Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(6)
Published: March 9, 2021
Abstract
Concepts
like
the
100‐year
flood
event
can
be
misleading
if
they
are
not
updated
to
reflect
significant
changes
over
time.
Here,
we
model
observed
annual
maximum
daily
streamflow
using
a
nonstationary
approach
provide
first
global
picture
of
in:
(a)
magnitudes
20‐,
50‐,
and
floods
(i.e.,
flows
given
exceedance
probability
in
each
year
);
(b)
return
periods
floods,
as
assessed
1970
fixed
magnitude
(c)
corresponding
probabilities.
Empirically,
find
20‐/50‐year
have
mostly
increased
temperate
climate
zones,
but
decreased
arid,
tropical,
polar,
cold
zones.
In
contrast,
arid/temperate
zones
exhibit
mixed
trends
results
influenced
by
small
number
stations
with
long
records,
highlight
need
for
continued
updating
hazard
assessments.
Earth s Future,
Journal Year:
2023,
Volume and Issue:
11(3)
Published: March 1, 2023
Abstract
The
risk
of
floods
has
increased
in
South
Asia
due
to
high
vulnerability
and
exposure.
August
2022
Pakistan
flood
shows
a
glimpse
the
enormity
devastation
that
can
further
rise
under
warming
climate.
deluge
caused
by
2022,
which
badly
hit
country’s
southern
provinces,
is
incomparable
any
recent
events
terms
vast
spatial
temporal
scale.
event
ranked
second
human
mortality,
while
this
was
top
displaced
about
33
million
people
Pakistan.
Using
observations
climate
projections,
we
examine
causes
implications
Multiday
(∼15
days)
extreme
precipitation
on
wet
antecedent
soil
moisture
conditions
primary
driver
2022.
two
atmospheric
rivers
passed
over
Streamflow
simulations
from
multiple
hydrological
models
show
multiday
floods.
Several
flood‐affected
stations
experienced
anomalously
higher
flow
than
upstream
stations.
highlights
adaptation
challenges
facing
along
with
substantial
need
for
mitigation
reduce
such
events.
Water Resources Research,
Journal Year:
2020,
Volume and Issue:
56(3)
Published: Feb. 19, 2020
Due
to
difficulties
in
identifying
a
climate
change
signal
flood
magnitude,
it
has
been
suggested
that
shifts
timing,
is,
the
day
of
annual
streamflow
maxima,
may
be
detectable.
Here,
we
use
high-quality
streamflow,
largely
free
snowmelt,
from
221
catchments
across
Australia
investigate
influence
soil
moisture
and
rainfall
timing
on
maxima
timing.
In
tropical
areas
find
is
strongly
linked
both
maxima.
However,
southern
more
correlated
with
than
The
link
between
flood,
moisture,
confounded
by
event
severity:
For
less
extreme
events
likely
correspond
whereas
becomes
increasingly
important
as
severity
increases.
Using
circular
regression
nonstationarity,
shifting
earlier
year
tropics
later
southwest
continent,
consistent
changes
mean
due
expansion.
southeast
Australia,
there
evidence
mechanisms
controlling
seasonality
are
changing
reversal
trends
post
Millennium
Drought.
Overall,
compared
found
have
greater
Precipitation
extremes
will
increase
in
a
warming
climate,
but
the
response
of
flood
magnitudes
to
heavier
precipitation
events
is
less
clear.
Historically,
there
little
evidence
for
systematic
increases
magnitude
despite
observed
extremes.
Here
we
investigate
how
change
warming,
using
large
initial-condition
ensemble
simulations
with
single
climate
model,
coupled
hydrological
model.
The
model
chain
was
applied
historical
(1961–2000)
and
warmer
future
(2060–2099)
conditions
78
watersheds
Bavaria,
region
comprising
headwater
catchments
Inn,
Danube
Main
River,
thus
representing
an
area
expressed
heterogeneity.
For
majority
catchments,
identify
‘return
interval
threshold’
relationship
between
increases:
at
return
intervals
above
this
threshold,
further
extreme
frequency
clearly
yield
increased
magnitudes;
below
modulated
by
land
surface
processes.
We
suggest
that
threshold
behaviour
can
reconcile
climatological
perspectives
on
changing
risk
climate.
Germany
rainfall
processes
not
above,
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(4)
Published: Feb. 10, 2021
Abstract
Hydrometeorological
flood
generating
processes
(excess
rain,
short
long
snowmelt,
and
rain‐on‐snow)
underpin
our
understanding
of
behavior.
Knowledge
about
improves
hydrological
models,
frequency
analysis,
estimation
climate
change
impact
on
floods,
etc.
Yet,
not
much
is
known
how
catchment
attributes
influence
the
spatial
distribution
processes.
This
study
aims
to
offer
a
comprehensive
structured
approach
close
this
knowledge
gap.
We
employ
large
sample
(671
catchments
across
contiguous
United
States)
evaluate
use
two
complementary
approaches:
A
statistics‐based
which
compares
attribute
distributions
different
processes;
random
forest
model
in
combination
with
an
interpretable
machine
learning
(accumulated
local
effects
[ALE]).
The
ALE
method
has
been
used
often
hydrology,
it
overcomes
significant
obstacle
many
statistical
methods,
confounding
effect
correlated
attributes.
As
expected,
we
find
(fraction
snow,
aridity,
precipitation
seasonality,
mean
precipitation)
be
most
influential
process
distribution.
However,
varies
both
type.
also
can
predicted
for
ungauged
relatively
high
accuracy
(
R
2
between
0.45
0.9).
implication
these
findings
should
considered
future
studies,
as
changes
characteristics
Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(6)
Published: March 9, 2021
Abstract
Concepts
like
the
100‐year
flood
event
can
be
misleading
if
they
are
not
updated
to
reflect
significant
changes
over
time.
Here,
we
model
observed
annual
maximum
daily
streamflow
using
a
nonstationary
approach
provide
first
global
picture
of
in:
(a)
magnitudes
20‐,
50‐,
and
floods
(i.e.,
flows
given
exceedance
probability
in
each
year
);
(b)
return
periods
floods,
as
assessed
1970
fixed
magnitude
(c)
corresponding
probabilities.
Empirically,
find
20‐/50‐year
have
mostly
increased
temperate
climate
zones,
but
decreased
arid,
tropical,
polar,
cold
zones.
In
contrast,
arid/temperate
zones
exhibit
mixed
trends
results
influenced
by
small
number
stations
with
long
records,
highlight
need
for
continued
updating
hazard
assessments.