Abstract.
Hydrological
drought
is
one
of
the
main
hydroclimatic
hazards
worldwide,
affecting
water
availability,
ecosystems
and
socioeconomic
activities.
This
phenomenon
commonly
characterized
by
Standardized
Streamflow
Index
(SSI),
which
widely
used
because
its
straightforward
formulation
calculation.
Nevertheless,
there
limited
understanding
what
SSI
actually
reveals
about
how
climate
anomalies
propagate
through
terrestrial
cycle.
To
find
possible
explanations,
we
implemented
SUMMA
hydrological
model
coupled
with
mizuRoute
routing
in
six
hydroclimatically
different
case
study
basins
located
on
western
slopes
extratropical
Andes,
examined
correlations
between
(computed
from
models
for
1,
3
6-month
time
scales)
potential
explanatory
variables
–
including
precipitation
simulated
catchment-scale
storages
aggregated
at
scales.
Additionally,
analyzed
impacts
adopting
scales
propagation
analyses
specific
events
meteorological
to
soil
moisture
focus
their
duration
intensity.
The
results
reveal
that
choice
scale
has
larger
effects
rainfall-dominated
regimes
compared
snowmelt-driven
basins,
especially
when
fluxes
are
longer
than
9
months.
In
all
analyzed,
strongest
relationships
(Spearman
rank
correlation
values
over
0.7)
were
obtained
using
aggregations
compute
9–12
months
variables,
excepting
aquifer
storage
basins.
Finally,
show
trajectories
Precipitation
(SPI),
Soil
Moisture
(SSMI)
may
change
drastically
selection
scale.
Overall,
this
highlights
need
caution
selecting
standardized
indices
associated
scales,
since
event
characterizations,
monitoring
analyses.
Environmental Research Letters,
Journal Year:
2024,
Volume and Issue:
19(5), P. 054030 - 054030
Published: April 12, 2024
Abstract
Droughts
exert
widespread
impacts
on
both
natural
and
social
systems,
there
is
accumulating
evidence
that
this
situation
may
worsen
in
the
context
of
global
warming.
Despite
importance
assessing
changes
droughts
to
understand
their
potential
future
society,
studies
are
unevenly
distributed
worldwide.
In
study,
utilizing
bias-corrected
CMIP6
simulations
a
standard
precipitation-evaporation
index
based
approach,
we
quantified
expected
drought
properties
across
735
Brazilian
catchments
under
SSP2-4.5
SSP5-8.5
scenarios.
Beyond
evaluating
statistical
droughts,
assessed
occurrence
land
use
water
demand
perspectives
propose
new
framework
better
link
with
long-
short-term
conditions
precipitation
(
P
)
evapotranspiration
PET
).
Our
results
indicate
events
projected
become
more
frequent
severe
future,
high
model
agreement.
According
scenario,
at
least
half
cropland
pasture
areas
will
experience
an
increase
over
30%
by
end
century.
Furthermore,
among
85%
nearly
90%
also
exhibit
increased
demand,
which
likely
exacerbate
scarcity.
The
investigation
relationship
between
climate
variables
suggests
augmented
long-term
average
-variability,
but
not
necessarily
.
For
instance,
50%
evaluated
intensification
even
increases
mean
We
believe
study
contribute
(a)
improve
resiliency
helping
achieve
objectives
National
Water
Security
Plan
(b)
deepen
our
understanding
uncertain
future.
International Journal of Climatology,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Sept. 28, 2024
Abstract
Global
climate
models
(GCMs)
are
extensively
used
to
calculate
standardized
drought
indices.
However,
inaccuracies
in
GCM
simulations
and
uncertainties
inherent
the
standardization
methodology
limit
precision
of
evaluations.
The
objective
this
research
is
remove
bias
GCMs
for
improving
monitoring
assessment.
Consequently,
article
proposes
a
new
framework
index
under
ensemble
GCMs—Multi‐Model
Quantile
Mapped
Standardized
Precipitation
Index
(MMQMSPI).
In
accordance
(SPI),
second
stage
derives
by
assessing
feasibility
parametric
nonparametric
during
standardization.
application,
we
18
from
Coupled
Model
Intercomparison
Project
Phase
6
(CMIP6)
data
precipitation
across
32
grid
points
within
Tibetan
Plateau
region.
comparative
findings
reveal
that
integration
KCGMD
most
suitable
choice
compared
other
best‐fitted
univariate
distributions
both
features
proposed
framework.
research,
assess
implications
evaluating
future
patterns
years
2015–2100
using
seven
different
time
periods
three
scenarios.
Temporal
behavior
clearly
shows
monthly
variations
pattern
MMQMSPI,
these
differ
on
each
scale,
but
drastic
change
can
be
seen
over
long
term,
i.e.,
extreme
dry
wet
conditions,
with
higher
probability
all
Abstract.
Hydrological
drought
is
one
of
the
main
hydroclimatic
hazards
worldwide,
affecting
water
availability,
ecosystems
and
socioeconomic
activities.
This
phenomenon
commonly
characterized
by
Standardized
Streamflow
Index
(SSI),
which
widely
used
because
its
straightforward
formulation
calculation.
Nevertheless,
there
limited
understanding
what
SSI
actually
reveals
about
how
climate
anomalies
propagate
through
terrestrial
cycle.
To
find
possible
explanations,
we
implemented
SUMMA
hydrological
model
coupled
with
mizuRoute
routing
in
six
hydroclimatically
different
case
study
basins
located
on
western
slopes
extratropical
Andes,
examined
correlations
between
(computed
from
models
for
1,
3
6-month
time
scales)
potential
explanatory
variables
–
including
precipitation
simulated
catchment-scale
storages
aggregated
at
scales.
Additionally,
analyzed
impacts
adopting
scales
propagation
analyses
specific
events
meteorological
to
soil
moisture
focus
their
duration
intensity.
The
results
reveal
that
choice
scale
has
larger
effects
rainfall-dominated
regimes
compared
snowmelt-driven
basins,
especially
when
fluxes
are
longer
than
9
months.
In
all
analyzed,
strongest
relationships
(Spearman
rank
correlation
values
over
0.7)
were
obtained
using
aggregations
compute
9–12
months
variables,
excepting
aquifer
storage
basins.
Finally,
show
trajectories
Precipitation
(SPI),
Soil
Moisture
(SSMI)
may
change
drastically
selection
scale.
Overall,
this
highlights
need
caution
selecting
standardized
indices
associated
scales,
since
event
characterizations,
monitoring
analyses.