International Journal of Climatology,
Год журнала:
2021,
Номер
41(13), С. 5899 - 5919
Опубликована: Апрель 29, 2021
Abstract
This
study
compared
the
historical
simulations
and
future
projections
of
precipitation
temperature
Coupled
Model
Intercomparison
Project
(CMIP)5
CMIP6
general
circulation
models
(GCMs)
to
quantify
differences
in
due
scenarios.
Five
performance
indicators
were
used
model
reproducibility
observed
levels
at
22
stations
for
period
1970–2005.
The
percentages
change
estimated
near
(2025–2060)
far
(2065–2100)
two
Representative
Concentration
Pathway
(RCP)4.5
RCP8.5
scenarios
CMIP5
Shared
Socioeconomic
(SSP)2–4.5
SSP5‐8.5
CMIP6.
uncertainty
projection
each
case
was
calculated
using
reliability
ensemble
average
(REA)
method.
As
a
result,
GCMs
showed
an
improvement
with
regard
ability
simulate
climate.
higher
SSPs
than
that
RCPs.
With
temperature,
RCPs
SSPs.
means
changes
both
contributes
confidence
bolsters
our
understanding
relative
Reviews of Geophysics,
Год журнала:
2022,
Номер
60(3)
Опубликована: Июнь 28, 2022
Abstract
Observation‐based
and
modeling
studies
have
identified
the
Eastern
Mediterranean
Middle
East
(EMME)
region
as
a
prominent
climate
change
hotspot.
While
several
initiatives
addressed
impacts
of
in
parts
EMME,
here
we
present
an
updated
assessment,
covering
wide
range
timescales,
phenomena
future
pathways.
Our
assessment
is
based
on
revised
analysis
recent
observations
projections
extensive
overview
scientific
literature
causes
effects
regional
change.
Greenhouse
gas
emissions
EMME
are
growing
rapidly,
surpassing
those
European
Union,
hence
contributing
significantly
to
Over
past
half‐century
especially
during
decades,
has
warmed
faster
than
other
inhabited
regions.
At
same
time,
changes
hydrological
cycle
become
evident.
The
observed
temperature
increase
about
0.45°C
per
decade
projected
continue,
although
strong
global
greenhouse
emission
reductions
could
moderate
this
trend.
In
addition
mean
conditions,
call
attention
extreme
weather
events
with
potentially
disruptive
societal
impacts.
These
include
strongly
increasing
severity
duration
heatwaves,
droughts
dust
storms,
well
torrential
rain
that
can
trigger
flash
floods.
review
complemented
by
discussion
atmospheric
pollution
land‐use
region,
including
urbanization,
desertification
forest
fires.
Finally,
identify
sectors
may
be
critically
affected
formulate
adaptation
research
recommendations
toward
greater
resilience
Earth Systems and Environment,
Год журнала:
2021,
Номер
5(1), С. 1 - 24
Опубликована: Янв. 1, 2021
Abstract
The
Coupled
Model
Intercomparison
Project
Phase
6
(CMIP6)
dataset
is
used
to
examine
projected
changes
in
temperature
and
precipitation
over
the
United
States
(U.S.),
Central
America
Caribbean.
are
computed
using
an
ensemble
of
31
models
for
three
future
time
slices
(2021–2040,
2041–2060,
2080–2099)
relative
reference
period
(1995–2014)
under
Shared
Socioeconomic
Pathways
(SSPs;
SSP1-2.6,
SSP2-4.5,
SSP5-8.5).
CMIP6
reproduces
observed
annual
cycle
distribution
mean
with
biases
between
−
0.93
1.27
°C
37.90
58.45%,
respectively,
most
region.
However,
modeled
too
large
western
Midwestern
U.S.
during
winter
spring
North
American
monsoon
region
summer,
while
small
southern
America.
Temperature
increase
entire
domain
all
SSPs,
by
as
much
SSP5-8.5,
more
pronounced
increases
northern
latitudes
regions
that
receive
snow
present
climate.
Annual
projections
end
twenty-first
century
have
uncertainty,
expected,
exhibit
a
meridional
dipole-like
pattern,
increasing
10–30%
decreasing
10–40%
Caribbean,
especially
Seasonally,
eastern
central
subregions
decrease
summer
autumn.
Over
America,
seasons
except
analysis
was
repeated
on
subset
9
best
performance
period;
however,
no
significant
difference
found,
suggesting
model
bias
not
strongly
influencing
projections.
Earth Systems and Environment,
Год журнала:
2021,
Номер
5(3), С. 481 - 497
Опубликована: Авг. 23, 2021
This
paper
presents
projected
changes
in
extreme
temperature
and
precipitation
events
by
using
Coupled
Model
Intercomparison
Project
phase
6
(CMIP6)
data
for
mid-century
(2036–2065)
end-century
(2070–2099)
periods
with
respect
to
the
reference
period
(1985–2014).
Four
indices
namely,
Annual
maximum
of
(TXx),
Extreme
heat
wave
days
frequency
(HWFI),
consecutive
5-day
(RX5day),
Consecutive
Dry
Days
(CDD)
were
investigated
under
four
socioeconomic
scenarios
(SSP1-2.6;
SSP2-4.5;
SSP3-7.0;
SSP5-8.5)
over
entire
globe
its
26
Special
Report
on
Managing
Risks
Events
Disasters
Advance
Climate
Change
Adaptation
(SREX)
regions.
The
projections
show
an
increase
intensity
hot
extremes
land.
hottest
(as
measured
TXx)
is
more
extratropical
regions
than
tropics,
while
extremely
HWFI)
tropics.
Drought
CDD)
Brazil,
Mediterranean,
South
Africa,
Australia.
Meanwhile,
Asian
monsoon
(i.e.,
Asia,
East
Southeast
Asia)
become
prone
flash
flooding
later
twenty-first
century
as
shown
higher
RX5day
index
projections.
reveal
large
spatial
variability
within
each
SREX
region.
studied
increases
increasing
greenhouse
gas
concentration
(GHG)
at
end
century.
change
pattern
their
minimum
low-emission
scenario
SSP1-2.6.
Our
results
indicate
that
increased
GHG
leads
substantial
intensities.
Hence,
limiting
CO2
emissions
could
substantially
limit
risks
associated
International Journal of Climatology,
Год журнала:
2021,
Номер
41(15), С. 6474 - 6496
Опубликована: Май 18, 2021
Abstract
This
study
examines
the
improvement
in
Coupled
Model
Intercomparison
Project
Phase
Six
(CMIP6)
models
against
predecessor
CMIP5
simulating
mean
and
extreme
precipitation
over
East
Africa
region.
The
compares
climatology
of
indices
simulated
by
CMIP
with
CHIRPS
data
set
using
robust
statistical
techniques
for
1981–2005.
results
display
varying
performance
general
circulation
(GCMs)
simulation
annual
seasonal
domain.
CMIP6
multi‐model
ensemble
(hereafter
MME)
shows
improved
local
cycle
a
better
representation
rainfall
within
two
peaks,
especially
MAM
relative
to
their
predecessor.
Moreover,
is
well
captured
CMIP5.
CMIP6‐MME
performed
than
CMIP5‐MME
lesser
biases
Simple
Daily
Intensity
Index
(SDII),
consecutive
dry
days
(CDD),
very
heavy
>20
mm
(R20mm)
Africa.
Remarkably,
most
are
unable
simulate
extremely
wet
(R95p).
Some
(e.g.,
NorESM2‐MM
CNRM‐CM6‐1)
depict
reproducing
observed
across
all
analyses.
OND
season
some
(i.e.,
R95p,
PRCPTOT),
except
SDII,
CDD,
R20mm
models.
Consistent
other
studies,
both
CMIP5/6
as
compared
individual
due
cancellation
systematic
errors
Generally,
depicts
However,
new
model
generation
still
marred
uncertainty,
thereby
depicting
unsatisfactory
calls
further
investigation
into
sources
persistent
methodology
identifying
features
that
can
accurately
patterns
future
usage.
Science Bulletin,
Год журнала:
2021,
Номер
66(24), С. 2528 - 2537
Опубликована: Июль 21, 2021
This
paper
presents
projections
of
climate
extremes
over
China
under
global
warming
1.5,
2,
and
3
°C
above
pre-industrial
(1861-1900),
based
on
the
latest
Coupled
Model
Intercomparison
Project
phase
6
(CMIP6)
simulations.
Results
are
compared
with
what
produced
by
precedent
project,
CMIP5.
evaluation
for
reference
period
(1985-2005)
indicates
that
CMIP6
models
outperform
their
predecessors
in
CMIP5,
especially
simulating
precipitation
extremes.
Areal
averages
changes
most
indices
found
larger
than
The
emblematic
annual
mean
temperature,
when
averaged
whole
CMIP6,
increases
1.49,
2.21,
3.53
(relative
to
1985-2005)
above-preindustrial
levels,
while
counterpart
CMIP5
is
1.20,
1.93
3.39
respectively.
Similarly,
total
5.3%,
8.6%,
16.3%
4.4%,
7.0%
12.8%
spatial
distribution
extreme
generally
consistent
both
but
significantly
higher
Northeast
Northwest
hottest
day
South
coldest
night
temperature.
In
south
bank
Yangtze
River,
regions
around
40°N,
shows
heavy
precipitation.
projected
difference
between
mainly
attributable
physical
upgrading
largely
independent
from
emission
scenarios.
Climate Dynamics,
Год журнала:
2021,
Номер
57(11-12), С. 3135 - 3158
Опубликована: Июнь 30, 2021
Abstract
We
provide
an
assessment
of
future
daily
characteristics
African
precipitation
by
explicitly
comparing
the
results
large
ensembles
global
(CMIP5,
CMIP6)
and
regional
(CORDEX,
CORE)
climate
models,
specifically
highlighting
similarities
inconsistencies
between
them.
Results
for
seasonal
mean
are
not
always
consistent
amongst
ensembles:
in
particular,
models
tend
to
project
a
wetter
compared
especially
over
Eastern
Sahel,
Central
East
Africa.
However,
other
more
consistent.
In
general,
all
increase
maximum
intensity
during
wet
season
regions
emission
scenarios
(except
West
Sahel
decrease
frequency
(under
Representative
Concentration
Pathways
RCP8.5)
Atlas
region,
southern
central
Africa,
Africa
Depending
on
season,
length
dry
spells
is
projected
consistently
most
(if
all)
Ethiopian
highlands
region.
Discrepancies
exist
change
specific
seasons.
For
instance,
July–August
show
but
robust
decrease.
Global
also
opposite
sign
spells.
CORE
marked
drying
affected
monsoon
throughout
year,
accompanied
May
July
that
present
ensembles.
This
enhanced
may
be
related
physical
mechanisms
better
resolved
higher
resolution
highlights
importance
process-based
evaluation
controlling
npj Climate and Atmospheric Science,
Год журнала:
2021,
Номер
4(1)
Опубликована: Март 23, 2021
Abstract
Global
climate
projections
suggest
a
significant
intensification
of
summer
heat
extremes
in
the
Middle
East
and
North
Africa
(MENA).
To
assess
regional
impacts,
underpin
mitigation
adaptation
measures,
robust
information
is
required
from
downscaling
studies,
which
has
been
lacking
for
region.
Here,
we
project
future
hot
spells
by
using
Heat
Wave
Magnitude
Index
comprehensive
ensemble
MENA.
Our
results,
business-as-usual
pathway,
indicate
that
second
half
this
century
unprecedented
super-
ultra-extreme
heatwave
conditions
will
emerge.
These
events
involve
excessively
high
temperatures
(up
to
56
°C
higher)
be
extended
duration
(several
weeks),
being
potentially
life-threatening
humans.
By
end
century,
about
MENA
population
(approximately
600
million)
could
exposed
annually
recurring
heatwaves.
It
expected
vast
majority
(>90%)
live
urban
centers,
who
would
need
cope
with
these
societally
disruptive
weather
conditions.