Advances in Climate Change Research,
Год журнала:
2024,
Номер
15(4), С. 737 - 750
Опубликована: Май 23, 2024
Non-methane
short-lived
climate
forcer
(SLCF)
or
near-term
(NTCF)
emissions,
as
a
significant
driver
of
change,
can
be
reduced
to
improve
air
quality.
These
reductions
may
contribute
additional
warming
the
system
in
short
term,
thereby
strongly
affecting
likelihood
extremes.
However,
there
has
been
no
quantitative
assessment
impact
non-methane
SLCF
mitigation
on
compound
flood–heatwave
extremes
(CFHEs).
This
study
quantitatively
investigates
changes
future
(2031–2050
versus
1995–2014)
CFHEs
and
resulting
population
exposure
Northern
Hemisphere
(NH)
due
reductions.
We
used
multi-model
ensemble
simulations
under
two
scenarios
from
Aerosol
Chemistry
Model
Intercomparison
Project
(AerChemMIP)
Coupled
Phase
6
(CMIP6).
The
share
same
greenhouse
gas
(GHG)
emissions
but
have
weak
(Shared
Socioeconomic
Pathway
(SSP)
3-7.0)
strong
(SSP3-7.0-lowNTCF)
levels
quality
control
measures.
results
show
that
during
2031–2050
about
7.3%
±
2.3%
increase
grid
NH
relative
period
1995–2014.
frequency,
intensity,
duration
by
varying
degrees.
During
2031–2050,
frequency
across
increases
2.9
0.9
events
per
decade
CFHE
are
more
pronounced
East
Asia,
South
Siberia,
northern
eastern
North
America.
In
intensities
both
heatwaves
floods
corresponding
markedly,
where
heatwave
magnitude
(HWM)
0.3
0.2
Asia
weighted
average
precipitation
(WAP)
18.3%
15.3%
12.0%
4.5%
respectively.
other
regions,
rising
temperatures
dominate
CFHEs.
With
regard
CFHEs,
SLCFs
0.1
d.
Regionally,
sensitivity
global
caused
is
1.2–1.9
times
higher
than
GHG
forcing.
NH-averaged
(5.0
2.0)
×
105
person
event
2031–2050.
emphasizes
importance
considering
impacts
cleaner
responses
societal
planning.
Abstract
Compound
climate
extremes
(here
referred
to
compound
dry–hot
events
and
pluvial–hot
events)
result
in
devastating
disasters
which
threaten
water‐food‐energy
security.
However,
a
warming
scenario,
the
risk
of
occurrence,
quantification
uncertainty,
associated
drivers
extremes—particularly
events—have
not
been
fully
explored.
By
leveraging
model
large
ensembles,
it
is
revealed
that
projected
increase
2–3
times
over
most
global
land
masses
future
Representative
Concentration
Pathway
(RCP)
8.5
forcing
compared
with
historical
forcing.
Increased
risks
are
mainly
attributed
changes
temperature
dependence
between
precipitation
temperature,
while
change
contributing
these
two
exhibits
approximately
spatial
complementary.
In
world,
hot
spots
lie
Europe,
South
Africa,
Amazon,
those
mostly
eastern
USA,
southern
Asia,
Australia,
central
Africa.
These
findings
help
stakeholders
decision
makers
develop
package
adaptation
strategies
manage
mitigate
extremes.
Journal of Climate,
Год журнала:
2022,
Номер
36(2), С. 693 - 709
Опубликована: Окт. 5, 2022
Abstract
Heavy
precipitation
(HP)
events
can
be
preceded
by
moist
heatwaves
(HWs;
i.e.,
hot
and
humid
weather),
both
intensified
urbanization.
However,
the
effect
of
HWs
on
increasing
urban
HP
remains
unknown.
Based
statistical
analyses
daily
weather
observations
ERA5
reanalysis
data,
we
herein
investigate
urban-intensified
dividing
summer
into
NoHW-
HW-preceded
in
Yangtze
River
delta
(YRD)
agglomeration
China.
During
period
1961–2019,
YRD
has
experienced
more
frequent,
longer-lasting,
stronger
intense
season
(i.e.,
June–August),
urbanization
contributed
to
these
increases
(by
22.66%–37.50%).
In
contrast,
effects
are
almost
absent
if
remove
from
all
events.
Our
results
show
that
urbanization-induced
associated
with,
magnified
by,
areas
region.
Moist
conducive
an
unstable
atmosphere
stormy
weather,
they
also
enhance
heat
island
intensity,
driving
over
areas.
Significance
Statement
The
contribution
heavy
been
widely
reported
previous
studies.
(hot
extremes);
however,
it
is
unknown
whether
HP.
We
choose
explore
this
question
find
contributes
frequency,
duration,
maximum
cumulative
intensity
season.
signal
not
detectable
other
words,
play
a
key
role
magnifying
Given
projected
continue
expanding
occur
with
frequency
future,
water
cycle
merits
further
investigation.
Geophysical Research Letters,
Год журнала:
2022,
Номер
49(18)
Опубликована: Сен. 20, 2022
Abstract
Compared
to
singular
hot
or
wet
extremes,
their
occurrence
in
close
sequence
might
cause
larger
impacts,
because
the
initial
hazard
either
increases
exposure/vulnerability
of
affected
communities
next
physically
worsens
second
hazard.
Heatwave‐preconditioned
hourly
precipitation
extremes
Yangtze
River
Valley
are
typical
latter
situation.
Fueled
by
soaring
convective
energy
after
heatwaves'
passage,
heavier,
intensifying
faster,
and
more
concentrated
during
afternoon
evening,
compared
those
not
proceeded
heatwaves.
Consequently,
flash
flood‐producing
events
(e.g.,
50
mm/hr
stronger)
account
for
fractions
preconditioned
than
non‐preconditioned
group,
with
spectrum
difference
further
exaggerated
warming.
This
drives
frequency
increase
potentially
high‐impact
several‐fold
expected
from
widely‐adopted
univariate
perspective.
These
results
point
heatwave‐preconditioned
as
an
emerging
climate
change
carrying
greater
flood
risks.
Geophysical Research Letters,
Год журнала:
2023,
Номер
50(14)
Опубликована: Июль 18, 2023
Abstract
The
abrupt
alternation
between
hot
and
wet
extremes
can
lead
to
more
severe
societal
impacts
than
isolated
extremes.
However,
despite
an
understanding
of
separately,
their
temporally
compounding
characteristics
are
not
well
examined
yet.
Our
study
presents
a
comprehensive
assessment
successive
heat‐pluvial
pluvial‐heat
events
globally.
We
find
that
these
within
week
occur
every
6–7
years
on
average
warm
seasons
during
1956–2015,
about
15%
often
would
be
expected
by
chance,
they
have
significant
increase
in
frequency
22%
per
decade
due
warming.
further
investigate
the
role
vapor
pressure
deficit
(VPD)
(pluvial‐heat)
linked
negative
(positive)
VPD
anomalies.
results
statistically
based
moving‐blocks
bootstrap
resampling
field
significance
tests,
highlighting
methods'
importance
robustly
identifying
compound
under
autocorrelation
multiple‐testing
conditions.
Ecological Indicators,
Год журнала:
2022,
Номер
138, С. 108817 - 108817
Опубликована: Апрель 1, 2022
Mountain
ecosystems
regulate
global
terrestrial
carbon
dynamics
and
are
sensitive
to
changes
of
extreme
climate.
To
discuss
climate's
impact
on
productivity
vegetation
by
using
the
elevation
change
as
a
binding
force
can
provide
new
reference
for
sink
management
ecosystem
in
alpine
regions.
The
CASA
model
Rclimdex1.0
were
used
calculate
NPP
16
climate
extremes
indices,
respectively,
from
1982
2019
Yunnan.
response
characteristics
regional
calculated
unary
regression
analysis,
correlation
geographic
detector,
relative
importance
analysis.
results
follows:
(1)
turning
point
various
types
appeared
late
1980s
(2)
between
precipitation
index
is
more
dependent
than
temperature
indices.
(3)
Extreme
indices
middle
high-elevation
areas.
As
result,
increased
10%
after
compared
with
that
before
point.
(4)
In
range
Ⅰ-IV
(76–4000
m),
proportion
double-factor
increase
was
30%,
while
4000–5000
m,
<10%.
(5)
primary
controlling
factors
Ⅰ﹣III
(76–3000
m)
R25mm,
R10mm,
respectively.
increasing
IV﹣Ⅵ
(4000–6000
SU25,
TR20,
FD0,
This
study
provides
insights
into
perspective
elevation,
emphasizing
ecological
environment
regions
which
response.
Advances in Climate Change Research,
Год журнала:
2024,
Номер
15(3), С. 547 - 556
Опубликована: Май 25, 2024
The
increasingly
frequent
and
severe
regional-scale
compound
heatwave‒drought
extreme
events
(CHDEs),
driven
by
global
warming,
present
formidable
challenges
to
ecosystems,
residential
livelihoods,
economic
conditions.
However,
uncertainty
persists
regarding
the
future
trend
of
CHDEs
their
insights
into
regional
spatiotemporal
heterogeneity.
By
integrating
daily
meteorological
data
from
observations
in
1961–2022
climate
models
(GCMs)
based
on
Shared
Socioeconomic
Pathways,
evolution
patterns
were
compared
examined
among
three
sub-catchments
Yangtze
River
Basin,
return
periods
CHDE
2050s
2100s
projected.
findings
indicate
that
during
2022
period
was
warmest
driest
recorded
1961–2022,
with
precipitation
less
than
154.5
mm
a
mean
maximum
temperature
3.4
°C
higher
average
1981–2010,
whereas
characteristics
exhibited
temporal
spatial
variation.
In
July–August
2022,
most
notable
feature
its
extremeness
since
1961,
∼
200-year
upstream,
80-year
midstream,
40-year
downstream,
respectively.
2050,
witnessed
would
likely
be
reduced
one-third.
Looking
towards
2100,
under
highest
emission
scenario
SSP585,
it
projected
substantially
increase
frequency
CHDEs,
one-third
upstream
as
well
halved
midstream.
These
provide
valuable
changing
risks
associated
forthcoming
extremes,
emphasizing
urgency
addressing
these
management
sustainable
development.
Abstract
The
increase
in
record‐breaking
extreme
events
caused
by
climate
change
poses
a
threat
to
human
health
and
well‐being.
Understanding
the
future
impacts
of
such
on
global
populations
can
provide
decision‐making
support
for
policies
aiming
mitigate
change.
Here,
we
investigated
population
exposure
eight
indices
drivers
trajectories
based
National
Aeronautics
Space
Administration
Earth
Exchange
Global
Daily
Downscaled
Projections
Coupled
Model
Intercomparison
Project
6
projection
data
under
four
shared
socioeconomic
pathway
scenarios
at
spatial
resolution
0.25°
×
0.25°.
results
show
that
mid‐twenty‐first
century,
most
regions
worldwide,
especially
Africa
South
America,
will
continue
experience
temperatures
compound
drought
heatwaves
(CDHWs).
Regarding
exposure,
SSP3‐7.0
late
twenty‐first
mean
value
multimodel
median
expected
annual
(EAE)
all
temperature
CDHW
reaches
8.12
billion
persons
per
year.
Population
hotspots
be
concentrated
Central
Africa,
Asia,
Southeast
East
mostly
developing
countries,
where
55.01%–87.42%
EAE
is
found.
are
spatially
heterogeneous.
probability
contributes
more
than
growth
world
except
Middle
East,
Africa.
These
findings
reveal
probabilities
exposures
extremes,
which
inform
understanding
intersections
between
risk
management.