Science,
Journal Year:
2025,
Volume and Issue:
387(6731), P. 278 - 284
Published: Jan. 16, 2025
Persistent
multiyear
drought
(MYD)
events
pose
a
growing
threat
to
nature
and
humans
in
changing
climate.
We
identified
inventoried
global
MYDs
by
detecting
spatiotemporally
contiguous
climatic
anomalies,
showing
that
have
become
drier,
hotter,
led
increasingly
diminished
vegetation
greenness.
The
terrestrial
land
affected
has
increased
at
rate
of
49,279
±
14,771
square
kilometers
per
year
from
1980
2018.
Temperate
grasslands
exhibited
the
greatest
declines
greenness
during
MYDs,
whereas
boreal
tropical
forests
had
comparably
minor
responses.
With
becoming
more
common,
this
quantitative
inventory
occurrence,
severity,
trend,
impact
provides
an
important
benchmark
for
facilitating
effective
collaborative
preparedness
toward
mitigation
adaptation
such
extreme
events.
Earth s Future,
Journal Year:
2020,
Volume and Issue:
8(6)
Published: April 19, 2020
There
is
strong
evidence
that
climate
change
will
increase
drought
risk
and
severity,
but
these
conclusions
depend
on
the
regions,
seasons,
metrics
being
considered.
We
analyze
changes
in
across
hydrologic
cycle
(precipitation,
soil
moisture,
runoff)
projections
from
Phase
Six
of
Coupled
Model
Intercomparison
Project
(CMIP6).
The
multimodel
ensemble
shows
robust
drying
mean
state
many
regions
by
end
21st
century,
even
following
more
aggressive
mitigation
pathways
(SSP1-2.6
SSP2-4.5).
Regional
hotspots
with
include
western
North
America,
Central
Europe
Mediterranean,
Amazon,
southern
Africa,
China,
Southeast
Asia,
Australia.
Compared
to
SSP3-7.0
SSP5-8.5,
however,
severity
lower
warming
scenarios
substantially
reduced
further
precipitation
declines
are
avoided.
Along
state,
historically
most
extreme
events
also
increases
warming,
200–300%
some
regions.
Soil
moisture
runoff
CMIP6
robust,
spatially
extensive,
severe
than
precipitation,
indicating
an
important
role
for
other
temperature-sensitive
processes,
including
evapotranspiration
snow.
Given
similarity
responses
between
CMIP5
CMIP6,
we
speculate
both
generations
models
subject
similar
uncertainties,
vegetation
model
representations
degree
which
consistent
observations.
These
topics
should
be
explored
evaluate
whether
offer
reasons
have
increased
confidence
projections.
Science,
Journal Year:
2020,
Volume and Issue:
368(6488), P. 256 - 260
Published: April 16, 2020
Droughts
of
the
future
are
likely
to
be
more
frequent,
severe,
and
longer
lasting
than
they
have
been
in
recent
decades,
but
drought
risks
will
lower
if
greenhouse
gas
emissions
cut
aggressively.
This
review
presents
a
synopsis
tools
required
for
understanding
statistics,
physics,
dynamics
its
causes
historical
context.
Although
these
applied
most
extensively
United
States,
Europe,
Amazon
region,
not
as
widely
used
other
drought-prone
regions
throughout
rest
world,
presenting
opportunities
research.
Water
resource
managers,
early
career
scientists,
veteran
researchers
see
improve
our
drought.
Annals of the New York Academy of Sciences,
Journal Year:
2020,
Volume and Issue:
1472(1), P. 49 - 75
Published: April 4, 2020
Abstract
Globally,
thermodynamics
explains
an
increase
in
atmospheric
water
vapor
with
warming
of
around
7%/°C
near
to
the
surface.
In
contrast,
global
precipitation
and
evaporation
are
constrained
by
Earth's
energy
balance
at
∼2–3%/°C.
However,
this
rate
is
suppressed
rapid
adjustments
response
greenhouse
gases
absorbing
aerosols
that
directly
alter
budget.
Rapid
forcings,
cooling
effects
from
scattering
aerosol,
observational
uncertainty
can
explain
why
observed
responses
currently
difficult
detect
but
expected
emerge
accelerate
as
increases
aerosol
forcing
diminishes.
Precipitation
be
smaller
over
land
than
ocean
due
limitations
on
moisture
convergence,
exacerbated
feedbacks
affected
adjustments.
Thermodynamic
fluxes
amplify
wet
dry
events,
driving
intensification
extremes.
The
deviate
a
simple
thermodynamic
in‐storm
larger‐scale
feedback
processes,
while
changes
large‐scale
dynamics
catchment
characteristics
further
modulate
frequency
flooding
increases.
Changes
circulation
radiative
evolving
surface
temperature
patterns
capable
dominating
cycle
some
regions.
Moreover,
direct
impact
human
activities
through
abstraction,
irrigation,
use
change
already
significant
component
regional
importance
demand
grows
population.
Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
47(11)
Published: May 10, 2020
Abstract
Quantifying
how
climate
change
drives
drought
is
a
priority
to
inform
policy
and
adaptation
planning.
We
show
that
the
latest
Coupled
Model
Intercomparison
Project
(CMIP6)
simulations
project
coherent
regional
patterns
in
meteorological
for
two
emissions
scenarios
2100.
find
robust
projected
changes
seasonal
duration
frequency
(robust
over
>45%
of
global
land
area),
despite
lack
agreement
across
models
mean
precipitation
(24%
area).
Future
are
larger
more
consistent
CMIP6
compared
CMIP5.
regionalized
increases
decreases
driven
by
both
variability.
Conversely,
intensity
most
regions
but
not
simulated
well
historically
models.
The
projections
provides
significant
new
opportunities
water
resource
Journal of Hydrology Regional Studies,
Journal Year:
2019,
Volume and Issue:
22, P. 100593 - 100593
Published: Feb. 15, 2019
This
study
has
three
spatial
scales:
global
(0.5°),
macro-regional,
and
country
scale.
The
database
of
drought
events
specific
entries
for
each
macro-region
country.
We
constructed
a
meteorological
from
1951
to
2016,
now
hosted
by
the
Global
Drought
Observatory
European
Commission's
Joint
Research
Centre.
Events
were
detected
at
macro-regional
scale
based
on
separate
analysis
Standardized
Precipitation-Evapotranspiration
Index
(SPEI)
Precipitation
(SPI)
different
accumulation
scales
(from
3
72
months),
using
as
input
Climatology
Centre
(GPCC)
Climatic
Unit
(CRU)
Time
Series
datasets.
includes
approximately
4800
SPEI-3
4500
SPI-3.
Each
event
is
described
its
start
end
date,
duration,
intensity,
severity,
peak,
average
maximum
area
in
drought,
special
score
classify
52
mega-droughts.
derived
trends
frequency
separately
SPI
SPEI
12-month
scale,
which
usually
related
hydrological
droughts.
Results
show
several
hotspots
last
decades:
Amazonia,
southern
South
America,
Mediterranean
region,
most
Africa,
north-eastern
China
and,
lesser
extent,
central
Asia
Australia.
Over
North
Europe,
Asia,
Australia,
recent
progressive
temperature
increase
outbalanced
precipitation
causing
more
frequent
severe
Journal of Climate,
Journal Year:
2019,
Volume and Issue:
33(9), P. 3635 - 3661
Published: Dec. 26, 2019
Abstract
Two
questions
motivated
this
study:
1)
Will
meteorological
droughts
become
more
frequent
and
severe
during
the
twenty-first
century?
2)
Given
projected
global
temperature
rise,
to
what
extent
does
inclusion
of
(in
addition
precipitation)
in
drought
indicators
play
a
role
future
droughts?
To
answer,
we
analyzed
changes
frequency,
severity,
historically
undocumented
extreme
over
1981–2100,
using
standardized
precipitation
index
(SPI;
including
only)
precipitation-evapotranspiration
(SPEI;
indirectly
temperature),
under
two
representative
concentration
pathways
(RCP4.5
RCP8.5).
As
input
data,
employed
103
high-resolution
(0.44°)
simulations
from
Coordinated
Regional
Climate
Downscaling
Experiment
(CORDEX),
based
on
combination
16
circulation
models
(GCMs)
20
regional
(RCMs).
This
is
first
study
projections
RCMs
such
large
ensemble
RCMs.
Based
only,
~15%
land
likely
experience
2071–2100
versus
1981–2010
for
both
scenarios.
increase
larger
(~47%
RCP4.5,
~49%
RCP8.5)
when
are
used.
Both
SPI
SPEI
project
droughts,
especially
RCP8.5,
southern
South
America,
Mediterranean
region,
Africa,
southeastern
China,
Japan,
Australia.
A
decrease
high
latitudes
Northern
Hemisphere
Southeast
Asia.
If
included,
characteristics
North
Amazonia,
central
Europe
Asia,
Horn
India,
Australia;
if
only
considered,
they
found
those
areas.
Abstract
This
review
examines
the
role
of
atmospheric
evaporative
demand
(AED)
in
drought.
AED
is
a
complex
concept
and
here
we
discuss
possible
definitions,
subsequent
metrics
to
measure
estimate
AED,
different
physical
drivers
that
control
it.
The
influence
on
meteorological,
environmental/agricultural
hydrological
droughts
discussed,
stressing
important
spatial
differences
related
climatological
conditions.
Likewise,
drought
has
implications
regarding
how
consider
their
attempts
quantify
severity.
Throughout
article,
assess
literature
findings
with
respect
to:
(a)
recent
trends
future
projections;
(b)
several
uncertainties
data
availability;
(c)
sensitivity
current
AED;
(d)
roles
both
radiative
physiological
effects
increasing
CO
2
concentrations
may
play
as
progress
into
future.
All
these
issues
preclude
identifying
simple
effect
Rather
it
calls
for
evaluations
impacts
under
climate
scenarios,
considering
feedbacks
governing
system.
article
categorized
under:
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