex
orography
could
be
better
simulated
by
Convection
Permitting
Regional
Climate
Models
(CP-RCMs)
thanks
to
an
improved
representation
of
the
orography,
land–sea
contrasts,
combination
coastal
and
orographic
effects,
explicit
deep
convection.
This
paper
evaluates
ability
CP-RCM
CNRM-AROME
(2.5-km
horizontal
resolution)
simulate
relevant
meteorological
characteristics
Mediterranean
island
Corsica
for
2000–2018
period.
These
hindcast
simulations
are
compared
their
driving
Model
(RCM)
CNRM-ALADIN
(12.5-km
resolution
parameterised
convection),
weather
stations
precipitation
wind
gridded
datasets.
The
main
benefits
found
in
(i)
extremes
resulting
mainly
from
mesoscale
convective
systems
affected
steep
mountains
during
autumn
(ii)
formation
convection
through
thermally
induced
diurnal
circulations
interaction
summer.
Simulations
hourly
extremes,
cycle
precipitation,
distribution
intensities,
duration
events,
sea
breezes
all
2.5-km
respect
RCM,
confirming
added
value.
However,
existing
differences
between
model
observations
difficult
explain
as
biases
related
availability
quality
observations,
particularly
at
high
elevations.
Overall,
results
resolution,
increase
our
confidence
CP-RCMs
investigate
future
climate
projections
terrain.
Climate Dynamics,
Год журнала:
2021,
Номер
57(1-2), С. 275 - 302
Опубликована: Апрель 9, 2021
Abstract
Here
we
present
the
first
multi-model
ensemble
of
regional
climate
simulations
at
kilometer-scale
horizontal
grid
spacing
over
a
decade
long
period.
A
total
23
run
with
$$\sim
$$
∼
3
km,
driven
by
ERA-Interim
reanalysis,
and
performed
22
European
research
groups
are
analysed.
Six
different
models
(RCMs)
represented
in
ensemble.
The
compared
against
available
high-resolution
precipitation
observations
coarse
resolution
(
12
km)
RCMs
parameterized
convection.
model
respect
to
mean
precipitation,
intensity
frequency,
heavy
on
daily
hourly
timescales
seasons.
results
show
that
produce
more
realistic
representation
than
RCMs.
most
significant
improvements
found
for
frequency
both
time
scales
summer
season.
In
general,
tend
intense
reduced
wet-hour
models.
On
average,
shows
reduction
bias
from
\,$$
−40%
km
−3%
summer.
Furthermore,
uncertainty
ranges
i.e.
variability
between
wet
hour
is
half
use
Although
differences
still
exist,
it
evident
these
superior
coarse-resolution
RCM
representing
present-day
climate,
thus
offer
promising
way
forward
investigations
change
local
scales.
Wiley Interdisciplinary Reviews Climate Change,
Год журнала:
2021,
Номер
12(6)
Опубликована: Авг. 16, 2021
Abstract
Approximately
10
years
ago,
convection‐permitting
regional
climate
models
(CPRCMs)
emerged
as
a
promising
computationally
affordable
tool
to
produce
fine
resolution
(1–4
km)
decadal‐long
simulations
with
explicitly
resolved
deep
convection.
This
explicit
representation
is
expected
reduce
projection
uncertainty
related
convection
parameterizations
found
in
most
models.
A
recent
surge
CPRCM
decadal
over
larger
domains,
sometimes
covering
continents,
has
led
important
insights
into
advantages
and
limitations.
Furthermore,
new
observational
gridded
datasets
spatial
temporal
(~1
km;
~1
h)
resolutions
have
leveraged
additional
knowledge
through
evaluations
of
the
added
value
CPRCMs.
With
an
improved
coordination
frame
ongoing
international
initiatives,
production
ensembles
provide
more
robust
projections
better
identification
their
associated
uncertainties.
review
paper
presents
overview
methodology
latest
research
on
current
future
climates.
Impact
studies
that
are
already
taking
advantage
these
highlighted.
ends
by
proposing
next
steps
could
be
accomplished
continue
exploiting
full
potential
article
categorized
under:
Climate
Models
Modeling
>
Earth
System
npj Climate and Atmospheric Science,
Год журнала:
2024,
Номер
7(1)
Опубликована: Фев. 28, 2024
Abstract
Extreme
precipitation
events
lead
to
dramatic
impacts
on
society
and
the
situation
will
worsen
under
climate
change.
Decision-makers
need
reliable
estimates
of
future
changes
as
a
basis
for
effective
adaptation
strategies,
but
projections
at
local
scale
from
regional
models
(RCMs)
are
highly
uncertain.
Here
we
exploit
km-scale
convection-permitting
multi-model
(CPM)
ensemble,
generated
within
FPS
Convection
project,
provide
new
understanding
in
extremes
related
uncertainties
over
greater
Alpine
region.
The
CPM
ensemble
shows
stronger
increase
fractional
contribution
extreme
than
driving
RCM
during
summer,
when
convection
dominates.
We
find
that
substantially
reduces
model
their
total
by
more
50%.
conclude
realistic
representation
dynamical
processes
CPMs
provides
change,
which
essential
policymakers
plan
measures.
International Journal of Climatology,
Год журнала:
2022,
Номер
42(14), С. 7162 - 7185
Опубликована: Апрель 3, 2022
Abstract
Convection‐permitting
climate
modelling
is
a
promising
avenue
for
change
research
and
services
especially
in
mountainous
regions.
Work
required
to
evaluate
the
results
of
high‐resolution
simulations
against
relevant
observations,
put
them
broader
context
coarser
resolution
frameworks.
Here
we
numerical
with
convection‐permitting
regional
model
CNRM‐AROME
ran
at
2.5
km
horizontal
over
large
pan‐Alpine
domain
European
Alps,
using
either
ERA‐Interim
or
output
as
boundary
conditions.
This
study
analyses
annual
seasonal
characteristics
2
m
temperature,
total
precipitation,
solid
fraction
precipitation
snow
depth
scale
French
Alps
under
past
future
The
are
compared
local
reanalysis
S2M,
raw
adjusted,
ADAMONT
method,
CNRM‐ALADIN
driven
by
CNRM‐CM5
global
model.
highlights
generally
similar
differences
between
datasets,
well
obstacles
use
some
outputs
they
stand.
These
consist
excessive
accumulation
on
ground
above
1,800
a.s.l.,
lower
temperature
values
same
elevations
than
S2M
ADAMONT‐adjusted
outputs.
Besides
these
obstacles,
present
several
advantages
Among
them,
significantly
smaller
cold
bias,
more
realistic
accumulated
precipitations,
better
representation
spatial
variability
different
variables
investigated,
which
always
stand
closer
reference
data
As
suggested
many
studies,
could
even
produce
precipitations
high
elevation
taken
our
consequently
projections,
but
lack
reliable
set
observations
remains
an
obstacle
their
evaluation.
The cryosphere,
Год журнала:
2023,
Номер
17(8), С. 3617 - 3660
Опубликована: Авг. 28, 2023
Abstract.
Assessing
past
distributions,
variability
and
trends
in
the
mountain
snow
cover
its
first-order
drivers,
temperature
precipitation,
is
key
for
a
wide
range
of
studies
applications.
In
this
study,
we
compare
results
various
modeling
systems
(global
regional
reanalyses
ERA5,
ERA5-Land,
ERA5-Crocus,
CERRA-Land,
UERRA
MESCAN-SURFEX
MTMSI
climate
model
simulations
CNRM-ALADIN
CNRM-AROME
driven
by
global
reanalysis
ERA-Interim)
against
observational
references
(in
situ,
gridded
datasets
satellite
observations)
across
European
Alps
from
1950
to
2020.
The
comparisons
are
performed
terms
monthly
seasonal
variables
(snow
depth
duration)
their
main
atmospherical
drivers
(near-surface
precipitation).
We
assess
multi-annual
averages
subregional
mean
values,
interannual
variations,
over
timescales,
mainly
winter
period
(from
November
through
April).
MESCAN-SURFEX,
CERRA-Land
offer
satisfying
description
evolution.
However,
spatial
comparison
observation
indicates
that
all
overestimate
duration,
especially
melt-out
date.
ERA5-Land
exhibit
an
overestimation
accumulation
during
winter,
increasing
with
elevations.
analysis
dynamics
remains
complex
multiple
scales
none
models
evaluated
here
fully
succeed
reproduce
compared
reference
datasets.
Indeed,
while
most
outputs
perform
well
at
representing
multi-decadal
precipitation
variability,
they
often
fail
address
duration.
discuss
several
artifacts
potentially
responsible
incorrect
long-term
products
(ERA5
MESCAN-SURFEX),
which
attribute
primarily
heterogeneities
assimilated.
Nevertheless,
many
considered
study
line
current
state
knowledge.
Based
on
these
datasets,
last
50
years
(1968–2017)
scale,
have
experienced
warming
0.3
0.4
∘C
per
decade,
stronger
lower
elevations,
small
reduction
homogeneous
elevation.
decline
duration
ranges
−7
%
−15
decade
−5
d
respectively,
both
showing
larger
decrease
low
intermediate
Overall,
show
no
strategy
outperforms
others
within
our
sample
upstream
choices
(horizontal
resolution,
heterogeneity
observations
used
data
assimilation
reanalyses,
coupling
between
surface
atmosphere,
level
complexity,
configuration
scheme,
etc.)
great
consequences
quality
potential
use.
Despite
limitations,
cases
can
be
characterize
features
Hydrology and earth system sciences,
Год журнала:
2024,
Номер
28(2), С. 375 - 389
Опубликована: Янв. 31, 2024
Abstract.
Extreme
sub-hourly
precipitation,
typically
convective
in
nature,
is
capable
of
triggering
natural
disasters
such
as
floods
and
debris
flows.
A
key
component
climate
change
adaptation
resilience
quantifying
the
likelihood
that
extreme
precipitation
will
exceed
historical
levels
future
scenarios.
Despite
this,
current
approaches
to
estimating
return
are
deemed
insufficient.
The
reason
for
this
can
be
attributed
two
factors:
there
limited
availability
data
from
convection-permitting
models
(capable
simulating
adequately)
statistical
methods
we
use
extrapolate
do
not
capture
physics
governing
global
warming.
We
present
a
novel
physical-based
method
levels.
proposed
model,
named
TEmperature-dependent
Non-Asymptotic
model
eXtreme
(TENAX),
based
on
parsimonious
non-stationary
non-asymptotic
theoretical
framework
incorporates
temperature
covariate
physically
consistent
manner.
first
explain
theory
TENAX
model.
Using
several
stations
Switzerland
case
study,
demonstrate
model's
ability
reproduce
some
observed
properties
precipitation.
then
illustrate
how
utilized
project
changes
warmer
only
projections
temperatures
during
wet
days
foreseen
frequency.
conclude
by
discussing
uncertainties
associated
with
its
limitations,
advantages.
With
one
extremes
at
different
daily
scale
any
location
globally
where
observations
near-surface
air
available.
Communications Earth & Environment,
Год журнала:
2023,
Номер
4(1)
Опубликована: Янв. 5, 2023
Abstract
Larger
organised
convective
storms
(mesoscale-convective
systems)
can
lead
to
major
flood
events
in
Europe.
Here
we
assess
end-of-century
changes
their
characteristics
two
convection-permitting
climate
simulations
from
the
UK
Met
Office
and
ETH-Zürich
that
both
use
high
Representative
Concentration
Pathway
8.5
scenario
but
different
approaches
represent
atmospheric
with
global
warming
models.
The
projections
indicate
more
frequent,
smaller,
slower-moving
storms,
while
show
fewer,
larger,
faster-moving
storms.
However,
increases
peak
precipitation
intensity,
total
volume,
temporal
clustering,
suggesting
increasing
risks
mesoscale-convective
systems
future.
Importantly,
largest
pose
increased
are
projected
increase
frequency
intensity.
These
results
highlight
understanding
large-scale
dynamical
drivers
as
well
thermodynamical
response
of
is
essential
for
accurate
storm
hazards,
needed
future
adaptation.
The
objective
of
this
study
was
to
analyze
the
climate
change
experienced
in
Spain
between
1971
and
2022
estimate
future
(2050).
main
objectives
were
as
follows:
(1)
temporal
evolution
temperature
from
present,
quantify
warming
process
case
evaluate
increase
extreme
heat
events
(heatwaves);
(2)
precipitation
regime
determine
whether
there
is
a
statistically
representative
trend
towards
drier
an
precipitation;
(3)
investigate
interaction
annual
continuous
temperature;
(4)
scenario
for
mainland
Balearic
Islands
2050,
analyzing
trends
land
aridity
predicting
possible
Mediterranean
warm
steppe
climate,
according
Köppen
classification.
aim
test
hypothesis
that
resulting
global
implies
tendency
progressive
drought.
Given
variability
addition
ordinary
least
squares
methodology,
techniques
mainly
used
Mann–Kendall
Kendall–Theil–Sen
(KTS)
regression.
confirmed
very
high
statistical
significance
relationship
(RR)
maximum
(TX).
If
recent
years
(1971–2022)
continues,
it
foreseeable
that,
by
will
be
reduction
14%
23%
with
respect
reference
period
(understood
average
2000).
Spain’s
likely
classification
system
(from
“C”
“B”).
Journal of Geophysical Research Atmospheres,
Год журнала:
2025,
Номер
130(4)
Опубликована: Фев. 11, 2025
Abstract
A
Variable‐Resolution,
global
configuration
of
the
Community
Earth
System
Model
(VR‐CESM)
in
which
atmosphere
and
land
are
only
active
components
is
employed
to
investigate
climate
Euro‐Mediterranean
region.
Two
variable‐resolution
grids
with
regionally
refined
resolutions
0.25°
0.125°
over
study
domain,
respectively,
used.
The
fidelity
these
VR‐CESM
simulations
evaluated
considering
near‐surface
air
temperature
precipitation
fields
for
2000–2014
period
comparison
available
observation‐based
data
sets
those
a
coarse
resolution
(quasi‐uniform
1°)
control
simulation.
Our
analysis
shows
that,
as
model,
can
be
an
alternative
regional
models
advance
our
understanding
climate.
improvements
obtained
mainly
related
better
representation
complex
topography
region
higher
resolution.
Increasing
generally
yields
considerable
simulation;
however,
some
persistent
biases
remain.
Doubling
highest
leads
modest
improvements,
primarily
small‐scale
processes
including
extreme
events
that
substantial
relevance
present
future