Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(4)
Published: Feb. 14, 2025
Abstract
Humid
heat
extremes,
characterized
by
high
wet
bulb
temperature
(Tw),
pose
significant
health
risks.
While
strong
El
Niño
events
are
known
to
affect
the
frequency
of
extreme
Tw
days,
distinct
impacts
Central
Pacific
(CP)
and
Eastern
(EP)
remain
understudied.
Using
a
12‐member
CMIP6
ensemble
at
discrete
global
warming
targets
(+1.5,
2,
3,
4°C),
this
study
shows
progressively
enhanced
humid
extent
during
EP
primarily
in
Mainland
Southeast
Asia,
while
South
Asia
experiences
regionally
opposing
effects
from
CP
events.
drive
distinctly
different,
varying
patterns
dangerous
Tw,
yet
both
significantly
increase
affected
population
area
impacted
extremes
all
levels.
This
amplification
surpasses
impact
an
additional
degree
warming,
highlighting
Niño's
compounding
effect
on
stress
threats
across
warmer
climates.
Proceedings of the National Academy of Sciences,
Journal Year:
2023,
Volume and Issue:
120(42)
Published: Oct. 9, 2023
As
heatwaves
become
more
frequent,
intense,
and
longer-lasting
due
to
climate
change,
the
question
of
breaching
thermal
limits
becomes
pressing.
A
wet-bulb
temperature
(T
w
)
35
°C
has
been
proposed
as
a
theoretical
upper
limit
on
human
abilities
biologically
thermoregulate.
But,
recent—empirical—research
using
subjects
found
significantly
lower
maximum
T
at
which
thermoregulation
is
possible
even
with
minimal
metabolic
activity.
Projecting
future
exposure
this
empirical
critical
environmental
not
done.
Here,
accurate
threshold
latest
coupled
model
results,
we
quantify
dangerous,
potentially
lethal
heat
for
climates
various
global
warming
levels.
We
find
that
humanity
vulnerable
moist
stress
than
previously
because
these
limits.
Still,
limiting
under
2
nearly
eliminates
risk
widespread
uncompensable
sharp
rise
in
occurs
3
warming.
Parts
Middle
East
Indus
River
Valley
experience
brief
exceedances
only
1.5
More
widespread,
but
brief,
dangerous
+2
climate,
including
eastern
China
sub-Saharan
Africa,
while
US
Midwest
emerges
hotspot
+3
climate.
In
future,
extremes
will
lie
outside
bounds
past
beyond
current
mitigation
strategies
billions
people.
While
some
physiological
adaptation
from
thresholds
described
here
possible,
additional
behavioral,
cultural,
technical
be
required
maintain
healthy
lifestyles.
npj Climate and Atmospheric Science,
Journal Year:
2023,
Volume and Issue:
6(1)
Published: May 26, 2023
Abstract
As
the
world
warms,
extremely
hot
days
are
becoming
more
frequent
and
intense,
reaching
unprecedented
temperatures
associated
with
excess
mortality.
Here,
we
assess
how
anthropogenic
forcings
affect
likelihood
of
maximum
daily
above
50
°C
at
12
selected
locations
around
Mediterranean
Middle
East.
We
adopt
a
risk-based
attribution
methodology
that
utilises
climate
model
simulations
without
human
influence
to
estimate
probability
extremes.
find
all
locations,
would
have
been
rare
or
impossible
in
pre-industrial
world,
but
under
human-induced
change
their
is
rapidly
increasing.
At
hottest
has
increased
by
factor
10–10
3
,
whereas
end
century
such
extremes
could
occur
every
year.
All
may
see
1–2
additional
months
thermal
deaths
2100,
which
stresses
need
for
effective
adaptation
planning.
Science Advances,
Journal Year:
2023,
Volume and Issue:
9(36)
Published: Sept. 8, 2023
As
our
planet
warms,
a
critical
research
question
is
when
and
where
temperatures
will
exceed
the
limits
of
what
human
body
can
tolerate.
Past
modeling
efforts
have
investigated
35°C
wet-bulb
threshold,
proposed
as
theoretical
upper
limit
to
survivability
taking
into
account
physiological
behavioral
adaptation.
Here,
we
conduct
an
extreme
value
theory
analysis
weather
station
observations
climate
model
projections
investigate
emergence
empirically
supported
heat
compensability
limit.
We
show
that
hottest
parts
world
already
experience
these
extremes
on
limited
basis
under
moderate
continued
warming
every
continent,
except
Antarctica,
see
rapid
increase
in
their
extent
frequency.
To
conclude,
discuss
consequences
this
noncompensable
need
for
incorporating
different
thermal
adaptation
planning.
Frontiers in Science,
Journal Year:
2024,
Volume and Issue:
2
Published: Oct. 1, 2024
The
reality
of
human-induced
climate
change
is
unequivocal
and
exerts
an
ever-increasing
global
impact.
Access
to
the
latest
scientific
information
on
current
projection
future
trends
important
for
planning
adaptation
measures
informing
international
efforts
reduce
emissions
greenhouse
gases
(GHGs).
Identification
hazards
risks
may
be
used
assess
vulnerability,
determine
limits
adaptation,
enhance
resilience
change.
This
article
highlights
how
recent
research
programs
are
continuing
elucidate
processes
advance
projections
across
major
systems
identifies
remaining
knowledge
gaps.
Key
findings
include
projected
increases
in
monsoon
rainfall,
resulting
from
a
changing
balance
between
rainfall-reducing
effect
aerosols
rainfall-increasing
GHGs;
strengthening
storm
track
North
Atlantic;
increase
fraction
precipitation
that
falls
as
rain
at
both
poles;
frequency
severity
El
Niño
Southern
Oscillation
(ENSO)
events,
along
with
changes
ENSO
teleconnections
America
Europe;
hazardous
hot-humid
extremes.
These
have
potential
human
natural
systems.
Nevertheless,
these
reduced
via
urgent,
science-led
by
reductions
GHGs.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(1)
Published: Jan. 8, 2024
Abstract
We
compare
high‐resolution
land‐surface
temperature
(LST)
estimates
from
the
GOES‐16/17
(GOES)
satellites
to
ERA‐5
Land
(ERA‐5)
reanalysis
data
across
nine
large
US
cities.
quantify
offset
and
find
that
generally
overestimates
LST
compared
GOES
by
1.63°C.
However,
this
overestimation
is
less
pronounced
in
urban
areas,
underscoring
limitations
of
capturing
gradient
between
non‐urban
areas.
then
examine
three
quantities:
Surface
Urban
Heat
Island
Intensity
(SUHII),
extreme
events,
exposure
population.
does
not
accurately
represent
diurnal
variation
magnitude
SUHII
GOES.
Furthermore,
while
was
on
average
too
warm,
underestimates
heat
an
2.40°C.
Our
analysis
reveals
higher
population
high
set
cities
studied.
This
discrepancy
especially
when
estimating
fraction
are
most
exposed
heat.